鲁西地区中生代穹盆构造与东亚构造体制转换

孙文军; 李三忠; 王鹏程; 李玺瑶; 刘晓光; 张剑; 兰浩圆; 李少俊

doi:10.16562/j.cnki.0256-1492.2017.04.007

鲁西地区中生代穹盆构造与东亚构造体制转换

孙文军^1,2,,
李三忠^1,2, ,,
王鹏程^1,2,
李玺瑶^1,2,
刘晓光^1,2,
张剑^1,2,
兰浩圆^1,2,
李少俊^1,2

1.
海底科学与探测技术教育部重点实验室，中国海洋大学海洋地球科学学院，青岛 266100
2.
青岛海洋科学与技术国家实验室海洋地质功能实验室，青岛 266237

基金项目:

山东省泰山学者特聘教授项目

鳌山卓越科学家计划 2015ASTP-0S10

国家自然科学基金杰出青年基金 41325009

国家重点研发计划 2016YFC060102

国家海洋局重大专项 GASI-GEOGE-01

国家重点研发计划 2017YFC0601401

详细信息

作者简介:
孙文军(1987—)，男，博士生，海洋地质专业，E-mail: sunwenjuna@163.com

通讯作者:
李三忠(1968—)，男，教授，博士生导师，构造地质与海洋地质专业，E-mail:sanzhong@ouc.edu.cn

中图分类号: P542
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出版历程
- 收稿日期: 2017-05-30
- 修回日期: 2017-07-25
- 刊出日期: 2017-08-27

MESOZOIC DOME-BASIN STRUCTURES IN WESTERN SHANDONG PROVINCE AND ITS BEARING ON TRANSITION OF TECTONIC REGIMES IN EAST ASIA

1.
Key Lab of Submarine Geosciences and Prospecting Techniques, MOE, College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
2.
Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China

摘要

摘要: 根据野外观察分析，综合前人研究成果，对鲁西地区中生代褶皱叠加期次、构造特征以及动力学机制进行了分析。结果表明，鲁西中生代构造期次主要分为印支期和燕山期两幕褶皱-逆冲推覆作用，印支期主要为近东西向的宽缓褶皱，燕山期则以北东—北北东向的逆冲推覆和相关褶皱为主，两期褶皱叠加，形成穹盆构造。鲁西地区这种穹盆构造是东亚构造体制转变的地壳变形构造特征的产物。中生代以来，华北和华南地块之间的拼合构成了最初的东亚大陆，主要以近东西向构造为主。中生代中晚期逐渐发育起来的北北东向的环太平洋构造带叠加在东亚大陆的东缘，意味着在这期间古特提斯构造域为主导的汇聚体制转变为古太平洋构造域的俯冲消减体制。
- 穹盆构造 /
- 印支运动 /
- 燕山运动 /
- 构造转换 /
- 鲁西
Abstract: According to field observation and previous research results, this paper makes a detailed study on fold superposition as well as structural styles and geodynamics in Western Shandong Province. The Mesozoic tectonic deformation in the region can be obviously divided into two groups, i.e. the Indosinian EW-striking open to tight folds and related reverse faults and the Yanshanian NNE- or NS-striking box fold and related propagating thrust fault system. The dome-basin structures in this region are the results of the superposition of the Indosinian and Yanshanian folds and represent the crustal deformation related to a transition of the geodynamic systems. The tectonic blocks of Yangtze, North China and Siberian assembled in Mesozoic, and then the East Asia formed, that resulted in the formation of EW-striking structures. Until the middle and late Mesozoic, the NNE-striking circum-Pacific tectonic belt gradually developed and began to affect the eastern margin of the East Asia Continent, Then happened the transition from the collisional systems of the Paleo-Asian Ocean and Paleo-Tethys tectonic domains to the the subduction system of the Paleo-Pacific Tectonic Domain.
- dome-basin structure /
- Indosinian /
- Yanshanian /
- tectonic conversion /
- western Shandong Province

HTML全文

图 1 中国东部及邻区构造格架图

(根据文献[30-36]编制)

Figure 1. Tectonic map of East China and adjacent areas

(modified after references [30-36])

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图 2 鲁西地块及邻区构造格架

(根据文献[14-20, 30-36]编制)

Figure 2. Tectonic map of the Luxi Block and adjacent areas

(modified after references[14-20, 30-36])

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图 3 鲁西地区穹盆构造

F1-F4:郯庐断裂带; F5:上五井断裂; F6:益都断裂; F7:博山断裂; F8:铜冶店-孙祖断裂; F9:文祖断裂; F10:泰山山前断裂; F11:新泰-蒙阴断裂; F12:蒙山山前断裂; F13:汶口断裂; F14:肥城断裂; F15:汶泗断裂; F16:苍山-尼山断裂; F17:枣庄断裂; F18:济南断裂; A、B、C、D、E、F为野外观察点位置

Figure 3. Dome-basin structure in Western Shandong Province

F1-F4: Tanlu Fault Zone; F5: Shangwujing Fault; F6: Yidu Fault; F7: Boshan Fault; F8 Tongyedian-Sunzu Fault; F9: Wenzu Fault; F10: Taishan Piedmont Fault; F11: Xintai-Mengyin Fault; F12: Mengshan Piedmont Fault; F13: Wenkou Fault; F14: Feicheng Fault; F15 Wensi Fault; F16: Cangshan-Nishan Fault; F17: Zaozhuang Fault; F18: Jinan Fault; A, B, C, D, E and F show the positions of field observation stations

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图 4 潍坊市临朐县西峪村构造剖面

(位置如图 3中A，GPS: 36.39089°N、118.31236°E, H292.7 m)

Figure 4. Structural profile at the Xiyu Village, Linqu County, Weifang City

(See A in Fig. 3 for location, GPS:36.39089°N、118.31236°E, H292.7 m)

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图 5 济南市章丘区文祖镇文盛路构造剖面

(位置如图 3中B，GPS: 36.62046°N、117.52599°E, H238.2 m)

Figure 5. Structural profile through the Wenzun Town, Zhangqiu County, Jinan City

(See B in Fig. 3 for location, GPS:36.62046°N、117.52599°E, H238.2 m)

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图 6 沂源县三岔乡璞邱一村构造剖面

(位置如图 3中C，GPS: 36.31564°N、118.23188°E, H343.9 m)

Figure 6. Structural profile at the Puqiouyi Village, Sancha Town, Yiyuan County

(See C in Fig. 3 for location, GPS: 36.31564°N、118.23188°E, H343.9 m)

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图 7 淄博市淄川区昆仑镇构造剖面

(位置如图 3中D，GPS: 36.55896°N、117.94433°E, H244.5 m)

Figure 7. Structural profile at the Kunlun Town, Zichuan county, Zibo City

(See D in Fig. 3 for location, GPS: 36.55896°N、117.94433°E, H244.5 m)

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图 8 章丘市文祖镇南青野村构造剖面

(位置如图 3中E，GPS: 36.55105°N、117.52975°E, H278.2 m)

Figure 8. Structural profile at the Qingye Village, Wenzu Town, Zhangqiu County

(See E in Fig. 3 for location, GPS: 36.55105°N、117.52975°E, H278.2 m)

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图 9 平邑县大泉村构造剖面

(位置如图 3中F，GPS: 35.36486°N、17.83423°E, H125.0 m)

Figure 9. Structural profile at the Daquan Village, Pingyi County

(See F in Fig. 3 for location, GPS: 35.36486°N、117.83423°E, H125.0 m)

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图 10 鲁西中生代盆地与断裂构造图

(根据文献[37]编制)
F1-F4:郯庐断裂带; F5:上五井断裂; F6:益都断裂; F7:博山断裂; F8:铜冶店-孙祖断裂; F9:文祖断裂; F10:泰山山前断裂; F11:新泰-蒙阴断裂; F12:蒙山山前断裂; F13:汶口断裂; F14:肥城断裂; F15:汶泗断裂; F16:苍山-尼山断裂; F17:枣庄断裂; F18:济南断裂; F19:兰聊断裂

Figure 10. Structural framework of the Luxi Block

(modified after reference[37])
F1-F4: Tanlu Fault Zone; F5: Shangwujing Fault; F6: Yidu Fault; F7: Boshan Fault; F8:Tongyedian-Sunzu Fault; F9: Wenzu Fault; F10: Taishan Piedmont Fault; F11: Xintai-Mengyin Fault; F12: Mengshan Piedmont Fault; F13: Wenkou Fault; F14: Feicheng Fault; F15:Wensi Fault; F16: Cangshan-Nishan Fault; F17: Zaozhuang Fault; F18: Jinan Fault; F19: Lanliao Fault

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图 11 鲁西地块褶皱构造与成因模式^{[32, 47, 54]}

Figure 11. Tectonic model of fold structure of the Luxi Block^{[32, 47, 54]}

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