Holocene sediment source-to-sink processes and their controlling factors in the central South Yellow Sea mud area

GU Yu; CHANG Xin; KONG Fanxing; LAN Kai; ZHUANG Guangchao; LIU Xiting

doi:10.16562/j.cnki.0256-1492.2024051401

Marine Geology & Quaternary Geology > 2024 > 44(5): 140-150. > DOI: 10.16562/j.cnki.0256-1492.2024051401

GU Yu，CHANG Xin，KONG Fanxing，et al. Holocene sediment source-to-sink processes and their controlling factors in the central South Yellow Sea mud area[J]. Marine Geology & Quaternary Geology，2024，44(5)：140-150. DOI: 10.16562/j.cnki.0256-1492.2024051401

Citation:

PDF (4065 KB)

Holocene sediment source-to-sink processes and their controlling factors in the central South Yellow Sea mud area

1.
College of Marine Geosciences, Key Laboratory of Submarine Geosciences and Prospecting Technology, Ocean University of China, Qingdao 266100, China
2.
Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, Qingdao 266100, China

More Information

Received Date: May 13, 2024
Revised Date: August 12, 2024
Accepted Date: August 12, 2024

Graphical Abstract

Abstract

Abstract

The central South Yellow Sea mud area is an ideal object for the study of sediment provenance because of the large amount of terrigenous sediments discharged from neighboring rivers. However, the transport processes and controlling factors of these sediments in this area remain unclear. To understand the sediment source-to-sink processes and their controlling factors in the study area since the Holocene, the grain size and element geochemistry of sediments in core YSCW-1 from the mud area were analyzed. The AMS¹⁴C ages of core YSCW-1 indicate that the time of deposition is since 9.3 ka, and the formation of the mud depocenter occurred around 6.5 ka. The sediments are mainly composed of sandy silt, clayey silt, and silt. Relevant geochemical indices reveal that, the sediment sources in the study area are mainly from the Huanghe (Yellow) River and the Changjiang (Yangtze) River. Before 6.7 ka, sediments were mainly derived from the Hanghe River. After 6.7 ka, contribution from the Changjiang River increased, which may be related to the establishment of the modern circulation system in the Yellow Sea. Marine fronts may have limited the transport of sediments from the Huanghe River and Korean rivers to the mud area in the central South Yellow Sea.
- grain size,
- element geochemistry,
- provenance,
- the central South Yellow Sea mud area

FullText(HTML)

References (76)

References

[1]	Liu J P, Li A C, Xu K H, et al. Sedimentary features of the Yangtze River-derived along-shelf clinoform deposit in the East China Sea[J]. Continental Shelf Research, 2006, 26(17):2141-2156.
[2]	Yang S Y, Jung H S, Lim D I, et al. A review on the provenance discrimination of sediments in the Yellow Sea[J]. Earth-Science Reviews, 2003, 63(1):93-120.
[3]	谷玉, 刘喜停, 吴晓, 等. 山东半岛全新世近岸泥质区沉积过程与沉积记录[J]. 古地理学报, 2022, 24(1):164-179 GU Yu, LIU Xiting, WU Xiao, et al. Sedimentary processes and records of the mud area off Shandong Peninsula[J]. Journal of Paleogeography, 2022, 24(1):164-179.]
[4]	刘健, 李绍全, 王圣洁, 等. 末次冰消期以来黄海海平面变化与黄海暖流的形成[J]. 海洋地质与第四纪地质, 1999, 19(1): 13-24 LIU Jian, LI Shaoquan, WANG Shengjie, et al. Sea level changes of the Yellow Sea and formation of the Yellow Sea Warm Current since the last deglaciation [J]. Marine Geology & Quaternary Geology, 1999, 19 (1): 1913-1924.]
[5]	向荣, 杨作升, 郭志刚, 等. 济州岛西南泥质区粒度组分变化的古环境应用[J]. 地球科学, 2005, 30(5):582-588 doi: 10.3321/j.issn:1000-2383.2005.05.010 XIANG Rong, YANG Zuosheng, GUO Zhigang, et al. Paleoenvironmental implications of grain-size component variations in the mud area southwest off Cheju island[J]. Earth Science, 2005, 30(5):582-588.] doi: 10.3321/j.issn:1000-2383.2005.05.010
[6]	Hu B Q, Yang Z S, Zhao M X, et al. Grain size records reveal variability of the East Asian Winter Monsoon since the Middle Holocene in the Central Yellow Sea mud area, China[J]. Science China Earth Sciences, 2012, 55(10):1656-1668. doi: 10.1007/s11430-012-4447-7
[7]	Hu B Q, Li J, Zhao J T, et al. Sr–Nd isotopic geochemistry of Holocene sediments from the South Yellow Sea: Implications for provenance and monsoon variability[J]. Chemical Geology, 2018, 479:102-112. doi: 10.1016/j.chemgeo.2017.12.033
[8]	Koo H, Lee Y, Kim S, et al. Clay mineral distribution and provenance in surface sediments of Central Yellow Sea Mud[J]. Geosciences Journal, 2018, 22(6):989-1000. doi: 10.1007/s12303-018-0019-y
[9]	Mei X, Li R H, Zhang X H, et al. Evolution of the Yellow Sea Warm Current and the Yellow Sea Cold Water Mass since the Middle Pleistocene[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2016, 442:48-60. doi: 10.1016/j.palaeo.2015.11.018
[10]	Xiang R, Yang Z S, Saito Y, et al. Paleoenvironmental changes during the last 8400 years in the southern Yellow Sea: Benthic foraminiferal and stable isotopic evidence[J]. Marine Micropaleontology, 2008, 67(1):104-119.
[11]	Gao F, Qiao L L, Li G X. Modelling the dispersal and depositional processes of the suspended sediment in the central South Yellow Sea during the winter[J]. Geological Journal, 2016, 51(S1):35-48. doi: 10.1002/gj.2827
[12]	Hu D X. Upwelling and sedimentation dynamics[J]. Chinese Journal of Oceanology and Limnology, 1984, 2(1):12-19. doi: 10.1007/BF02888388
[13]	Hu D X. Some Striking Features of Circulation in Huanghai Sea and East China Sea [M]//Oceanology of China Seas. Dordrecht, Springer Netherlands. 1994: 27-38.
[14]	Lie H J, Oh K H, Cho C H, et al. Wintertime Large Temperature inversions in the Yellow Sea Associated with the Cheju and Yellow Sea Warm Currents[J]. Journal of Geophysical Research: Oceans, 2019, 124(7):4856-4874. doi: 10.1029/2019JC015180
[15]	Lin X P, Yang J Y, Guo J S, et al. An asymmetric upwind flow, Yellow Sea Warm Current: 1. New observations in the western Yellow Sea[J]. Journal of Geophysical Research: Oceans, 2011, 116(C04026):1-13.
[16]	Dong L X, Guan W B, Chen Q, et al. Sediment transport in the Yellow Sea and East China Sea[J]. Estuarine, Coastal and Shelf Science, 2011, 93(3):248-258. doi: 10.1016/j.ecss.2011.04.003
[17]	Zhu Y, Chang R. Preliminary Study of the dynamic origin of the distribution pattern of bottom sediments on the continental shelves of the Bohai Sea, Yellow Sea and East China Sea[J]. Estuarine, Coastal and Shelf Science, 2000, 51(5):663-680. doi: 10.1006/ecss.2000.0696
[18]	Gao F, Qiao L L, Li G X. Winter meso-scale shear front in the Yellow Sea and its sedimentary effects[J]. Journal of Ocean University of China, 2016, 15(1):50-56. doi: 10.1007/s11802-016-2668-7
[19]	Shi Y, Gao J H, Sheng H, et al. Cross-Front sediment transport induced by quick oscillation of the Yellow Sea Warm Current: Evidence from the sedimentary record[J]. Geophysical Research Letters, 2019, 46(1):226-234. doi: 10.1029/2018GL080751
[20]	Zhang X D, Ji Y, Yang Z S, et al. End member inversion of surface sediment grain size in the South Yellow Sea and its implications for dynamic sedimentary environments[J]. Science China Earth Sciences, 2016, 59(2):258-267. doi: 10.1007/s11430-015-5165-8
[21]	Alexander C R, DeMaster D J, Nittrouer C A. Sediment accumulation in a modern epicontinental-shelf setting: The Yellow Sea[J]. Marine Geology, 1991, 98(1):51-72. doi: 10.1016/0025-3227(91)90035-3
[22]	Milliman J D, Shen H T, Yang Z S, et al. Transport and deposition of river sediment in the Changjiang estuary and adjacent continental shelf[J]. Continental Shelf Research, 1985, 4(1):37-45.
[23]	Milliman J D, Meade R H. World-wide delivery of river sediment to the oceans[J]. The Journal of Geology, 1983, 91:1-21. doi: 10.1086/628741
[24]	Wang H J, Yang Z S, Saito Y, et al. Stepwise decreases of the Huanghe (Yellow River) sediment load (1950–2005): Impacts of climate change and human activities[J]. Global and Planetary Change, 2007, 57(3):331-354.
[25]	Yang S L, Milliman J D, Xu K H, et al. Downstream sedimentary and geomorphic impacts of the Three Gorges Dam on the Yangtze River[J]. Earth-Science Reviews, 2014, 138:469-486. doi: 10.1016/j.earscirev.2014.07.006
[26]	Yang S L, Xu K H, Milliman J D, et al. Decline of Yangtze River water and sediment discharge: Impact from natural and anthropogenic changes[J]. Scientific Reports, 2015, 5(1):1-14.
[27]	Kim D, Park B K, Shin I C. Paleoenvironmental changes of the Yellow Sea during the Late Quaternary[J]. Geo-Marine Letters, 1998, 18(3):189-194. doi: 10.1007/s003670050067
[28]	Lee H J, Chough S K. Sediment distribution, dispersal and budget in the Yellow Sea[J]. Marine Geology, 1989, 87(2):195-205.
[29]	Milliman J D, Li F, Zhao Y Y, et al. Suspended matter regime in the Yellow Sea[J]. Progress in Oceanography, 1986, 17(3):215-227.
[30]	Yang Z S, Liu J P. A unique Yellow River-derived distal subaqueous delta in the Yellow Sea[J]. Marine Geology, 2007, 240(1):169-176.
[31]	Li J, Hu B Q, Wei H L, et al. Provenance variations in the Holocene deposits from the southern Yellow Sea: Clay mineralogy evidence[J]. Continental Shelf Research, 2014, 90:41-51. doi: 10.1016/j.csr.2014.05.001
[32]	杨守业, 李从先, Lee C B, 等. 黄海周边河流的稀土元素地球化学及沉积物物源示踪[J]. 科学通报, 1233, 48(11):1233-1236 YANG Shouye, LI Congxian, Lee C B, et al. REE geochemistry of suspended sediments from the rivers around the Yellow Sea and provenance indicators[J]. Science Bulletin, 48(11): 1233, 48(11):1233-1236.]
[33]	刘庚, 韩喜彬, 陈燕萍, 等. 南黄海沉积物磁性特征及其对物源变化的指示——以南黄海中部泥质区YSC-10孔为例[J]. 沉积学报, 2021, 39(2):383-394 LIU Geng, HAN Xibin, CHEN Yanping, et al. Magnetic characteristics of core YSC-310 sediments in the Central Yellow Sea mud area and implications for provenance changes[J]. Acta Sedimentologica Sinica, 2021, 39(2):383-394.]
[34]	Wang Y H, Li G X, Zhang W G, et al. Sedimentary environment and formation mechanism of the mud deposit in the central South Yellow Sea during the past 40kyr[J]. Marine Geology, 2014, 347:123-135. doi: 10.1016/j.margeo.2013.11.008
[35]	Bian C W, Jiang W S, Greatbatch R J. An exploratory model study of sediment transport sources and deposits in the Bohai Sea, Yellow Sea, and East China Sea[J]. Journal of Geophysical Research: Oceans, 2013, 118(11):5908-5923. doi: 10.1002/2013JC009116
[36]	Li G X, Qiao L L, Dong P, et al. Hydrodynamic condition and suspended sediment diffusion in the Yellow Sea and East China Sea[J]. Journal of Geophysical Research: Oceans, 2016, 121(8):6204-6222. doi: 10.1002/2015JC011442
[37]	Naimie C E, Blain C A, Lynch D R. Seasonal mean circulation in the Yellow Sea — a model-generated climatology[J]. Continental Shelf Research, 2001, 21(6):667-695.
[38]	Park S, Chu P C, Lee J H. Interannual-to-interdecadal variability of the Yellow Sea Cold Water Mass in 1967–2008: Characteristics and seasonal forcings[J]. Journal of Marine Systems, 2011, 87(3):177-193.
[39]	李广雪, 杨子赓, 刘勇. 中国东部海域海底沉积环境成因研究[M]. 北京: 科学出版社, 2005: 1-44 LI Guangxue, YANG Zigeng, LIU Yong. Formation environment of the seafloor sediment in the Eastern China Seas [M]. Beijing: Science Press, 2005: 1-44.]
[40]	Zhong F C, Xiang R, Zhang L L, et al. A synthesized study of the spatiotemporal evolution of Central Yellow Sea Mud depositional processes during the Holocene[J]. Frontiers in Earth Science, 2021, 9:1-16.
[41]	Kim J M, Kucera M. Benthic foraminifer record of environmental changes in the Yellow Sea (Hwanghae) during the last 15000 years[J]. Quaternary Science Reviews, 2000, 19(11):1067-1085. doi: 10.1016/S0277-3791(99)00086-4
[42]	Kim H, Lee H, Lee G A. New marine reservoir correction values (ΔR) applicable to dates on Neolithic Shells from the south coast of Korea[J]. Radiocarbon, 2021, 63(4):1287-1302. doi: 10.1017/RDC.2021.45
[43]	Kong G S, Lee C W. Marine reservoir corrections (ΔR) for southern coastal waters of Korea [J]. 2005, 10(2): 124-128.
[44]	Southon J, Kashgarian M, Fontugne M, et al. Marine reservoir corrections for the Indian Ocean and Southeast Asia[J]. Radiocarbon, 2002, 44(1):167-180. doi: 10.1017/S0033822200064778
[45]	Yoneda M, Uno H, Shibata Y, et al. Radiocarbon marine reservoir ages in the western Pacific estimated by pre-bomb molluscan shells[J]. Nuclear Instruments and Methods in Physics Research Section B: Beam Interactions with Materials and Atoms, 2007, 259(1):432-437. doi: 10.1016/j.nimb.2007.01.184
[46]	Taylor S R, McLennan S M. The continental crust: Its composition and evolution [M]. United States: Blackwell Scientific Publication, 1985.
[47]	杨守业, 李从先. 长江与黄河沉积物REE地球化学及示踪作用[J]. 地球化学, 1999, 28(4):374-380 YANG Shouye, LI Congxian. REE geochemistry and tracing application in the Yangtze River and theYellow River sediments[J]. Geochimica, 1999, 28(4):374-380.]
[48]	杨守业, 李从先, Jung H S, 等. 中韩河流沉积物微量元素地球化学研究[J]. 海洋地质与第四纪地质, 2003, 23(2):19-24 YANG Shouye, LI Congxian, JUNG Hoisoo, et al. Geochemistry of trace elements in Chinese and Korean river sediments[J]. Marine Geology & Quaternary Geology, 2003, 23(2):19-24.]
[49]	杨守业, Jung H S, 李从先, 等. 黄河、长江与韩国Keum、Yeongsan江沉积物常量元素地球化学特征[J]. 地球化学, 2004, 33(1):99-105 doi: 10.3321/j.issn:0379-1726.2004.01.013 YANG Shouye, JUNG Hoisoo, LI Congxian, et al. Major element geochemistry of sediments from Chinese and Korean rivers[J]. Geochimica, 2004, 33(1):99-105.] doi: 10.3321/j.issn:0379-1726.2004.01.013
[50]	Yang S Y, Li C X, Jung H S, et al. Discrimination of geochemical compositions between the Changjiang and the Huanghe sediments and its application for the identification of sediment source in the Jiangsu coastal plain, China[J]. Marine Geology, 2002, 186(3):229-241.
[51]	Cho Y G, Lee C B, Choi M S. Geochemistry of surface sediments off the southern and western coasts of Korea[J]. Marine Geology, 1999, 159(1):111-129.
[52]	Yang S Y, Youn J S. Geochemical compositions and provenance discrimination of the central south Yellow Sea sediments[J]. Marine Geology, 2007, 243(1):229-241.
[53]	Lu J, Li A C, Zhang J, et al. Yangtze River-derived sediments in the southwestern South Yellow Sea: Provenance discrimination and seasonal transport mechanisms[J]. Journal of Asian Earth Sciences, 2019, 176:353-367. doi: 10.1016/j.jseaes.2019.03.007
[54]	蓝先洪, 张志珣, 李日辉, 等. 南黄海NT2孔沉积物物源研究[J]. 沉积学报, 2010, 28(6): 1182-1189 LAN Xianhong, ZHANG Zhixun, LI Rihui, et al. Provenance study of sediments in core NT2 of the South Yellow Sea [J]. Acta Sedimentologica Sinica, 2020, 28(6): 1182-1189.]
[55]	密蓓蓓, 张勇, 梅西, 等. 中国东部海域表层沉积物稀土元素赋存特征及物源探讨[J]. 中国地质, 2020, 47(5):1530-1541 MI Beibei, ZHANG Yong, MEI Xi, et al. The rare earth element content in surface sediments of coastal areas in eastern China's sea areas and an analysis of material sources[J]. Geology in China, 2020, 47(5):1530-1541.]
[56]	Zhu Y T, Bao R, Zhu L H, et al. Investigating the provenances and transport mechanisms of surface sediments in the offshore muddy area of Shandong Peninsula: Insights from REE analyses[J]. Journal of Marine Systems, 2022, 226:1-12.
[57]	Rao W B, Mao C P, Wang Y G, et al. Geochemical constraints on the provenance of surface sediments of radial sand ridges off the Jiangsu coastal zone, East China[J]. Marine Geology, 2015, 359:35-49. doi: 10.1016/j.margeo.2014.11.007
[58]	Rao W B, Mao C P, Wang Y G, et al. Using Nd-Sr isotopes and rare earth elements to study sediment provenance of the modern radial sand ridges in the southwestern Yellow Sea[J]. Applied Geochemistry, 2017, 81:23-35. doi: 10.1016/j.apgeochem.2017.03.011
[59]	孙效功, 方明, 黄伟. 黄、东海陆架区悬浮体输运的时空变化规律[J]. 海洋与湖沼, 2000, 31(6):581-587 doi: 10.3321/j.issn:0029-814X.2000.06.001 SUN Xiaogong, FANG Ming, HUANG Wei. 2000. Spatial and temporal variations in suspended particulate matter transport on the Yellow and East China Sea shelf[J]. Oceanologia et Limnologia Sinica, 2000, 31(6):581-587.] doi: 10.3321/j.issn:0029-814X.2000.06.001
[60]	王勇智, 乔璐璐, 杨作升, 等. 近岸强海流切变锋作用下悬浮沉积物的输送和沉积——以山东半岛东端外海为例[J]. 沉积学报, 2013, 31(3):486-496 WANG Yongzhi, QIAO Lulu, YANG Zuosheng, et al. Suspend sediment transport and deposition due to strong regional shear current front: an example from the shelf waters off eastern Shandong Peninsula[J]. Acta Sedimentologica Sinica, 2013, 31(3):486-496.]
[61]	杨作升, 郭志刚, 王兆祥, 等. 黄东海陆架悬浮体向其东部深海区输送的宏观格局[J]. 海洋学报, 1992, 14(1992):81-90 YANG Zuosheng, GUO Zhigang, WANG Zhaoxiang, et al. The macro pattern of the suspended body of the Yellow Sea and the East China Sea to the eastern deep sea area[J]. Acta Oceanologica Sinica, 1992, 14(1992):81-90.]
[62]	Lambeck K, Rouby H, Purcell A, et al. Sea level and global ice volumes from the Last Glacial Maximum to the Holocene[J]. Proceedings of the National Academy of Sciences, 2014, 111(43):15296-15303. doi: 10.1073/pnas.1411762111
[63]	Liu J, Saito Y, Kong X H, et al. Delta development and channel incision during marine isotope stages 3 and 2 in the western South Yellow Sea[J]. Marine Geology, 2010, 278(1):54-76.
[64]	薛春汀, 周永青, 朱雄华. 晚更新世末至公元前7世纪的黄河流向和黄河三角洲[J]. 海洋学报, 2004, 26(1):48-61 doi: 10.3321/j.issn:0253-4193.2004.01.006 XUE Chunting, ZHOU Yongqing, ZHU Xionghua. The Huanghe River course and delta from end of Late Pleistocene to the 47th century BC[J]. Acta Oceanologica Sinica, 2004, 26(1):48-61.] doi: 10.3321/j.issn:0253-4193.2004.01.006
[65]	Liu J P, Xu K H, Li A C, et al. Flux and fate of Yangtze River sediment delivered to the East China Sea[J]. Geomorphology, 2007, 85(3):208-224.
[66]	夏东兴, 刘振夏. 末次冰期盛期长江入海流路探讨[J]. 海洋学报, 2001, 23(5):87-94 XIA Dongxing, LIU Zhenxia. Tracing the Changjiang River’s flowing route entering the sea during the last ice age maximum[J]. Acta Oceanologica Sinica, 2001, 23(5):87-94.]
[67]	Hori K, Saito Y, Zhao Q H, et al. Evolution of the coastal depositional systems of the Changjiang (Yangtze) River in response to Late Pleistocene-Holocene sea-level changes[J]. Journal of Sedimentary Research, 2002, 72(6):884-897. doi: 10.1306/052002720884
[68]	Saito Y, Wei H, Zhou Y, et al. Delta progradation and chenier formation in the Huanghe (Yellow River) delta, China[J]. Journal of Asian Earth Sciences, 2000, 18(4):489-497. doi: 10.1016/S1367-9120(99)00080-2
[69]	Liu J P, Milliman J D, Gao S, et al. Holocene development of the Yellow River's subaqueous delta, North Yellow Sea[J]. Marine Geology, 2004, 209(1):45-67.
[70]	Yang D Y, Yu G, Xie Y B, et al. Sedimentary records of large Holocene floods from the middle reaches of the Yellow River, China[J]. Geomorphology, 2000, 33(1):73-88.
[71]	Li T G, Nan Q Y, Jiang B, et al. Formation and evolution of the modern warm current system in the East China Sea and the Yellow Sea since the last deglaciation[J]. Chinese Journal of Oceanology and Limnology, 2009, 27(2):237-249. doi: 10.1007/s00343-009-9149-4
[72]	Zhao S Q, Zhao J T, Jia C, et al. The impact of Holocene interactions among climate, ocean current, and shear front factors on fine sediment dispersal in the central South Yellow Sea[J]. Continental Shelf Research, 2022, 246:1-9.
[73]	Xu K H, Li A C, Liu J P, et al. Provenance, structure, and formation of the mud wedge along inner continental shelf of the East China Sea: A synthesis of the Yangtze dispersal system[J]. Marine Geology, 2012, 291-294:176-191. doi: 10.1016/j.margeo.2011.06.003
[74]	Zhong Y, Qiao L L, Song D H, et al. Impact of cold water mass on suspended sediment transport in the South Yellow Sea[J]. Marine Geology, 2020, 428:1-20.
[75]	Hu B Q, Yang Z S, Qiao S Q, et al. Holocene shifts in riverine fine-grained sediment supply to the East China Sea Distal Mud in response to climate change[J]. The Holocene, 2014, 24(10):1253-1268. doi: 10.1177/0959683614540963
[76]	Lim D, Xu Z K, Choi J Y, et al. Holocene changes in detrital sediment supply to the eastern part of the central Yellow Sea and their forcing mechanisms[J]. Journal of Asian Earth Sciences, 2015, 105:18-31. doi: 10.1016/j.jseaes.2015.03.032

[1]	LU Kai, SUN Jun, LI Guangxue, YANG Huiliang, WANG Zhonglei, MEI Xi, CHEN Xiaohui, QI Jianghao, ZHU Xiaoqing, QIANG Xiaoke. Magnetostratigraphy of Quaternary sediments from borehole SYS90-1A in the South Yellow Sea[J]. Marine Geology & Quaternary Geology, 2024, 44(2): 97-109. DOI: 10.16562/j.cnki.0256-1492.2023052203
[2]	CHEN Xiaohui, LU Kai, TIAN Zhenxing, WEN Zhenhe, XU Xiaoda, ZHANG Yong, KONG Xianghuai. Progradational sediment: succession and paleo-channel system in the central South Yellow Sea since the Late Pleistocene[J]. Marine Geology & Quaternary Geology, 2023, 43(4): 85-96. DOI: 10.16562/j.cnki.0256-1492.2022072701
[3]	HUANG Long, GENG Wei, LU Kai, TIAN Zhenxing, ZHANG Yong, WEN Zhenhe. Rare earth element composition and provenance implication of sediments in the Central South Yellow Sea since MIS6[J]. Marine Geology & Quaternary Geology, 2023, 43(2): 92-105. DOI: 10.16562/j.cnki.0256-1492.2022072501
[4]	WANG Zhonglei, LU Kai, SUN Jun, ZHANG Yong, ZHU Xiaoqing, HU Gang, HE Mengying, HUANG Xiangtong, MI Beibei. Detrital zircon U-Pb age and provenance discrimination in sediments of the central mud area in the South Yellow Sea[J]. Marine Geology & Quaternary Geology, 2022, 42(5): 70-82. DOI: 10.16562/j.cnki.0256-1492.2022062402
[5]	LENG Chuanxu, YUAN Hongjie, XU Cuiling, HAO Yanan, ZHAO Guangtao. APPLICATIONS OF LOGARITHM RATIO TRANSFORMATION TO EXTRACTION OF THE SENSITIVE GRAIN SIZE OF EAST ASIAN WINTER MONSOON BY THE METHOD OF FACTOR ANALYSIS: A CASE STUDY OF CORE H07 FROM THE CENTRAL MUD AREA OF THE SOUTH YELLOW SEA[J]. Marine Geology & Quaternary Geology, 2017, 37(1): 151-161. DOI: 10.16562/j.cnki.0256-1492.2017.01.018
[6]	WANG Feifei, LIU Jian, QIU Jiandong, LIU Xianguang, MEI Xi. THICKNESS VARIATION AND PROVENANCE OF MID-HOLOCENE MUD SEDIMENTS IN THE CENTRAL AND WESTERN SOUTH YELLOW SEA[J]. Marine Geology & Quaternary Geology, 2014, 34(5): 1-11. DOI: 10.3724/SP.J.1140.2014.05001
[7]	XU Gang, LIU Jian, KONG Xianghuai, ZHANG Junqiang, QIU Jiandong. RARE EARTH ELEMENTS IN SURFACE SEDIMENTS OF WESTERN SOUTH YELLOW SEA AND THEIR PROVENANCE IMPLICATIONS[J]. Marine Geology & Quaternary Geology, 2012, 32(1): 11-17. DOI: 10.3724/SP.J.1140.2012.01011
[8]	WANG Libo, YANG Zuosheng, ZHAO Xiaohui, XING Lei, ZHAO Meixun, Yoshiki Saito, FAN Dejiang. SEDIMENTARY CHARACTERISTICS OF CORE YE-2 FROM THE CENTRAL MUD AREA IN THE SOUTH YELLOW SEA DURING LAST 8 400 YEARS AND ITS INTERSPACE COARSE LAYERS[J]. Marine Geology & Quaternary Geology, 2009, 29(5): 1-11. DOI: 10.3724/SP.J.1140.2009.05001
[9]	LAN Xian-hong, ZHANG Xian-jun, WANG Hong-xia, ZHAO Guang-tao, ZHANG Zhi-xun, LIN Zhen-hong. SEDIMENTARY GEOCHEMISTRY IN CORE NT2 OF THE SOUTH YELLOW SEA AND ITS PROVENANCE[J]. Marine Geology & Quaternary Geology, 2008, 28(1): 51-60.
[10]	KONG Xiang-huai, LIU Jian, LI Wei-ran, ZHANG Xian-jun, LIANG Yuan. GEOCHEMISTRY OF REE AND PROVENANCE OF SURFACE SEDIMENTS IN THE LITTORAL AREA OF THE NORTHEASTERN SHANDONG PENINSULA[J]. Marine Geology & Quaternary Geology, 2007, 27(3): 51-59.

Cited By

Cited by

Periodical cited type(4)

1.	李磊，李宁，尹文笋，张武，何新建. 西湖凹陷平湖斜坡A潜山储层特征与裂缝预测. 海洋石油. 2024(02): 22-28 .
2.	苗清. 西湖凹陷中央反转构造带中南部花港组母质条件分析. 中国石油和化工标准与质量. 2023(11): 91-93+96 .
3.	苗清，苗苗. 西湖凹陷平北区平湖组岩浆岩物源条件分析. 中国石油和化工标准与质量. 2023(11): 148-151 .
4.	李磊，张武，何新建，孙永壮，赵天亮. 东海西湖凹陷平湖斜坡带基底潜山储层发育模式. 上海国土资源. 2023(02): 134-139 .

Other cited types(1)

Get Citation

PDF

XML

Article views (56) PDF downloads (41) Cited by(5)

Turn off MathJax

Article Contents

Abstract

References

Holocene sediment source-to-sink processes and their controlling factors in the central South Yellow Sea mud area