胶州湾基底新元古代变花岗岩的发现与地质意义

董杰; 朱晓青; 窦衍光; 宋维宇; 薛碧颖; 邹亮

doi:10.16562/j.cnki.0256-1492.2023031002

胶州湾基底新元古代变花岗岩的发现与地质意义

董杰^{1, 2,},
朱晓青^{1, 3, ,},
窦衍光^{1, 3},
宋维宇³,
薛碧颖³,
邹亮^{1, 3}

1.
自然资源部滨海城市地下空间地质安全重点实验室，青岛 266101
2.
青岛地质工程勘察院，青岛 266101
3.
中国地质调查局青岛海洋地质研究所，青岛 266237

基金项目: 自然资源部滨海城市地下空间地质安全重点实验室开放课题（BHKF2021Z06）；中国地质调查局青岛多要素城市地质调查项目（DD20189230）

详细信息

作者简介:
董杰（1981—），男，博士，正高级工程师，主要从事水工环地质研究，E-mail：13853286966@163.com

通讯作者:
朱晓青（1982—），男，博士，副研究员，主要从事构造地质与海洋地质等研究，E-mail：xq_zhu0819@126.com

中图分类号: P736
计量
- 文章访问数: 35
- HTML全文浏览量: 1
- PDF下载量: 16
出版历程
- 收稿日期: 2023-03-09
- 修回日期: 2024-02-27
- 刊出日期: 2024-12-27

Discovery and geological implications of Neoproterozoic metagranite in Jiaozhou Bay

DONG Jie^{1, 2,},
ZHU Xiaoqing^{1, 3, ,},
DOU Yanguang^{1, 3},
SONG Weiyu³,
XUE Biying³,
ZOU Liang^{1, 3}

1.
Key Laboratory of Geological Safety of Coastal Urban Underground Space, Ministry of Natural Resources China, Qingdao 266101, China
2.
Qingdao Geo-Engineering Surveying Institute, Qingdao 266101, China
3.
Qingdao Institute of Marine Geology, China Geological Survey, Qingdao 266237, China

摘要

摘要:
胶州湾为青岛市的半封闭海湾，对湾内基底岩石属性等的基础地质认识是青岛城市重大工程建设与未来城市规划的重要依据。本文借助锆石U-Pb测年的方法，在胶州湾区钻孔岩芯中首次发现新元古代变花岗岩质基底，其形成时代为约772 Ma，与区域上苏鲁造山带内广泛分布的新元古代花岗岩同期。钻孔内新元古代变花岗岩下部为早白垩世花岗岩侵入，花岗岩时代为约120 Ma，与毗邻的崂山花岗岩等岩体时代一致。钻孔岩芯中早白垩世花岗岩锆石与新元古代变花岗岩锆石的微量元素分布特征相似，但其含量值范围更窄。胶州湾区早白垩世花岗岩岩浆可能源自新元古代花岗质岩石的重熔。借助锆石Ti温度计计算获得胶州湾内新元古代变花岗岩与早白垩世花岗岩岩浆结晶温度均超过750 ℃，表明锆石结晶的岩浆源区呈水不饱和状态，暗示两期岩浆活动的动力学机制可能均与洋壳俯冲对应的“大地幔楔”模式无关。
- 新元古代变花岗岩 /
- 早白垩世花岗岩 /
- 基底岩系 /
- 胶州湾
Abstract:
Jiaozhou Bay is a semi-enclosed bay in Qingdao City in Shandong Peninsula, East China. Understanding the main geological frame of the basement rocks in the bay is crucial for large engineering projects and future urban planning in Qingdao. In this study, Neoproterozoic metamorphic granites (ca. 772 Ma) was discovered for the first time from drilling cores in Jiaozhou Bay .The basement rock is contemporaneous with Neoproterozoic granites that widely distributed in the Sulu orogenic belt. The lower part of the Neoproterozoic metamorphic granites in drilling cores was intruded by Early Cretaceous granites in age of ca. 120 Ma, which is consistent with the ages of adjacent Laoshan granites. The trace element distribution patterns of zircons in the Early Cretaceous granites and Neoproterozoic metamorphic granites in the drilling cores of Jiaozhou Bay are similar but showing a narrower range. The Early Cretaceous granite magma in the Jiaozhou Bay area might be derived from the remelting of Neoproterozoic granitic rocks. The crystallization temperatures of the Neoproterozoic metamorphic granites and Early Cretaceous granites determined by using zircon-Ti thermometer are both higher than 750°C, indicating that the source magma were water-undersaturated. This results suggest that the dynamic mechanisms of the two magmatic events may not be related to the oceanic subduction-related "Big mantle wedge" model.
- Neoproterozoic metagranite /
- early Cretaceous granite /
- basement rocks /
- Jiaozhou Bay

HTML全文

图 1 胶州湾及邻区基岩地质简图

陆区基岩岩性据山东省地质调查院^[10]修改；胶州湾区基底岩性据李官保等^[6]修改。

Figure 1. Sketched geological map of the basement rocks in Jiaozhou Bay and adjacent areas

Modified after references [6,10].

下载: 全尺寸图片幻灯片

图 2 钻孔剖面构造与样品镜下特征

a：胶州湾JZW1与QDQZ1钻孔剖面与取样位置示意图（据窦衍光等^[9]修改）；b：JZW1孔不同深度岩石镜下薄片特征，Kfs=钾长石，Mc=微斜长石，Pth=条纹长石，Bt=黑云母，Qtz=石英。

Figure 2. Sampling locations of borehole profile and photomicrographs of samples

a: Profile and sampling locations of JZW1 and QDQZ1 boreholes in Jiaozhou Bay (modified after reference [9]); b: photomicrographs of rocks at different depths of JZW1 borehole. Kfs: K-feldspar; Mc: microcline; Pth: perthite; Bt: biotite; Qtz: quartz.

下载: 全尺寸图片幻灯片

图 3 JZW1与QDQZ1钻孔5件样品锆石U-Pb协和图、加权平均年龄及代表性锆石CL图

Figure 3. Concordia diagrams, weighted mean ages, and typical cathodoluminescene (CL) images of zircons from JZW1 core and QDQZ1 core in Jiaozhou Bay

下载: 全尺寸图片幻灯片

图 4 胶州湾早白垩世花岗岩与新元古代变花岗岩中锆石的Th/U比值

Figure 4. Th/U ratios of zircons from ther Early Cretaceous granite and Neoproterozoic metagranite in Jiaozhou Bay

下载: 全尺寸图片幻灯片

图 5 胶州湾早白垩世花岗岩与新元古代变花岗岩中锆石的稀土元素特征

标准化数据为原始地幔值，据文献[20]。

Figure 5. Rare earth element distribution pattern of zircons from Early Cretaceous granite and Neoproterozoic metagranite in Jiaozhou Bay

The primitive mantle values are from reference [20].

下载: 全尺寸图片幻灯片

图 6 锆石Ti温度计计算获得的胶州湾早白垩世花岗岩（a）与新元古代变花岗岩（b）锆石晶出的温度分布图

Figure 6. Ti-in-zircon thermometer results for the Early Cretaceous granite and Neoproterozoic metagranite in Jiaozhou Bay

下载: 全尺寸图片幻灯片

图 7 胶州湾早白垩世花岗岩与新元古代变花岗岩锆石来源岩浆属性判别

底图据文献[40]。

Figure 7. Discriminant diagrams with continental and ocean crust zircon fields for zircons from Early Cretaceous granite and Neoproterozoic metagranite in Jiaozhou Bay

Modified after reference [40].

下载: 全尺寸图片幻灯片

图 8 胶州湾早白垩世花岗岩与新元古代变花岗岩中锆石来源岩石类型判别图

底图据文献[42]。

Figure 8. The fields of zircon compositions used as discriminants for different rocks types

Modified after reference [42].

下载: 全尺寸图片幻灯片

1 胶州湾JZW1孔与QDQZ1孔样品锆石测年结果

1 Zircon U-Pb dating results of samples from JZW1 core and QDQZ1 core in Jiaozhou Bay

点号	Th /10⁻⁶	U /10⁻⁶	Th/U	比值						年龄/Ma						谐和度^* /%
点号	Th /10⁻⁶	U /10⁻⁶	Th/U	²⁰⁷Pb/²⁰⁶Pb	± 1σ	²⁰⁷Pb/²³⁵U	± 1σ	²⁰⁶Pb/²³⁸U	± 1σ	²⁰⁷Pb/²⁰⁶Pb	± 1σ	²⁰⁷Pb/²³⁵U	± 1σ	²⁰⁶Pb/²³⁸U	± 1σ	谐和度^* /%
JZW-01-01	669.7	229.7	2.7	1.4403	0.0361	0.12829	0.00169	0.08322	0.00179	778	10	906	15	1274	41	86
JZW-01-02	360.3	296.9	1.2	1.29226	0.02745	0.13871	0.00211	0.06878	0.00111	837	12	842	12	891	33	99
JZW-01-03	181.3	111.7	1.5	1.11424	0.0245	0.12849	0.00133	0.06523	0.0015	779	8	760	12	781	47	103
JZW-01-04	332.3	395.9	0.8	1.06176	0.01795	0.11616	0.00123	0.06722	0.00116	708	7	735	9	844	35	96
JZW-01-05	113.0	58.1	1.8	1.16269	0.03986	0.1312	0.00188	0.06609	0.0022	795	11	783	19	808	68	102
JZW-01-06	402.5	263.9	1.4	1.07708	0.01994	0.11961	0.00134	0.06801	0.00124	728	8	742	10	868	37	98
JZW-01-07	80.9	69.9	1.1	1.14929	0.03557	0.1294	0.00178	0.06811	0.00221	784	10	777	17	871	66	101
JZW-01-08	287.2	225.1	1.2	1.12284	0.02266	0.12253	0.0013	0.06733	0.00135	745	7	764	11	847	41	98
JZW-01-09	322.9	290.8	1.0	1.1426	0.01936	0.13163	0.00136	0.06661	0.0011	797	8	774	9	825	34	103
JZW-01-10	303.5	309.3	0.9	1.25712	0.02953	0.14369	0.00255	0.06766	0.00108	865	14	827	13	857	33	105
JZW-01-11	514.9	318.4	1.5	1.17837	0.02322	0.135	0.00191	0.06656	0.00126	816	11	791	11	823	39	103
JZW-01-12	320.2	239.9	1.3	1.24712	0.03392	0.12463	0.00171	0.07067	0.00153	757	10	822	15	947	44	92
JZW-01-13	626.9	402.6	1.4	1.17282	0.02055	0.13259	0.00185	0.06657	0.00096	803	11	788	10	824	30	102
JZW-01-14	114.4	110.8	1.0	1.17701	0.02845	0.12999	0.00165	0.06834	0.00148	788	9	790	13	878	44	100
JZW-01-15	236.7	207.2	1.0	1.14284	0.02036	0.13008	0.0018	0.06462	0.00125	788	10	774	10	761	40	102
JZW-01-16	248.0	158.1	1.5	1.10722	0.03494	0.12474	0.00164	0.06784	0.00159	758	9	757	17	863	48	100
JZW-01-17	544.4	389.4	1.3	1.17504	0.02037	0.13119	0.00193	0.06634	0.0011	795	11	789	10	816	34	101
JZW-01-18	201.0	195.8	0.9	1.21819	0.02411	0.13051	0.00164	0.06686	0.0012	791	9	809	11	832	37	98
JZW-01-19	202.1	185.9	1.0	1.04561	0.03018	0.12031	0.00167	0.06388	0.00145	732	10	727	15	737	47	101
JZW-01-20	174.2	129.6	1.3	1.17847	0.03521	0.12686	0.0016	0.06758	0.00179	770	9	791	16	855	54	97
JZW-01-21	731.5	293.6	2.4	1.16334	0.02313	0.13009	0.00162	0.06635	0.00108	788	9	784	11	817	34	101
JZW-01-22	391.5	243.5	1.5	1.05473	0.01869	0.12302	0.00133	0.06475	0.00143	748	8	731	9	765	46	102
JZW-01-23	941.0	567.3	1.6	1.10458	0.0197	0.12339	0.0014	0.06448	0.00094	750	8	756	10	757	31	99
JZW-01-24	375.6	172.4	2.0	1.20271	0.02918	0.12569	0.00157	0.07023	0.00141	763	9	802	13	934	41	95
JZW-01-25	220.1	212.9	1.0	1.15278	0.025	0.12685	0.00157	0.06575	0.00135	770	9	779	12	798	43	99
JZW-01-26	224.3	278.6	0.8	1.14376	0.02252	0.13061	0.00151	0.06471	0.00118	791	9	774	11	764	38	102
JZW-01-27	503.9	379.1	1.3	1.00595	0.02033	0.11154	0.00131	0.06527	0.00097	682	8	707	10	782	31	96
JZW-01-28	283.3	291.5	0.9	1.16308	0.02477	0.13435	0.00192	0.065	0.0011	813	11	783	12	773	35	104
JZW-01-29	266.5	181.5	1.4	1.19534	0.02468	0.13404	0.00216	0.06648	0.00107	811	12	798	11	821	33	102
JZW-01-30	211.1	232.8	0.9	1.13833	0.01842	0.12606	0.00142	0.06625	0.00099	765	8	772	9	813	31	99
JZW-02-01	143.0	204.9	0.6	1.19795	0.02529	0.13154	0.00204	0.06637	0.00151	797	12	800	12	817	47	100
JZW-02-02	176.1	206.8	0.8	1.07629	0.02166	0.1285	0.00163	0.06131	0.00142	779	9	742	11	649	49	105
JZW-02-03	52.9	36.8	1.3	1.13787	0.03702	0.12761	0.00195	0.06435	0.00234	774	11	772	18	752	75	100
JZW-02-04	120.8	140.7	0.8	1.13268	0.02611	0.13418	0.0021	0.06163	0.00153	812	12	769	12	660	52	106
JZW-02-05	103.4	236.8	0.4	1.08885	0.02295	0.11893	0.00151	0.06538	0.0012	724	9	748	11	786	38	97
JZW-02-06	106.5	70.5	1.4	1.23326	0.04417	0.13935	0.00212	0.06199	0.00176	841	12	816	20	673	60	103
JZW-02-07	176.4	197.4	0.8	1.11315	0.02228	0.12891	0.00169	0.06353	0.00107	782	10	760	11	725	35	103
JZW-02-08	187.0	184.8	0.9	1.12112	0.0261	0.12631	0.00134	0.06359	0.0011	767	8	764	13	727	36	100
JZW-02-09	145.8	97.3	1.4	1.21582	0.03101	0.13081	0.00142	0.06633	0.0016	792	8	808	14	816	50	98
JZW-02-10	155.1	109.6	1.3	1.11421	0.02713	0.12305	0.00133	0.06637	0.00185	748	8	760	13	817	57	98
JZW-02-11	151.5	118.2	1.2	1.21528	0.0277	0.12958	0.00128	0.06747	0.00158	785	7	808	13	852	48	97
JZW-02-12	53.4	37.2	1.4	1.24489	0.03938	0.13882	0.00247	0.06637	0.00214	838	14	821	18	817	66	102
JZW-02-13	174.3	236.7	0.7	1.13792	0.02494	0.12703	0.0016	0.0662	0.00123	771	9	772	12	812	38	100
JZW-02-14	231.9	120.5	1.8	1.15105	0.02571	0.12865	0.00215	0.06579	0.00135	780	12	778	12	799	42	100
JZW-02-15	76.6	61.9	1.2	1.25943	0.03937	0.13147	0.0021	0.07087	0.00232	796	12	828	18	953	65	96
JZW-02-16	147.1	146.6	0.9	1.19843	0.03005	0.13076	0.00198	0.06568	0.00175	792	11	800	14	795	55	99
JZW-02-17	98.2	66.3	1.4	1.14363	0.03052	0.13033	0.00162	0.06363	0.00179	790	9	774	14	728	59	102
JZW-02-18	246.0	311.2	0.7	1.14949	0.02042	0.12832	0.00171	0.06507	0.00094	778	10	777	10	776	30	100
JZW-02-19	244.6	264.8	0.9	1.1237	0.02198	0.1273	0.00178	0.06603	0.00126	772	10	765	11	806	39	101
JZW-02-20	116.3	111.2	1.0	1.1599	0.0233	0.12832	0.00155	0.06648	0.00132	778	9	782	11	821	41	99
JZW-02-21	264.1	292.1	0.8	1.10176	0.02056	0.12749	0.00171	0.06503	0.00115	774	10	754	10	774	37	103
JZW-02-22	124.1	111.3	1.0	1.13004	0.029	0.13189	0.00168	0.06471	0.00174	799	10	768	14	764	56	104
JZW-02-23	95.1	106.6	0.8	1.13791	0.02724	0.12635	0.00188	0.06567	0.00172	767	11	772	13	795	54	99
JZW-02-24	442.2	512.8	0.8	1.07005	0.02297	0.11248	0.0016	0.06927	0.00118	687	9	739	11	906	35	93
JZW-02-25	80.0	56.0	1.3	1.13451	0.04302	0.12697	0.00129	0.06809	0.00239	771	7	770	20	870	71	100
JZW-02-26	178.1	185.0	0.9	1.12234	0.02397	0.12189	0.00162	0.06634	0.00125	741	9	764	11	816	39	97
JZW-02-27	586.6	477.5	1.1	1.10374	0.01803	0.11915	0.00136	0.06827	0.00095	726	8	755	9	876	29	96
JZW-02-28	265.7	373.1	0.7	1.1319	0.02094	0.12604	0.00154	0.06648	0.00109	765	9	769	10	821	34	99
JZW-02-29	101.9	160.6	0.6	1.11472	0.02824	0.12306	0.0012	0.06517	0.00153	748	7	760	14	779	48	98
JZW-02-30	190.5	279.3	0.6	1.1677	0.02645	0.13415	0.00204	0.06651	0.0011	812	12	786	12	822	34	103
JZW-03-01	209.4	156.8	1.3	0.13707	0.00816	0.0191	0.00035	0.05218	0.003	122	2	130	7	292	126	94
JZW-03-02	404.7	216.9	1.8	0.13236	0.00634	0.01838	0.00027	0.05076	0.00233	117	2	126	6	229	103	93
JZW-03-03	175.2	147.5	1.1	0.12284	0.00721	0.01984	0.00037	0.04611	0.00262	127	2	118	7	2	131	108
JZW-03-04	325.1	236.8	1.3	0.11865	0.00672	0.01831	0.00036	0.04819	0.00266	117	2	114	6	107	125	103
JZW-03-05	257.4	195.6	1.2	0.23283	0.00754	0.02016	0.00027	0.08039	0.00261	129	2	213	6	1206	63	61
JZW-03-06	113.8	112.5	1.0	0.14019	0.00809	0.01943	0.0003	0.05198	0.00291	124	2	133	7	283	123	93
JZW-03-07	243.4	109.2	2.2	0.1479	0.00998	0.02008	0.00045	0.05666	0.00359	128	3	140	9	477	134	91
JZW-03-08	93.0	58.1	1.5	0.18842	0.01191	0.01843	0.0005	0.07909	0.00486	118	3	175	10	1174	117	67
JZW-03-09	290.6	250.8	1.1	0.12809	0.00597	0.01882	0.00036	0.04727	0.00215	120	2	122	5	62	105	98
JZW-03-10	183.0	161.3	1.1	0.11894	0.00682	0.01891	0.00032	0.04861	0.00269	121	2	114	6	128	125	106
JZW-03-11	180.5	88.6	2.0	0.14062	0.0085	0.01866	0.0003	0.04904	0.00291	119	2	134	8	149	133	89
JZW-03-12	589.2	375.6	1.5	0.22686	0.00804	0.02045	0.00035	0.0821	0.00275	131	2	208	7	1247	64	63
JZW-03-13	233.1	183.2	1.2	0.12703	0.00742	0.01964	0.0003	0.04454	0.00252	125	2	121	7	-1	52	103
JZW-03-14	292.4	199.7	1.4	0.11298	0.00548	0.01839	0.0003	0.04497	0.00211	117	2	109	5	-1	53	107
JZW-03-15	584.5	267.7	2.1	0.12041	0.00418	0.01854	0.0003	0.04807	0.00173	118	2	115	4	101	83	103
JZW-03-16	302.5	230.0	1.2	0.12295	0.00583	0.01933	0.00031	0.0473	0.00221	123	2	118	5	63	108	104
JZW-03-17	196.7	168.0	1.1	0.13463	0.0081	0.01889	0.00032	0.04908	0.00283	121	2	128	7	150	130	95
JZW-03-18	54.1	48.1	1.1	0.11902	0.01272	0.01955	0.0008	0.04414	0.00522	125	5	114	12	-1	165	110
JZW-03-19	108.5	44.9	2.3	0.21171	0.01382	0.0181	0.00045	0.08062	0.00519	116	3	195	12	1211	122	59
JZW-03-20	53.5	54.0	0.9	0.10579	0.00879	0.01824	0.00048	0.0405	0.00355	117	3	102	8	-1	108	115
JZW-03-21	245.9	193.0	1.2	0.13134	0.0081	0.01834	0.00029	0.05187	0.00306	117	2	125	7	278	130	94
JZW-03-22	335.2	216.3	1.4	0.14951	0.00538	0.01866	0.00024	0.05656	0.00199	119	2	141	5	474	76	84
JZW-03-23	395.9	260.0	1.4	0.14816	0.00757	0.01937	0.00036	0.05778	0.00288	124	2	140	7	521	106	89
JZW-03-24	607.2	403.9	1.4	0.13661	0.00619	0.01933	0.00031	0.05374	0.00224	123	2	130	6	359	92	95
JZW-03-25	224.4	147.7	1.5	0.12756	0.0078	0.01859	0.00031	0.05088	0.00297	119	2	122	7	235	129	98
JZW-03-26	593.3	365.9	1.5	0.14599	0.00583	0.01948	0.00034	0.05438	0.00186	124	2	138	5	386	75	90
JZW-03-27	348.8	226.7	1.4	0.1106	0.0049	0.01843	0.00024	0.04237	0.00185	118	2	107	4	-1	98	110
JZW-03-28	234.7	173.2	1.3	0.10853	0.00522	0.01859	0.00033	0.04466	0.00214	119	2	105	5	-1	39	113
JZW-03-29	401.6	231.2	1.6	0.12443	0.00626	0.01825	0.00034	0.04847	0.00237	117	2	119	6	121	111	98
JZW-03-30	139.2	92.7	1.4	0.22629	0.01376	0.01978	0.00036	0.08446	0.00495	126	2	207	11	1302	110	61
JZW-04-01	288.8	215.9	1.2	1.27024	0.0335	0.1281	0.00182	0.0708	0.00167	777	10	833	15	951	47	93
JZW-04-02	726.9	377.5	1.8	1.08527	0.01967	0.12201	0.00135	0.06416	0.00107	742	8	746	10	746	35	99
JZW-04-03	883.8	480.5	1.7	1.14052	0.02766	0.13159	0.00205	0.06256	0.00105	797	12	773	13	692	36	103
JZW-04-04	923.2	624.1	1.4	1.09263	0.02082	0.12658	0.0017	0.0634	0.00101	768	10	750	10	721	33	102
JZW-04-05	851.7	597.6	1.3	1.12713	0.01547	0.13124	0.00161	0.06269	0.00085	795	9	766	7	697	29	104
JZW-04-06	2572.6	1412.2	1.7	0.76492	0.01399	0.08792	0.00134	0.06162	0.00076	543	8	577	8	660	26	94
JZW-04-07	398.1	308.5	1.2	1.15906	0.02353	0.13774	0.00203	0.06211	0.00105	832	11	782	11	677	36	106
JZW-04-08	144.2	102.7	1.3	1.17651	0.04646	0.11953	0.00241	0.0754	0.00285	728	14	790	22	1078	74	92
JZW-04-09	477.7	321.9	1.4	1.08343	0.02055	0.12786	0.00163	0.06229	0.00116	776	9	745	10	683	39	104
JZW-04-10	184.0	176.6	1.0	1.15229	0.02225	0.12885	0.00183	0.06392	0.00113	781	10	778	11	738	37	100
JZW-04-11	236.4	222.8	1.0	1.13853	0.0245	0.12944	0.0017	0.06391	0.00123	785	10	772	12	738	40	102
JZW-04-12	559.8	464.0	1.1	1.12519	0.02579	0.12851	0.00115	0.06344	0.00102	779	7	765	12	722	34	102
JZW-04-13	1466.6	900.6	1.5	0.83189	0.01283	0.08931	0.00072	0.06424	0.0009	551	4	615	7	749	29	90
JZW-04-14	611.2	400.2	1.4	1.16212	0.02293	0.12807	0.00113	0.06553	0.00121	777	6	783	11	790	38	99
JZW-04-15	513.2	412.5	1.2	2.03348	0.07396	0.13809	0.00403	0.10331	0.00289	834	23	1127	25	1684	51	74
JZW-04-16	988.6	810.0	1.2	1.07833	0.01777	0.12206	0.0013	0.06346	0.0009	742	7	743	9	723	30	100
JZW-04-17	482.8	342.3	1.3	1.17701	0.02459	0.1298	0.00179	0.06674	0.00122	787	10	790	11	829	38	100
JZW-04-18	135.2	109.2	1.2	1.09585	0.04017	0.12707	0.00153	0.06101	0.00167	771	9	751	19	639	58	103
JZW-04-19	1159.2	854.2	1.3	0.93626	0.01841	0.10705	0.00151	0.06294	0.00095	656	9	671	10	705	32	98
JZW-04-20	1207.3	841.4	1.3	1.10951	0.02476	0.1305	0.00278	0.06191	0.00094	791	16	758	12	670	32	104
JZW-04-21	589.9	359.8	1.6	1.11879	0.02119	0.12444	0.00116	0.06445	0.00099	756	7	762	10	756	32	99
JZW-04-22	478.1	344.8	1.4	1.23183	0.02607	0.12742	0.00136	0.07067	0.00154	773	8	815	12	947	44	95
JZW-04-23	477.3	423.7	1.1	1.16814	0.0187	0.13019	0.00155	0.06504	0.00113	789	9	786	9	775	36	100
JZW-04-24	312.3	308.6	1.0	1.26999	0.02832	0.12659	0.0017	0.07127	0.00142	768	10	832	13	964	40	92
JZW-04-25	889.6	435.8	2.0	1.25961	0.02825	0.12675	0.00166	0.07326	0.00139	769	10	828	13	1020	38	93
JZW-04-26	1230.5	715.8	1.3	0.83103	0.01937	0.08349	0.00143	0.07239	0.00118	517	9	614	11	996	33	84
JZW-04-27	827.7	495.9	1.6	1.11584	0.02	0.11736	0.00112	0.06555	0.00093	715	6	761	10	791	29	94
JZW-04-28	1194.1	822.9	1.4	0.88285	0.01663	0.09454	0.00107	0.0657	0.00106	582	6	643	9	796	33	91
JZW-04-29	1481.5	1151.4	1.3	0.95564	0.01789	0.09343	0.00111	0.07331	0.00117	576	7	681	9	1022	32	85
JZW-04-30	297.9	251.5	1.1	1.18307	0.02795	0.12986	0.0015	0.06786	0.00139	787	9	793	13	863	42	99
JZW-05-01	73.3	51.0	1.3	0.12365	0.0092	0.01843	0.00042	0.0501	0.00378	118	3	118	8	199	167	100
JZW-05-02	145.4	135.1	1.0	0.14137	0.00577	0.01899	0.00039	0.05226	0.00205	121	2	134	5	296	87	90
JZW-05-03	381.3	269.1	1.3	0.14914	0.00563	0.01887	0.00032	0.05997	0.00244	121	2	141	5	602	86	86
JZW-05-04	259.5	163.9	1.5	0.12501	0.00582	0.0182	0.00027	0.04941	0.00238	116	2	120	5	166	109	97
JZW-05-05	230.3	175.6	1.2	0.12433	0.00461	0.01836	0.00025	0.05034	0.00297	117	2	119	4	210	131	98
JZW-05-06	203.7	172.7	1.1	0.12457	0.00579	0.01812	0.00028	0.04843	0.00232	116	2	119	5	119	109	97
JZW-05-07	200.9	173.7	1.1	0.12748	0.00545	0.01929	0.0003	0.0495	0.00229	123	2	122	5	170	105	101
JZW-05-08	428.9	241.1	1.6	0.12047	0.00566	0.01825	0.00023	0.04533	0.00215	117	1	116	5	-1	73	101
JZW-05-09	207.5	163.7	1.2	0.15246	0.0088	0.0189	0.00027	0.05746	0.00346	121	2	144	8	508	127	84
JZW-05-10	225.0	177.4	1.2	0.12733	0.00584	0.01897	0.0003	0.04729	0.0023	121	2	122	5	63	112	99
JZW-05-11	796.7	348.8	2.1	0.12137	0.00593	0.01807	0.0002	0.04818	0.00245	115	1	116	5	107	116	99
JZW-05-12	168.9	108.7	1.4	0.11255	0.00766	0.01861	0.00043	0.0481	0.00336	119	3	108	7	103	158	110
JZW-05-13	40.4	35.4	1.1	0.19981	0.01694	0.01882	0.0005	0.06945	0.00722	120	3	185	14	911	201	65
JZW-05-14	67.0	51.1	1.2	0.12462	0.01016	0.01838	0.00041	0.05326	0.00418	117	3	119	9	339	169	98
JZW-05-15	455.7	247.6	1.7	0.25707	0.01112	0.01887	0.00029	0.09185	0.00381	121	2	232	9	1463	77	52
JZW-05-16	459.5	305.1	1.4	0.23588	0.00908	0.01816	0.00022	0.09596	0.00375	116	1	215	7	1546	72	54
JZW-05-17	300.4	205.5	1.3	0.12443	0.0061	0.01832	0.00031	0.04721	0.00236	117	2	119	6	59	115	98
JZW-05-18	185.6	167.9	1.0	0.12405	0.0059	0.01855	0.00027	0.04886	0.00239	118	2	119	5	140	111	99
JZW-05-19	153.0	145.8	1.0	0.1203	0.00804	0.01898	0.00033	0.04433	0.00296	121	2	115	7	-1	64	105
JZW-05-20	169.5	158.1	1.0	0.15622	0.00774	0.01857	0.00038	0.06266	0.00317	119	2	147	7	696	104	81
JZW-05-21	228.2	139.2	1.5	0.12757	0.00807	0.01899	0.0003	0.04665	0.00297	121	2	122	7	30	146	99
JZW-05-22	148.4	133.4	1.0	0.1213	0.0068	0.01973	0.00046	0.04619	0.00268	126	3	116	6	7	134	109
JZW-05-23	330.6	228.0	1.3	0.30474	0.01123	0.0174	0.00034	0.13388	0.00489	111	2	270	9	2149	62	41
JZW-05-24	226.6	179.5	1.1	0.13651	0.00658	0.01818	0.00028	0.052	0.00259	116	2	130	6	285	110	89
JZW-05-25	202.2	165.4	1.1	0.13994	0.00529	0.0181	0.0003	0.05257	0.00199	116	2	133	5	309	84	87
JZW-05-26	337.7	179.1	1.7	0.12719	0.00525	0.01819	0.00023	0.04974	0.00226	116	1	122	5	182	102	95
JZW-05-27	277.8	201.1	1.3	0.14816	0.00727	0.0186	0.00028	0.05553	0.00278	119	2	140	6	432	108	85
JZW-05-28	159.6	130.6	1.1	0.1291	0.00634	0.018	0.0003	0.05429	0.00275	115	2	123	6	382	110	93
JZW-05-29	581.6	381.2	1.4	0.12592	0.00403	0.01865	0.00024	0.04801	0.00164	119	1	120	4	99	79	99
JZW-05-30	274.3	147.2	1.7	0.26374	0.0108	0.02078	0.0004	0.09157	0.0038	133	3	238	9	1458	77	56
*谐和度 =（206Pb/ 238U age×100）/（207Pb/206Pb age）

下载: 导出CSV

2 胶州湾JZW1孔与QDQZ1孔样品锆石微量元素测试结果

2 Trace element compositions of zircons from JZW1 core and QDQZ1 core in Jiaozhou Bay 10⁻⁶

点号	La	Ce	Pr	Nd	Sm	Eu	Gd	Tb	Dy	Ho	Er	Tm	Yb	Lu	Hf	Ti
JZW-01-01	1018.09	2075.51	209.84	700.39	123.60	7.21	106.09	17.29	148.03	48.66	230.11	47.25	446.87	96.28	8052.23	24.80
JZW-01-02	3.64	66.44	0.93	5.63	4.52	1.14	21.80	7.36	96.28	38.25	198.57	42.76	412.08	87.53	9254.33	3.41
JZW-01-03	4.53	87.43	1.06	7.26	8.63	3.12	45.14	15.05	191.01	74.22	368.59	74.11	665.69	137.95	7046.69	14.24
JZW-01-04	0.24	55.89	0.13	1.63	4.57	1.11	30.39	11.65	161.82	67.53	360.79	79.61	757.69	162.57	10077.28	48.92
JZW-01-05	0.02	73.03	0.25	4.05	6.89	2.98	36.12	11.38	147.00	57.44	276.73	55.21	494.19	104.33	6370.91	19.33
JZW-01-06	0.00	58.25	0.08	1.73	3.55	1.25	20.08	6.89	88.58	35.00	177.06	38.18	360.21	78.81	8838.92	3.16
JZW-01-07	0.00	37.76	0.09	1.47	3.56	1.07	19.99	6.74	86.21	34.30	173.22	36.87	346.69	74.27	8095.71	8.04
JZW-01-08	0.01	55.77	0.09	1.46	3.31	1.13	19.06	6.56	86.20	34.44	177.99	38.53	372.08	80.12	8737.96	2.91
JZW-01-09	0.02	71.61	0.08	1.71	4.07	0.78	25.13	9.00	119.12	47.61	245.09	52.46	491.79	102.57	9632.82	3.44
JZW-01-10	0.01	42.09	0.12	2.29	5.82	1.64	32.21	11.55	150.67	61.01	309.88	67.80	643.55	137.84	9143.00	1.85
JZW-01-11	0.01	75.99	0.14	2.13	4.69	1.54	26.76	8.72	112.62	44.97	230.28	48.87	468.99	100.49	8474.57	4.47
JZW-01-12	0.02	57.95	0.08	1.66	3.48	1.32	20.43	6.75	91.29	36.44	190.87	41.86	411.42	90.22	8605.37	5.45
JZW-01-13	0.00	82.33	0.08	1.76	4.73	1.63	29.24	10.17	136.52	54.45	286.03	61.66	594.76	128.63	9000.23	3.57
JZW-01-14	3.73	54.24	1.23	6.38	3.49	0.54	15.33	5.38	75.17	31.17	166.90	36.58	350.50	75.75	10111.06	4.10
JZW-01-15	0.02	50.48	0.09	1.47	3.27	1.21	20.24	6.70	88.56	36.79	195.86	44.65	436.12	98.56	8698.54	3.72
JZW-01-16	0.01	59.89	0.11	2.09	4.00	1.43	23.11	7.74	98.55	38.13	186.74	39.06	354.25	75.12	8340.87	7.31
JZW-01-17	0.00	62.88	0.08	1.30	3.43	1.23	24.48	8.60	111.23	43.86	222.51	47.91	454.96	95.76	9492.71	3.99
JZW-01-18	2.17	58.68	1.10	5.52	3.21	0.55	17.41	6.70	94.49	39.13	209.79	45.88	431.31	88.85	10484.49	3.68
JZW-01-19	9.33	81.49	4.22	20.28	8.71	1.83	26.68	8.05	104.69	41.82	221.93	49.04	479.65	106.59	8607.39	4.14
JZW-01-20	3.07	59.16	0.93	4.75	3.76	1.05	19.55	6.73	90.32	36.51	186.64	39.91	376.43	79.29	9124.39	6.07
JZW-01-21	0.03	117.63	0.24	4.12	8.02	3.09	43.17	13.51	169.87	65.16	320.43	66.85	622.62	131.89	7828.62	7.20
JZW-01-22	0.11	68.52	0.12	2.01	4.31	1.69	24.70	8.02	106.18	42.30	221.71	47.93	465.41	101.50	8230.45	4.99
JZW-01-23	0.00	85.87	0.10	1.74	5.18	1.61	31.95	11.21	146.16	57.07	284.68	60.24	562.62	118.09	9432.92	2.15
JZW-01-24	0.07	95.21	0.16	2.87	5.60	2.24	31.88	10.55	133.43	50.45	251.83	51.79	471.84	99.21	8692.12	9.84
JZW-01-25	0.00	64.60	0.07	1.56	3.49	1.27	21.26	7.45	101.75	42.06	228.92	50.94	500.73	111.57	8713.45	4.53
JZW-01-26	0.00	62.96	0.05	1.33	3.70	1.18	23.70	8.68	119.98	51.82	284.44	64.26	633.78	141.76	9036.02	3.37
JZW-01-27	0.03	61.97	0.09	1.71	4.02	1.28	22.04	7.45	99.01	39.34	206.82	46.56	459.51	102.76	8961.60	3.52
JZW-01-28	0.00	67.75	0.06	1.50	4.05	1.26	24.60	8.84	121.21	50.59	272.18	60.42	592.67	131.61	8922.28	4.10
JZW-01-29	0.14	78.17	0.17	2.48	4.85	1.74	26.54	8.75	112.95	45.67	234.12	51.00	487.63	107.25	8098.04	7.91
JZW-01-30	0.00	62.79	0.08	1.48	3.62	1.23	22.85	7.66	105.86	45.45	249.06	57.14	563.07	126.76	8709.09	4.13
JZW-02-01	0.12	49.71	0.08	1.16	4.18	0.21	29.04	10.74	143.35	55.56	265.62	51.69	450.04	90.98	7097.15	2.46
JZW-02-02	0.00	54.57	0.06	1.46	4.48	0.21	29.53	11.22	144.10	54.76	257.86	49.28	412.54	81.35	7062.30	1.82
JZW-02-03	0.01	29.60	0.08	1.47	2.48	0.99	13.88	4.32	55.05	21.00	105.16	21.79	198.94	43.30	7472.35	8.20
JZW-02-04	0.08	56.37	0.10	1.64	4.47	0.24	31.18	11.15	144.26	54.62	261.13	50.51	433.52	87.24	6949.59	3.17
JZW-02-05	0.10	26.40	0.15	1.19	2.83	0.17	19.18	7.66	102.23	40.07	197.63	41.64	349.63	70.43	7251.57	2.46
JZW-02-06	0.04	80.86	0.19	2.99	5.39	1.89	31.13	9.96	125.22	48.56	230.43	46.23	407.81	86.21	6861.10	7.14
JZW-02-07	0.01	53.26	0.08	1.56	4.67	0.19	30.05	10.95	141.34	53.34	255.35	48.55	412.08	81.10	7234.16	2.49
JZW-02-08	3.24	70.54	1.93	9.19	7.42	0.29	34.90	12.14	152.99	56.94	266.36	51.28	436.50	87.27	6963.91	3.83
JZW-02-09	0.02	53.49	0.09	1.86	3.54	1.20	19.86	6.51	85.12	33.43	167.60	34.80	324.84	69.19	8312.15	5.89
JZW-02-10	0.01	59.63	0.09	2.08	4.08	1.24	23.45	7.84	105.58	42.95	218.20	46.16	425.48	91.52	8312.61	6.59
JZW-02-11	0.02	45.00	0.14	2.16	4.73	2.02	25.27	8.65	114.73	46.81	242.34	52.62	486.04	108.19	7576.30	9.18
JZW-02-12	0.73	45.27	0.46	3.62	4.11	1.29	19.95	5.83	69.88	25.79	123.87	24.76	223.84	48.14	6937.23	11.70
JZW-02-13	0.00	50.18	0.06	1.21	4.04	0.21	29.51	11.26	146.37	55.15	261.19	50.40	423.45	83.00	7406.24	1.82
JZW-02-14	6.35	81.64	1.98	10.65	6.38	2.11	29.91	9.41	118.18	44.94	219.71	45.28	402.97	83.96	7588.86	7.56
JZW-02-15	3.21	43.47	0.99	5.55	4.07	1.38	19.20	6.04	77.30	30.12	151.52	31.66	289.98	63.64	7662.10	8.45
JZW-02-16	26.42	119.13	9.71	41.41	17.34	0.50	55.60	17.41	208.93	76.12	353.16	67.01	560.25	113.03	6822.89	4.33
JZW-02-17	0.02	40.62	0.11	1.72	3.48	0.88	20.23	6.56	84.62	32.75	165.76	34.95	319.99	69.05	8300.78	8.53
JZW-02-18	0.08	59.59	0.07	1.48	5.85	0.24	41.48	15.94	208.23	77.29	365.65	69.62	580.41	112.75	8186.50	3.06
JZW-02-19	0.01	61.01	0.08	1.55	5.77	0.25	36.08	13.43	172.19	65.43	304.10	58.78	492.83	96.28	7474.52	1.80
JZW-02-20	0.65	42.00	0.28	1.72	2.36	0.38	13.99	5.16	70.93	29.28	155.00	32.71	303.13	63.37	10215.00	4.03
JZW-02-21	0.00	63.14	0.05	1.38	4.74	0.22	35.23	13.32	173.73	64.99	306.88	59.05	498.67	95.97	7313.24	3.18
JZW-02-22	1.03	50.82	0.37	2.32	3.02	0.68	16.83	5.89	80.94	33.30	173.22	37.84	351.89	74.92	9649.28	4.31
JZW-02-23	0.00	51.93	0.06	1.36	4.26	0.26	26.27	9.67	124.41	47.61	229.59	45.07	396.13	81.49	6668.52	3.00
JZW-02-24	0.80	89.10	0.56	4.90	10.86	0.48	68.15	24.09	302.13	112.23	522.04	99.72	843.87	164.92	8024.29	6.83
JZW-02-25	0.01	35.16	0.10	1.65	4.04	0.96	19.71	6.28	78.92	30.46	151.88	31.68	290.90	62.72	7941.94	12.87
JZW-02-26	38.50	155.69	10.22	37.82	12.50	0.46	42.86	14.29	173.41	65.56	308.35	59.79	508.39	100.30	6934.72	22.54
JZW-02-27	0.29	127.12	0.31	3.27	8.96	0.45	60.46	22.17	280.88	102.53	481.57	91.50	766.31	149.40	8067.98	7.76
JZW-02-28	0.21	64.97	0.12	1.53	5.48	0.23	39.60	15.56	201.38	77.04	365.15	70.63	591.81	113.93	8365.11	2.09
JZW-02-29	0.01	35.88	0.04	0.57	1.75	0.29	13.29	5.15	72.82	30.17	158.35	33.62	310.18	64.92	11029.09	2.31
JZW-02-30	0.00	56.16	0.07	1.33	4.82	0.19	34.43	13.18	172.56	64.93	307.48	59.72	508.34	99.33	8141.57	2.34
JZW-03-01	104.58	321.33	23.95	80.32	15.96	0.64	28.99	8.61	109.18	44.77	239.64	52.30	484.92	100.55	9688.99	4.36
JZW-03-02	0.17	92.80	0.09	1.12	2.07	0.19	14.47	5.62	85.95	37.98	214.24	48.46	461.03	97.27	10035.95	6.53
JZW-03-03	0.13	70.98	0.10	1.24	2.64	0.26	17.30	6.96	104.17	47.07	268.41	61.68	593.90	127.52	9774.50	2.58
JZW-03-04	0.01	98.59	0.04	1.01	1.98	0.21	14.27	6.03	92.90	43.36	256.37	60.48	597.67	130.00	10018.27	3.09
JZW-03-05	0.09	89.84	0.06	1.13	2.29	0.26	14.72	6.07	88.06	39.73	222.29	50.09	487.60	103.91	10119.18	4.46
JZW-03-06	0.05	45.01	0.06	0.87	1.91	0.18	13.79	5.50	79.98	36.08	201.29	45.99	438.94	93.56	9703.64	2.70
JZW-03-07	0.02	80.63	0.18	3.09	4.85	0.99	24.50	8.08	95.26	35.42	169.66	33.79	297.43	60.20	7259.57	11.75
JZW-03-08	0.04	78.62	0.37	5.57	8.73	1.62	37.99	10.92	127.69	47.43	216.18	41.99	370.15	76.53	6966.70	14.47
JZW-03-09	0.09	104.75	0.07	0.97	2.19	0.25	14.56	6.05	92.44	42.85	252.27	59.73	592.20	129.95	10222.49	2.08
JZW-03-10	0.01	92.08	0.06	0.96	2.81	0.30	18.74	7.65	112.83	50.91	288.99	65.43	629.40	134.46	9641.73	3.19
JZW-03-11	0.01	83.68	0.13	2.59	5.52	1.02	30.14	9.80	122.45	44.35	208.63	40.60	348.34	69.62	7749.77	8.00
JZW-03-12	0.04	136.71	0.12	1.75	3.31	0.68	21.72	8.60	127.95	61.84	383.17	95.65	1008.50	233.21	10210.68	5.50
JZW-03-13	0.00	75.65	0.06	0.82	2.13	0.26	13.70	5.34	79.10	34.98	195.56	44.43	431.49	94.01	10363.22	3.19
JZW-03-14	0.02	89.77	0.06	1.18	2.43	0.28	17.18	6.76	97.48	41.92	227.04	49.90	466.21	98.12	9815.08	4.03
JZW-03-15	0.06	190.42	0.26	3.77	9.70	0.84	54.86	18.67	236.86	91.56	440.76	87.61	767.10	150.77	8964.54	4.95
JZW-03-16	1.43	90.49	0.34	1.70	2.14	0.22	13.44	5.59	82.34	37.45	216.11	50.14	488.85	106.98	10220.57	3.40
JZW-03-17	4.80	98.48	1.01	3.56	2.47	0.27	16.52	6.73	102.95	48.27	282.36	65.59	640.51	139.90	9911.09	3.61
JZW-03-18	0.01	42.55	0.14	2.43	4.70	1.20	21.86	6.59	79.73	29.83	143.74	28.81	259.07	55.50	6884.80	13.66
JZW-03-19	0.03	108.27	0.33	5.10	7.63	2.09	34.67	10.94	134.54	50.07	239.05	46.97	409.98	87.56	6104.11	16.06
JZW-03-20	7.60	64.65	2.61	11.79	5.66	0.98	21.66	6.59	78.88	29.77	143.38	29.30	262.64	55.86	7529.97	9.35
JZW-03-21	0.01	85.44	0.06	0.98	1.91	0.19	12.82	5.21	80.42	36.89	212.57	49.44	479.75	103.86	10154.03	3.37
JZW-03-22	0.00	83.09	0.07	0.98	2.29	0.18	13.57	5.75	82.83	36.79	203.28	45.00	422.53	89.92	9802.70	3.11
JZW-03-23	0.04	108.79	0.09	1.43	3.57	0.47	22.77	8.81	123.24	53.67	293.87	65.27	623.74	131.52	9961.44	4.68
JZW-03-24	0.01	128.19	0.09	0.87	2.12	0.29	14.70	6.02	91.49	44.93	274.41	67.41	681.80	153.00	10502.97	3.76
JZW-03-25	0.01	82.09	0.17	2.68	5.51	0.38	33.71	12.65	176.33	71.31	367.87	76.47	677.36	136.72	9158.01	3.31
JZW-03-26	0.01	108.55	0.07	0.84	1.59	0.23	12.04	5.03	78.54	37.91	232.18	55.86	564.77	126.53	10370.33	2.68
JZW-03-27	0.01	90.35	0.06	0.86	2.02	0.19	13.97	5.58	83.02	37.64	212.50	47.88	453.09	96.84	9747.43	3.12
JZW-03-28	0.11	84.86	0.08	1.17	2.54	0.29	15.95	6.77	99.04	43.56	240.53	54.01	509.62	108.80	9936.16	3.82
JZW-03-29	0.01	124.13	0.10	1.60	3.97	0.29	25.34	10.03	142.58	60.07	316.10	67.22	602.16	123.45	9159.22	4.12
JZW-03-30	0.00	69.24	0.13	2.30	5.18	0.72	28.86	10.07	125.74	47.12	216.98	42.22	350.25	68.20	8256.95	6.90
JZW-04-01	10.98	133.28	4.70	21.88	11.75	1.25	49.49	16.43	206.46	80.27	385.05	77.39	679.07	139.45	8267.47	3.90
JZW-04-02	11.37	156.57	5.38	24.31	14.34	1.21	57.07	18.21	223.35	82.16	383.42	73.46	624.56	123.17	8519.84	4.16
JZW-04-03	0.02	124.92	0.13	2.52	6.96	0.97	49.70	17.37	220.00	82.82	388.07	75.80	654.74	129.38	8831.18	3.57
JZW-04-04	0.05	107.17	0.07	1.29	3.54	0.43	25.77	9.86	141.61	60.62	328.48	72.77	687.68	147.77	10592.43	4.56
JZW-04-05	0.01	175.29	0.16	3.31	9.97	1.26	70.30	24.51	310.94	118.32	558.88	109.82	954.95	190.59	8696.51	3.47
JZW-04-06	2.31	233.28	0.74	4.43	8.15	0.76	57.73	22.02	301.46	125.68	655.73	141.12	1296.06	267.82	10471.40	16.71
JZW-04-07	0.01	79.72	0.07	1.84	6.97	0.87	47.42	17.71	234.54	93.87	460.06	93.58	824.40	166.35	8049.02	2.74
JZW-04-08	0.12	54.22	0.11	2.01	3.96	1.24	19.43	6.08	74.45	28.85	143.82	30.37	283.96	61.46	8116.11	6.03
JZW-04-09	0.06	118.87	0.15	2.85	8.53	1.12	53.97	19.01	243.26	91.73	440.27	87.45	756.82	152.46	8183.57	6.42
JZW-04-10	1.10	50.78	0.35	2.35	2.71	0.63	15.56	5.80	81.66	34.90	192.04	45.68	419.89	91.51	9954.15	2.27
JZW-04-11	0.08	60.23	0.10	1.51	4.82	0.74	34.50	12.91	174.05	69.66	339.41	68.72	618.52	125.46	8616.76	2.80
JZW-04-12	0.10	66.99	0.11	1.22	3.82	0.43	27.46	10.98	154.77	65.89	358.34	79.94	762.57	163.27	9936.60	2.55
JZW-04-13	11.97	171.56	5.26	23.34	10.17	0.63	39.98	13.89	189.94	79.71	419.94	91.83	859.67	181.63	10578.09	10.30
JZW-04-14	65.37	298.78	22.37	101.52	32.55	2.35	85.02	24.36	286.94	105.04	491.43	95.66	824.79	162.26	8480.97	6.04
JZW-04-15	6.79	115.23	4.49	25.02	14.77	1.17	56.54	18.63	235.21	89.19	432.63	87.74	770.86	155.70	8253.51	13.14
JZW-04-16	0.08	143.10	0.10	1.57	4.49	0.43	33.03	13.20	188.02	78.72	430.31	96.19	912.88	196.97	10688.80	4.02
JZW-04-17	8.13	125.60	2.89	13.83	9.52	1.78	42.63	14.84	186.48	71.21	349.84	70.31	627.67	124.93	9154.39	4.07
JZW-04-18	99.95	319.33	32.92	124.85	33.94	2.91	52.05	11.97	128.29	46.46	220.98	46.51	429.63	93.21	8121.98	5.88
JZW-04-19	0.52	145.07	0.34	2.67	5.21	0.45	37.68	14.74	205.22	86.48	461.45	101.44	951.29	198.27	10518.91	9.08
JZW-04-20	0.08	137.48	0.09	1.44	4.50	0.42	31.88	12.67	176.65	75.00	408.63	90.49	865.90	183.19	10703.89	4.38
JZW-04-21	2.05	133.21	1.26	7.90	10.48	1.22	59.34	20.30	252.37	94.63	444.29	87.25	758.64	150.01	8540.00	4.23
JZW-04-22	0.49	84.70	0.25	2.64	5.50	1.06	39.35	14.09	184.25	71.05	350.12	73.39	647.51	131.99	8587.79	4.98
JZW-04-23	0.11	118.60	0.13	2.18	6.76	0.82	47.01	16.70	220.64	84.53	405.59	81.20	721.80	143.89	8768.51	8.39
JZW-04-24	21.44	105.25	5.66	16.59	6.26	0.54	21.75	7.68	104.51	42.90	232.29	51.84	514.12	112.00	10329.94	2808.17
JZW-04-25	0.56	145.56	0.65	5.15	10.22	1.37	62.03	21.59	257.28	92.67	428.98	81.97	708.60	138.17	8311.77	4.35
JZW-04-26	0.18	96.88	0.16	2.06	3.95	1.21	24.04	7.91	103.66	43.35	241.27	58.56	628.70	153.42	9891.64	4.89
JZW-04-27	24.08	210.60	7.57	32.58	14.39	1.56	65.71	21.62	266.03	98.20	458.92	89.47	777.46	154.23	8691.08	13.87
JZW-04-28	1.01	138.07	0.57	4.21	6.61	0.57	39.70	14.90	205.15	83.56	438.19	94.46	881.23	184.71	10204.75	9.06
JZW-04-29	1.93	193.99	0.95	5.27	7.22	0.55	45.36	17.91	252.49	109.41	595.09	132.24	1264.24	265.59	10649.64	12.07
JZW-04-30	35.37	147.57	9.43	39.58	14.17	1.24	51.10	16.83	216.77	83.30	400.43	80.64	720.52	145.29	8072.14	3.62
JZW-05-01	3.52	55.70	1.18	6.79	5.49	1.33	23.57	6.84	78.72	28.61	132.49	25.70	228.90	47.07	6998.19	13.91
JZW-05-02	66.05	207.46	12.01	34.53	7.40	0.48	19.65	6.61	95.47	43.51	247.95	56.03	544.28	115.60	9100.90	3.61
JZW-05-03	0.12	150.49	0.20	2.47	4.23	0.56	25.80	10.69	160.62	71.80	407.86	92.42	885.37	184.43	9345.31	4.44
JZW-05-04	0.53	76.69	0.22	2.64	4.68	0.42	27.21	10.53	149.22	64.82	356.12	77.68	726.64	150.37	9370.79	2.46
JZW-05-05	0.02	103.62	0.07	1.02	2.44	0.20	16.99	7.08	105.03	46.81	264.79	58.50	568.26	117.87	9142.27	3.73
JZW-05-06	0.09	103.82	0.10	1.07	2.66	0.21	18.49	7.74	115.67	51.66	292.12	65.65	636.98	133.88	8976.60	2.95
JZW-05-07	0.03	81.17	0.05	0.96	1.88	0.21	13.53	5.65	84.91	38.64	226.75	51.86	516.92	110.68	9750.69	2.30
JZW-05-08	39.16	225.79	11.62	42.28	11.94	0.49	38.63	13.31	171.08	67.81	345.69	69.54	623.04	121.26	8627.30	3.71
JZW-05-09	0.21	84.22	0.09	1.01	2.00	0.20	13.73	5.60	85.17	38.13	219.47	49.95	487.72	104.37	9242.52	7.32
JZW-05-10	0.69	89.47	0.19	1.51	2.25	0.29	15.84	6.26	93.02	41.90	230.95	51.44	510.79	105.55	9545.73	3.16
JZW-05-11	0.02	130.31	0.11	1.58	3.71	0.41	20.98	7.99	112.68	49.38	269.79	59.22	565.94	118.07	9352.64	3.25
JZW-05-12	0.04	76.73	0.18	3.36	6.28	1.17	30.87	9.68	115.40	41.82	194.90	36.86	321.93	63.52	7503.40	8.37
JZW-05-13	1.79	40.57	0.66	3.93	3.52	1.07	17.39	5.33	64.40	23.70	112.27	22.47	202.84	42.93	6998.19	10.62
JZW-05-14	0.66	48.84	0.33	3.03	4.37	1.26	23.31	7.33	87.03	32.30	153.62	30.04	271.22	56.70	7003.49	10.91
JZW-05-15	0.05	130.81	0.12	1.70	4.54	0.38	31.69	12.24	163.89	64.75	323.48	63.61	568.70	110.20	8744.06	96.47
JZW-05-16	1.55	114.35	0.58	3.30	2.65	0.40	14.91	6.35	90.90	41.05	240.62	56.82	574.96	124.76	10613.62	11.62
JZW-05-17	0.13	105.48	0.11	1.25	2.43	0.20	16.52	6.89	101.80	46.14	259.45	57.74	559.63	116.49	9370.74	2.92
JZW-05-18	0.00	82.78	0.05	0.75	2.08	0.30	14.98	6.27	93.53	42.84	247.67	55.98	555.67	120.49	9649.52	3.92
JZW-05-19	0.01	80.57	0.06	0.96	2.62	0.33	18.22	7.30	107.43	47.87	270.70	60.27	589.80	126.89	9435.65	2.74
JZW-05-20	8.71	104.45	2.31	7.61	3.21	0.33	15.11	6.12	92.77	43.24	253.77	59.23	583.61	127.17	9470.15	3.59
JZW-05-21	0.01	77.44	0.18	2.57	5.66	0.49	33.74	12.07	166.50	69.42	366.97	76.42	693.62	140.40	9343.39	2.52
JZW-05-22	0.00	75.07	0.06	0.87	2.38	0.26	14.64	6.07	87.75	39.06	219.58	49.56	476.16	100.63	9733.09	2.22
JZW-05-23	1.26	86.98	0.34	1.98	2.80	0.31	15.16	6.18	89.07	38.68	213.55	47.83	459.09	96.91	9677.14	10.20
JZW-05-24	0.01	126.17	0.08	1.40	3.07	0.23	22.62	9.35	137.96	61.41	339.00	74.70	694.82	144.57	8805.60	3.66
JZW-05-25	0.00	74.81	0.06	0.95	2.10	0.29	14.64	5.88	84.45	36.56	202.35	45.24	433.01	92.05	10068.98	1.79
JZW-05-26	15.22	157.07	3.59	17.78	17.15	1.83	82.79	27.13	328.20	118.13	539.31	102.02	857.80	165.30	8373.90	4.73
JZW-05-27	3.88	140.22	1.02	5.08	4.97	0.31	30.43	11.90	161.00	65.97	333.79	68.31	602.43	120.86	8710.49	3.78
JZW-05-28	0.03	69.00	0.04	0.76	1.85	0.18	12.35	4.78	72.68	31.85	178.35	39.74	382.00	80.10	9697.32	2.73
JZW-05-29	0.02	126.55	0.08	1.08	2.05	0.24	13.69	5.81	92.59	44.53	273.11	65.87	664.95	147.45	10278.35	1.93
JZW-05-30	72.90	243.84	14.56	48.56	15.56	1.42	52.46	16.10	199.04	74.98	360.71	71.52	614.60	122.51	8529.27	9.80

下载: 导出CSV

3 锆石Ti含量与锆石晶出温度计算结果

3 Ti content in zircon and calculation results of zircon crystallization temperature

点号	Ti/10⁻⁶	$\rm 1a_{SiO_2} $	$\rm 2a_{TiO_2} $	$\rm 3a_{TiO_2} $	$\rm a_{TiO_2} $	1T/℃	2T/℃	3T/℃
JZW-01-01	24.80	1	0.9	0.5	0.3	851	922	992
JZW-01-02	3.41	1	0.9	0.5	0.3	662	711	758
JZW-01-03	14.24	1	0.9	0.5	0.3	791	855	917
JZW-01-04	48.92	1	0.9	0.5	0.3	934	1017	1099
JZW-01-05	19.33	1	0.9	0.5	0.3	823	891	957
JZW-01-06	3.16	1	0.9	0.5	0.3	656	704	751
JZW-01-07	8.04	1	0.9	0.5	0.3	735	792	848
JZW-01-08	2.91	1	0.9	0.5	0.3	650	697	743
JZW-01-09	3.44	1	0.9	0.5	0.3	663	712	759
JZW-01-10	1.85	1	0.9	0.5	0.3	616	660	702
JZW-01-11	4.47	1	0.9	0.5	0.3	684	735	785
JZW-01-12	5.45	1	0.9	0.5	0.3	701	754	805
JZW-01-13	3.57	1	0.9	0.5	0.3	666	715	762
JZW-01-14	4.10	1	0.9	0.5	0.3	677	727	776
JZW-01-15	3.72	1	0.9	0.5	0.3	669	719	766
JZW-01-16	7.31	1	0.9	0.5	0.3	727	783	837
JZW-01-17	3.99	1	0.9	0.5	0.3	675	725	773
JZW-01-18	3.68	1	0.9	0.5	0.3	668	718	765
JZW-01-19	4.14	1	0.9	0.5	0.3	678	728	777
JZW-01-20	6.07	1	0.9	0.5	0.3	710	764	817
JZW-01-21	7.20	1	0.9	0.5	0.3	725	781	835
JZW-01-22	4.99	1	0.9	0.5	0.3	693	746	796
JZW-01-23	2.15	1	0.9	0.5	0.3	627	672	715
JZW-01-24	9.84	1	0.9	0.5	0.3	754	814	871
JZW-01-25	4.53	1	0.9	0.5	0.3	685	737	786
JZW-01-26	3.37	1	0.9	0.5	0.3	661	710	757
JZW-01-27	3.52	1	0.9	0.5	0.3	665	714	761
JZW-01-28	4.10	1	0.9	0.5	0.3	677	727	776
JZW-01-29	7.91	1	0.9	0.5	0.3	734	791	846
JZW-01-30	4.13	1	0.9	0.5	0.3	677	728	777
JZW-02-01	2.46	1	0.9	0.5	0.3	637	683	727
JZW-02-02	1.82	1	0.9	0.5	0.3	615	659	701
JZW-02-03	8.20	1	0.9	0.5	0.3	737	794	850
JZW-02-04	3.17	1	0.9	0.5	0.3	656	705	751
JZW-02-05	2.46	1	0.9	0.5	0.3	637	683	727
JZW-02-06	7.14	1	0.9	0.5	0.3	724	780	834
JZW-02-07	2.49	1	0.9	0.5	0.3	638	684	729
JZW-02-08	3.83	1	0.9	0.5	0.3	671	721	769
JZW-02-09	5.89	1	0.9	0.5	0.3	707	761	813
JZW-02-10	6.59	1	0.9	0.5	0.3	717	772	825
JZW-02-11	9.18	1	0.9	0.5	0.3	748	806	863
JZW-02-12	11.70	1	0.9	0.5	0.3	771	832	892
JZW-02-13	1.82	1	0.9	0.5	0.3	615	659	701
JZW-02-14	7.56	1	0.9	0.5	0.3	730	786	841
JZW-02-15	8.45	1	0.9	0.5	0.3	740	798	853
JZW-02-16	4.33	1	0.9	0.5	0.3	681	732	781
JZW-02-17	8.53	1	0.9	0.5	0.3	741	799	854
JZW-02-18	3.06	1	0.9	0.5	0.3	654	702	748
JZW-02-19	1.80	1	0.9	0.5	0.3	614	658	700
JZW-02-20	4.03					675	726	774
JZW-02-21	3.18					657	705	751
JZW-02-22	4.31	1	0.9	0.5	0.3	681	732	781
JZW-02-23	3.00	1	0.9	0.5	0.3	652	700	746
JZW-02-24	6.83	1	0.9	0.5	0.3	720	776	829
JZW-02-25	12.87	1	0.9	0.5	0.3	780	843	904
JZW-02-26	22.54	1	0.9	0.5	0.3	840	910	978
JZW-02-27	7.76	1	0.9	0.5	0.3	732	789	844
JZW-02-28	2.09	1	0.9	0.5	0.3	625	670	713
JZW-02-29	2.31	1	0.9	0.5	0.3	632	678	722
JZW-02-30	2.34	1	0.9	0.5	0.3	633	679	723
JZW-03-01	4.36	1	0.9	0.5	0.3	682	733	782
JZW-03-02	6.53	1	0.9	0.5	0.3	716	771	824
JZW-03-03	2.58	1	0.9	0.5	0.3	641	687	732
JZW-03-04	3.09	1	0.9	0.5	0.3	654	702	749
JZW-03-05	4.46	1	0.9	0.5	0.3	684	735	784
JZW-03-06	2.70	1	0.9	0.5	0.3	644	691	736
JZW-03-07	11.75	1	0.9	0.5	0.3	771	833	892
JZW-03-08	14.47	1	0.9	0.5	0.3	792	856	919
JZW-03-09	2.08	1	0.9	0.5	0.3	625	670	712
JZW-03-10	3.19	1	0.9	0.5	0.3	657	705	752
JZW-03-11	8.00	1	0.9	0.5	0.3	735	792	847
JZW-03-12	5.50	1	0.9	0.5	0.3	701	755	806
JZW-03-13	3.19	1	0.9	0.5	0.3	657	705	752
JZW-03-14	4.03	1	0.9	0.5	0.3	675	726	774
JZW-03-15	4.95	1	0.9	0.5	0.3	693	745	795
JZW-03-16	3.40	1	0.9	0.5	0.3	662	711	758
JZW-03-17	3.61	1	0.9	0.5	0.3	667	716	763
JZW-03-18	13.66	1	0.9	0.5	0.3	787	850	911
JZW-03-19	16.06	1	0.9	0.5	0.3	803	869	932
JZW-03-20	9.35	1	0.9	0.5	0.3	749	808	865
JZW-03-21	3.37	1	0.9	0.5	0.3	661	710	757
JZW-03-22	3.11	1	0.9	0.5	0.3	655	703	749
JZW-03-23	4.68	1	0.9	0.5	0.3	688	740	789
JZW-03-24	3.76	1	0.9	0.5	0.3	670	720	767
JZW-03-25	3.31	1	0.9	0.5	0.3	660	708	755
JZW-03-26	2.68	1	0.9	0.5	0.3	643	690	735
JZW-03-27	3.12	1	0.9	0.5	0.3	655	703	749
JZW-03-28	3.82	1	0.9	0.5	0.3	671	721	769
JZW-03-29	4.12	1	0.9	0.5	0.3	677	728	776
JZW-03-30	6.90	1	0.9	0.5	0.3	721	777	830
JZW-04-01	3.90	1	0.9	0.5	0.3	673	723	771
JZW-04-02	4.16	1	0.9	0.5	0.3	678	729	777
JZW-04-03	3.57	1	0.9	0.5	0.3	666	715	762
JZW-04-04	4.56	1	0.9	0.5	0.3	686	737	787
JZW-04-05	3.47	1	0.9	0.5	0.3	663	713	760
JZW-04-06	16.71	1	0.9	0.5	0.3	807	873	937
JZW-04-07	2.74	1	0.9	0.5	0.3	645	692	737
JZW-04-08	6.03	1	0.9	0.5	0.3	709	764	816
JZW-04-09	6.42	1	0.9	0.5	0.3	715	770	823
JZW-04-10	2.27	1	0.9	0.5	0.3	631	677	720
JZW-04-11	2.80	1	0.9	0.5	0.3	647	694	739
JZW-04-12	2.55	1	0.9	0.5	0.3	640	686	731
JZW-04-13	10.30	1	0.9	0.5	0.3	759	818	876
JZW-04-14	6.04	1	0.9	0.5	0.3	710	764	816
JZW-04-15	13.14	1	0.9	0.5	0.3	783	845	906
JZW-04-16	4.02	1	0.9	0.5	0.3	675	726	774
JZW-04-17	4.07	1	0.9	0.5	0.3	676	727	775
JZW-04-18	5.88	1	0.9	0.5	0.3	707	761	813
JZW-04-19	9.08	1	0.9	0.5	0.3	747	805	862
JZW-04-20	4.38	1	0.9	0.5	0.3	682	733	783
JZW-04-21	4.23	1	0.9	0.5	0.3	679	730	779
JZW-04-22	4.98	1	0.9	0.5	0.3	693	745	796
JZW-04-23	8.39	1	0.9	0.5	0.3	739	797	852
JZW-04-24	2808.17	1	0.9	0.5	0.3	1892	2174	2486
JZW-04-25	4.35	1	0.9	0.5	0.3	682	733	782
JZW-04-26	4.89	1	0.9	0.5	0.3	691	744	794
JZW-04-27	13.87	1	0.9	0.5	0.3	788	852	913
JZW-04-28	9.06	1	0.9	0.5	0.3	746	805	861
JZW-04-29	12.07	1	0.9	0.5	0.3	774	836	896
JZW-04-30	3.62	1	0.9	0.5	0.3	667	716	764
JZW-05-01	13.91	1	0.9	0.5	0.3	788	852	914
JZW-05-02	3.61	1	0.9	0.5	0.3	667	716	763
JZW-05-03	4.44	1	0.9	0.5	0.3	683	735	784
JZW-05-04	2.46	1	0.9	0.5	0.3	637	683	727
JZW-05-05	3.73	1	0.9	0.5	0.3	669	719	767
JZW-05-06	2.95	1	0.9	0.5	0.3	651	698	744
JZW-05-07	2.30	1	0.9	0.5	0.3	632	678	721
JZW-05-08	3.71	1	0.9	0.5	0.3	669	718	766
JZW-05-09	7.32	1	0.9	0.5	0.3	727	783	837
JZW-05-10	3.16	1	0.9	0.5	0.3	656	704	751
JZW-05-11	3.25	1	0.9	0.5	0.3	658	707	753
JZW-05-12	8.37	1	0.9	0.5	0.3	739	797	852
JZW-05-13	10.62	1	0.9	0.5	0.3	762	822	880
JZW-05-14	10.91	1	0.9	0.5	0.3	764	825	883
JZW-05-15	96.47	1	0.9	0.5	0.3	1031	1128	1225
JZW-05-16	11.62	1	0.9	0.5	0.3	770	832	891
JZW-05-17	2.92	1	0.9	0.5	0.3	650	698	743
JZW-05-18	3.92	1	0.9	0.5	0.3	673	723	772
JZW-05-19	2.74	1	0.9	0.5	0.3	645	692	737
JZW-05-20	3.59	1	0.9	0.5	0.3	666	716	763
JZW-05-21	2.52	1	0.9	0.5	0.3	639	685	730
JZW-05-22	2.22	1	0.9	0.5	0.3	629	675	718
JZW-05-23	10.20	1	0.9	0.5	0.3	758	817	875
JZW-05-24	3.66	1	0.9	0.5	0.3	668	717	765
JZW-05-25	1.79	1	0.9	0.5	0.3	614	658	699
JZW-05-26	4.73	1	0.9	0.5	0.3	689	741	790
JZW-05-27	3.78	1	0.9	0.5	0.3	670	720	768
JZW-05-28	2.73	1	0.9	0.5	0.3	645	692	737
JZW-05-29	1.93	1	0.9	0.5	0.3	619	664	706
JZW-05-30	9.80	1	0.9	0.5	0.3	754	813	871
锆石Ti饱和温度计计算公式据Ferry and Watson（2007） T(K)= $ \frac{4800（\pm 86）}{5.711（\pm 0.072）-\left[\mathrm{log}\left({ppm}_{Ti-in-zircon}\right)+\mathrm{log}\left({a}_{SiO2}\right)-\mathrm{l}\mathrm{o}\mathrm{g}\left({a}_{TiO2}\right)\right]} $ 1T，2T，3T分别为1a_SiO2，2a_SiO2，3a_SiO2活度对应的锆石晶出温度

下载: 导出CSV

参考文献(52)

[1]	张金川. 南黄海海域构造单元的重新命名及其特征对比[J]. 海洋地质动态, 1995(6):3-5 ZHANG Jinchuan. The renaming of the tectonic units in the south yellow sea and their characteristics comparison[J]. Marine Geology Letters, 1995(6):3-5.]
[2]	栾光忠, 刘红军, 范德江. 青岛胶州湾地质特征及其成因[J]. 海洋湖沼通报, 1998(3):18-23 LUAN Guangzhong, LIU Hongjun, FAN Dejiang. The geological feature and origin of the Jiaozhou Bay in Qingdao[J]. Transactions of Oceanology and Limnology, 1998(3):18-23.]
[3]	栾光忠, 张海平. 青岛沧口-温泉断裂的空间展布及现代活动性研究[J]. 地震地质, 2001, 23(1):63-68 doi: 10.3969/j.issn.0253-4967.2001.01.008 LUAN Guangzhong, ZHANG Haiping. Plane geometry and mordern activity of the Qingdao Cangkou-Wenquan fault[J]. Seismology and Geology, 2001, 23(1):63-68.] doi: 10.3969/j.issn.0253-4967.2001.01.008
[4]	郭玉贵, 邓志辉, 尤惠川, 等. 青岛沧口断裂的地质构造特征与第四纪活动性研究[J]. 震灾防御技术, 2007, 2(2):102-115 doi: 10.11899/zzfy20070202 GUO Yugui, DENG Zhihui, YOU Huichuan, et al. Geological features and Quaternary activities of Cangkou fault in Qingdao, China[J]. Technology for Earthquake Disaster Prevention, 2007, 2(2):102-115.] doi: 10.11899/zzfy20070202
[5]	支鹏遥, 刘保华, 李西双, 等. 胶州湾湾口区的地质特征[J]. 海洋地质动态, 2008, 24(2):11-14,27 doi: 10.3969/j.issn.1009-2722.2008.02.003 ZHI Pengyao, LIU Baohua, LI Xishuang, et al. Geological characteristics of Baymouth area of Jiaozhou bay[J]. Marine Geology Letters, 2008, 24(2):11-14,27.] doi: 10.3969/j.issn.1009-2722.2008.02.003
[6]	李官保, 刘保华, 韩国忠, 等. 胶州湾基岩类型与分布特征研究[J]. 海洋科学进展, 2009, 27(1):34-41 doi: 10.3969/j.issn.1671-6647.2009.01.005 LI Guanbao, LIU Baohua, HAN Guozhong et al. Types and distributions of bed rocks in the Jiaozhou Bay[J]. Advances in Marine Science, 2009, 27(1):34-41.] doi: 10.3969/j.issn.1671-6647.2009.01.005
[7]	栾光忠, 王红霞, 尹明泉, 等. 青岛城市主要断裂构造特征以及对城市地质环境的影响[J]. 地球学报, 2010, 31(1):102-108 LUAN Guangzhong, WANG Hongxia, YIN Mingquan, et al. Characteristics of main faulted structures in Qingdao City and their influence on urban geological environment[J]. Acta Geoscientica Sinica, 2010, 31(1):102-108.]
[8]	韩宗珠, 宋红瑛, 张贺, 等. 青岛胶州湾口海底隧道火成岩岩石地球化学及成因[J]. 海洋湖沼通报, 2012(2):11-21 doi: 10.3969/j.issn.1003-6482.2012.02.002 HAN Zongzhu, SONG Hongying, ZHANG He, et al. Study of Geochemistry and cause of formation of igneous rocks of cross-harbour tunnel in the mouth of Jiaozhou Bay of Qingdao[J]. Transactions of Oceanology and Limnology, 2012(2):11-21.] doi: 10.3969/j.issn.1003-6482.2012.02.002
[9]	窦衍光, 印萍, 陈斌, 等. 滨海基岩城市地质调查成果应用探索与理论技术创新: 以青岛市为例[J]. 海洋地质前沿, 2019, 37(9):1-9 DOU Yanguang, YIN Ping, CHEN Bin, et al. Application exploration, theoretical and technological innovation of geological survey results in coastal bedrock city: Taking Qingdao as an example[J]. Marine Geology Frontiers, 2019, 37(9):1-9.]
[10]	山东省地质调查院. 1: 25万青岛市幅区域地质调查报告与地质图[R]. 2004: 1-420 Shandong Institute of Geological Survey. 1: 250000 Qingdao regional geological survey report and geological map[R]. 2004: 1-420.]
[11]	李桂群. 青岛区域构造特征及其与地震的关系[J]. 海洋湖沼通报, 1994(3):26-32 LI Guiqun. The regional structure characteristics and their relation to earthquakes in Qingdao area[J]. Transactions of Oceanology and Limnology, 1994(3):26-32.]
[12]	侯方辉, 田振兴, 张训华, 等. 南黄海盆地两条地震剖面的重磁数据联合反演效果[J]. 石油地球物理勘探, 2012, 47(5):808-814 HOU Fanghui, TIAN Zhenxing, ZHANG Xunhua, et al. Joint inversion of gravity, magnetic and seismic data of the South Yellow Sea Basin[J]. Oil Geophysical Prospecting, 2012, 47(5):808-814.]
[13]	张玄杰, 张婉, 范子梁, 等. 南黄海北部航空重力场特征及主要地质认识[J]. 中国地质调查, 2017, 4(1):50-56 ZHANG Xuanjie, ZHANG Wan, FAN Ziliang, et al. Characteristics of airborne gravity field and the main geological discovery in the northern South Yellow Sea[J]. Geological Survey of China, 2017, 4(1):50-56.]
[14]	孙中宇, 刘展, 杨博, 等. 海阳凹陷东、西边界以及胶莱盆地东部边界讨论[J]. 地球物理学进展, 2018, 33(5):2166-2171 doi: 10.6038/pg2018BB0372 SUN Zhongyu, LIU Zhan, YANG Bo, et al. Discussion on the eastern and western boundary of Haiyang depression and eastern boundary of Jiaolai Basin[J]. Progress in Geophysics, 2018, 33(5):2166-2171.] doi: 10.6038/pg2018BB0372
[15]	祁江豪, 吴志强, 张训华, 等. 胶莱盆地在南黄海的延伸: 来自OBS深地震探测的新证据[J]. 吉林大学学报(地球科学版), 2019, 49(1):106-114 QI Jianghao, WU Zhiqiang, ZHANG Xunhua, et al. Extension of Jiaolai basin into Qianliyan uplift in south yellow sea: new evidence from OBS deep seismic detection[J]. Journal of Jilin University (Earth Science Edition), 2019, 49(1):106-114.]
[16]	Yuan H L, Gao S, Liu X M, et al. Accurate U-Pb age and trace element determinations of zircon by Laser Ablation-Inductively Coupled Plasma-Mass Spectrometry[J]. Geostandards and Geoanalytical Research, 2004, 28(3):353-370. doi: 10.1111/j.1751-908X.2004.tb00755.x
[17]	Liu Y S, Hu Z C, Zong K Q, et al. Reappraisement and refinement of zircon U-Pb isotope and trace element analyses by LA-ICP-MS[J]. Chinese Science Bulletin, 2010, 55(15):1535-1546. doi: 10.1007/s11434-010-3052-4
[18]	高晓英, 郑永飞. 金红石Zr和锆石Ti含量地质温度计[J]. 岩石学报, 2011, 27(2):417-432 GAO Xiaoying, ZHENG Yongfei. On the Zr-in-rutile and Ti-in-zircon geothermometers[J]. Acta Petrologica Sinica, 2011, 27(2):417-432.]
[19]	雷玮琰, 施光海, 刘迎新. 不同成因锆石的微量元素特征研究进展[J]. 地学前缘, 2013, 20(4):273-284 LEI Weiyan, SHI Guanghai, LIU Yingxin. Research progress on trace element characteristics of zircons of different origins[J]. Earth Science Frontiers, 2013, 20(4):273-284.]
[20]	McDonough W F, Sun S S. The composition of the Earth[J]. Chemical Geology, 1995, 120(3-4):223-253. doi: 10.1016/0009-2541(94)00140-4
[21]	Watson E B, Wark D A, Thomas J B. Crystallization thermometers for zircon and rutile[J]. Contributions to Mineralogy and Petrology, 2006, 151(4):413-433. doi: 10.1007/s00410-006-0068-5
[22]	Fu B, Page F Z, Cavosie A J, et al. Ti-in-zircon thermometry: applications and limitations[J]. Contributions to Mineralogy and Petrology, 2008, 156(2):197-215. doi: 10.1007/s00410-008-0281-5
[23]	Ferry J M, Watson E B. New thermodynamic models and revised calibrations for the Ti-in-zircon and Zr-in-rutile thermometers[J]. Contributions to Mineralogy and Petrology, 2007, 154(4):429-437. doi: 10.1007/s00410-007-0201-0
[24]	Harrison T M, Watson E B, Aikman A B. Temperature spectra of zircon crystallization in plutonic rocks[J]. Geology, 2007, 35(7):635-638. doi: 10.1130/G23505A.1
[25]	Hayden L A, Watson E B. Rutile saturation in hydrous siliceous melts and its bearing on Ti-thermometry of quartz and zircon[J]. Earth and Planetary Science Letters, 2007, 258(3-4):561-568. doi: 10.1016/j.jpgl.2007.04.020
[26]	Schiller D, Finger F. Application of Ti-in-zircon thermometry to granite studies: problems and possible solutions[J]. Contributions to Mineralogy and Petrology, 2019, 174(6):51. doi: 10.1007/s00410-019-1585-3
[27]	Ghent E D, Stout M Z. TiO₂ activity in metamorphosed pelitic and basic rocks: principles and applications to metamorphism in southeastern Canadian Cordillera[J]. Contributions to Mineralogy and Petrology, 1984, 86(3):248-255. doi: 10.1007/BF00373670
[28]	赵广涛, 王德滋, 曹钦臣. 崂山花岗岩岩石地球化学与成因[J]. 高校地质学报, 1997, 3(1):1-15 ZHAO Guangtao, WANG Dezi, CAO Qinchen. The Geochemistry and genesis of the Laoshan granitoids, Shandong Province[J]. Geological Journal of China Universities, 1997, 3(1):1-15.]
[29]	赵广涛, 王德滋, 曹钦臣, 等. I-A型复合花岗岩体的热演化及其意义: 以崂山花岗岩体为例[J]. 中国科学(D辑), 1998, 28(4): 296-302 ZHAO Guangtao, WANG Dezi, CAO Qinchen, et al. Thermal evolution and its significance of I-A type granitoid complex The Laoshan Granitoid as an example[J]. Science in China Series D: Earth Sciences, 1998, 41(5): 529-536.]
[30]	刘利双, 刘福来, 冀磊, 等. 北苏鲁超高压变质带内多成因类型的变花岗质岩石及其地质意义[J]. 岩石学报, 2018, 34(6):1557-1580 LIU Lishuang, LIU Fulai, JI Lei, et al. The polygenetic meta-granitic rocks and their geological significance, within the North Sulu ultrahigh-pressure belt[J]. Acta Petrologica Sinia, 2018, 34(6):1557-1580.]
[31]	王斌, 宋明春, 周建波, 等. 山东省四期A型花岗岩类及其对大地构造演化的启示[J]. 华北地质, 2022, 45(2):1-17 WANG Bin, SONG Mingchun, ZHOU Jianbo, et al. Four stages A-type granitoids in Shandong Province and their implications for tectonic evolution[J]. North China Geology, 2022, 45(2):1-17.]
[32]	Zheng Y F, Wu Y B, Chen F K, et al. Zircon U-Pb and oxygen isotope evidence for a large-scale ¹⁸O depletion event in igneous rocks during the Neoproterozoic[J]. Geochimica et Cosmochimica Acta, 2004, 68(20):4145-4165. doi: 10.1016/j.gca.2004.01.007
[33]	Zhu D C, Lü D W, Shen X L, et al. Discovery and geological significance of neoproterozoic metamorphic granite in Jimo, Shandong province, eastern China[J]. Acta Geologica Sinica, 2016, 90(6):2080-2096. doi: 10.1111/1755-6724.13023
[34]	Gao Y J, Niu Y L, Duan M, et al. The petrogenesis and tectonic significance of the Early Cretaceous intraplate granites in eastern China: The Laoshan granite as an example[J]. Lithos, 2019, 328-329:200-211. doi: 10.1016/j.lithos.2019.01.031
[35]	侯建华, 任天龙, 杨仕鹏, 等. 山东即墨马连山地区新元古代花岗质片麻岩捕掳体的发现及其地质意义[J]. 地质调查与研究, 2016, 39(2):81-88 HOU Jianhua, REN Tianlong, YANG Shipeng, et al. The discovery of Neo proterozoic granitic gneiss xenolith in Malianshan of Jimo, Shandong province, and its geological significance[J]. Geological Survey and Research, 2016, 39(2):81-88.]
[36]	Wei C S, Zhao Z F, Spicuzza M J. Zircon oxygen isotopic constraint on the sources of late Mesozoic A-type granites in eastern China[J]. Chemical Geology, 2008, 250(1-4):1-15. doi: 10.1016/j.chemgeo.2008.01.004
[37]	Goss S C, Wilde S A, Wu F Y, et al. The age, isotopic signature and significance of the youngest Mesozoic granitoids in the Jiaodong Terrane, Shandong Province, North China Craton[J]. Lithos, 2010, 120(3-4):309-326. doi: 10.1016/j.lithos.2010.08.019
[38]	王来明, 任天龙, 刘汉栋, 等. 胶东地区中生代花岗岩划分[J]. 山东国土资源, 2021, 37(8):1-14 doi: 10.12128/j.issn.1672-6979.2021.08.001 WANG Laiming, REN Tianlong, LIU Handong, et al. Division of Mesozoic granites in Jiaodong area[J]. Shandong Land and Resources, 2021, 37(8):1-14.] doi: 10.12128/j.issn.1672-6979.2021.08.001
[39]	刘瑞杨, 周瑶琪, 周腾飞, 等. 青岛大珠山高分异花岗岩地球化学特征与含矿性分析[J]. 地质论评, 2023, 69(1):179-198 LIU Ruiyang, ZHOU Yaoqi, ZHOU Tengfei, et al. Geochemical characteristics and mineralization analysis of Dazhushan highly differentiated granite[J]. Geological Review, 2023, 69(1):179-198.]
[40]	Grimes C B, John B E, Kelemen P B, et al. Trace element chemistry of zircons from oceanic crust: A method for distinguishing detrital zircon provenance[J]. Geology, 2007, 35(7):643-646. doi: 10.1130/G23603A.1
[41]	Hoskin P W O, Schaltegger U. The composition of zircon and igneous and metamorphic petrogenesis[J]. Reviews in Mineralogy and Geochemistry, 2003, 53(1):27-62. doi: 10.2113/0530027
[42]	Belousova E, Griffin W, O'Reilly S Y, et al. Igneous zircon: trace element composition as an indicator of source rock type[J]. Contributions to Mineralogy and Petrology, 2002, 143(5):602-622. doi: 10.1007/s00410-002-0364-7
[43]	郑永飞, 陈福坤, 龚冰, 等. 大别-苏鲁造山带超高压变质岩原岩性质: 锆石氧同位素和U-Pb年龄证据[J]. 科学通报, 2003, 48(2):110-119 doi: 10.3321/j.issn:0023-074X.2003.02.002 ZHENG Yongfei, CHEN Fukun, GONG Bing, et al. Protolith properties of ultrahigh-pressure metamorphic rocks in the Dabie-Sulu orogenic belt: Evidence from zircon oxygen isotope and U-Pb age[J]. Chinese Science Bulletin, 2003, 48(2):110-119.] doi: 10.3321/j.issn:0023-074X.2003.02.002
[44]	Li S, Miller C F, Tao W, et al. Role of sediment in generating contemporaneous, diverse “type” granitoid magmas[J]. Geology, 2021, 50(4):427-431.
[45]	张旗. 中国东部中生代岩浆活动与太平洋板块向西俯冲有关吗?[J]. 岩石矿物学杂志, 2013, 32(1):113-128 doi: 10.3969/j.issn.1000-6524.2013.01.010 ZHANG Qi. Is the Mesozoic magmatism in eastern China related to the westward subduction of the Pacific plate?[J]. Acta Petrologica et Mineralogica, 2013, 32(1):113-128.] doi: 10.3969/j.issn.1000-6524.2013.01.010
[46]	郑永飞, 吴福元. 克拉通岩石圈的生长和再造[J]. 科学通报, 2009, 54(14): 1945-1949 ZHENG Yongfei, WU Fuyuan. Growth and reworking of cratonic lithosphere[J]. Chinese Science Bulletin, 2009, 54(19): 3347-3353.]
[47]	朱晓青, 侯方辉, 刘洪滨, 等. 山东即墨马山粗面英安岩年代学与地球化学特征及其地质意义[J]. 海洋地质与第四纪地质, 2021, 41(6):138-150 ZHU Xiaoqing, HOU Fanghui, LIU Hongbin, et al. Geochronology and geochemistry of Mashan trachydacite, JiMo District, Shandong Province and their geological implications[J]. Marine Geology & Quaternary Geology, 2021, 41(6):138-150.]
[48]	张旗, 王焰, 熊小林, 等. 埃达克岩和花岗岩: 挑战与机遇[M]. 北京: 中国大地出版社, 2008: 1-344 ZHANG Qi, WANG Yan, XIONG Xiaolin, et al. Adakite and Granite: Challenges and Opportunities[M]. Beijing: China Land Press, 2008: 1-344.]
[49]	何登洋, 邱昆峰, 于皓丞, 等. 华北克拉通胶莱盆地马山地区早白垩世粗面英安岩岩石成因[J]. 岩石学报, 2020, 36(12):3705-3720 doi: 10.18654/1000-0569/2020.12.09 HE Dengyang, QIU Kunfeng, YU Haocheng, et al. Petrogenesis of the Early Cretaceous trachy-dacite from Mashan in the Jiaolai Basin, North China Craton[J]. Acta Petrologica Sinica, 2020, 36(12):3705-3720.] doi: 10.18654/1000-0569/2020.12.09
[50]	Cherniak D J, Watson E B. Pb diffusion in zircon[J]. Chemical Geology, 2001, 172(1-2):5-24. doi: 10.1016/S0009-2541(00)00233-3
[51]	Lee J K W, Williams I S, Ellis D J. Pb, U and Th diffusion in natural zircon[J]. Nature, 1997, 390(6656):159-162. doi: 10.1038/36554
[52]	章邦桐, 凌洪飞, 吴俊奇, 等. “花岗岩浆晶出锆石U-Pb体系的封闭温度≥850℃”质疑: 基于元素扩散理论、锆石U-Pb年龄与全岩Rb-Sr年龄对比的证据[J]. 地质论评, 2013, 59(1):63-70 doi: 10.3969/j.issn.0371-5736.2013.01.007 ZHANG Bangtong, LING Hongfei, WU Junqi, et al. Doubts about “the closure temperature of U-Pb isotopic systerm in the zircon crystallized from granitic Magma≥850℃”: evidences of element diffusion theory and comparision between the zircon U-Pb ages and the whole-rock Rb-Sr ages of granite plutons[J]. Geological Review, 2013, 59(1):63-70.] doi: 10.3969/j.issn.0371-5736.2013.01.007