DOU Yanguang, CHEN Xiaohui, LI Jun, CAI Feng, WEN Zhenhe, XU Gang, ZOU Liang. Origin and provenance of the surficial sediments in the subenvironments of the East China Sea[J]. Marine Geology & Quaternary Geology, 2018, 38(4): 21-31. DOI: 10.16562/j.cnki.0256-1492.2018.04.002
Citation: DOU Yanguang, CHEN Xiaohui, LI Jun, CAI Feng, WEN Zhenhe, XU Gang, ZOU Liang. Origin and provenance of the surficial sediments in the subenvironments of the East China Sea[J]. Marine Geology & Quaternary Geology, 2018, 38(4): 21-31. DOI: 10.16562/j.cnki.0256-1492.2018.04.002
shu

Origin and provenance of the surficial sediments in the subenvironments of the East China Sea

  • 1.

    Key Laboratory of Marine Hydrocarbon Resource of Environmental Geology, Ministry of Land and Resources, China Geology Survey, Qingdao Institute of Marine Geology, Qingdao 266071, China

  • 2.

    Laboratory for Marine Geology and Environment, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266061, China

  • 3.

    Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China

More Information
  • Received Date: January 29, 2018
  • Revised Date: May 03, 2018
    Graphical Abstract
    • Abstract
  • Grain size and clay mineral composition are analyzed for the surface sediments in various depositional units of the East China Sea including its outer shelf and slope, and the Okinawa Trough.Upon the basis, the origin and provenance of the sediments are discussed.Results show that the grain size of the sediments becomes finer gradually from the outer continental shelf, slope, to the Okinawa Trough.The sediments in the outer continental shelf are dominated by beach sands or breaker zone deposits formed during the deglacial transgression of late Pleistocene, and belong to the so-called "relict sediment", while the sediment on the western slope of the Okinawa Trough is characterized by gravity flow deposits, indicating a transportation pattern from the outer continental shelf to the Trough.Suspended deposits predominate the bottom fine sediment of the Okinawa Trough, having the characteristics of bathyal deposits.They are mainly from the rivers of Taiwan and Mainland China, such as the Changjiang and Minjiang Rivers.Provenance study reveals that the fine materials from Taiwan is mainly transported by Kuroshio Current, and the fine sediments from Mainland China are mainly transported by various transportation mechanisms, such as the"near-bottom lateral transportation"and"storage in winter and transporting in summer."
    • FullText(HTML)
    • References (52)
  • [1]
    郭志刚, 杨作升, 曲艳慧, 等.东海陆架泥质区沉积地球化学比较研究[J].沉积学报, 2000, 18 (22) :284-289. http://d.old.wanfangdata.com.cn/Periodical/cjxb200002020

    GUO Zhigang, YANG Zuosheng, QU Yanhui, et al, Study on composition sedimentary geochemistry of mud area on East China continental shelf[J].Acta Sedimentologica Sinica, 2000, 18 (22) :284-289. http://d.old.wanfangdata.com.cn/Periodical/cjxb200002020
    [2]
    Liu J P, Li A C, Xu K H, et al.Sedimentary features of the Yangtze River-derived alongshore clinoform deposit in the East China Sea[J].Continental Shelf Research, 2006, 26:2141-2156. doi: 10.1016/j.csr.2006.07.013
    [3]
    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, 5 (3) :208-224. doi: 10.1016-j.geomorph.2006.03.023/
    [4]
    Xu K H, Milliman J D, Li A C, et al.Yangtze-and Taiwanderived sediments on the inner shelf of East China Sea[J].Continental Shelf Research, 2009, 29 (18) :2240-2256. doi: 10.1016/j.csr.2009.08.017
    [5]
    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
    [6]
    Xu G, Liu J, Liu S F, et al.Modern muddy deposit along the Zhejiang coast in the East China Sea:response to large-scale human projects[J].Continental Shelf Research, 2016, 130:68-78. doi: 10.1016/j.csr.2016.10.007
    [7]
    李广雪, 杨子赓, 刘勇, 等.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.

    LI Guangxue, YANG Zigeng, LIU Yong, et al.A Study on the Genesis of the Seabed Sedimentary Environment in the Eastern China Sea[M].Beijing:Science Press, 2005.
    [8]
    何起祥, 等.中国海洋沉积地质学[M].北京:海洋出版社, 2006.

    HE Qixiang, et al.Marine sedimentary geology of China[M].Beijing:Ocean Press, 2006.
    [9]
    Liu Z X, Berné S, Saito Y, Yu H J, et al.Internal architecture and mobility of tidal sand ridges in the East China Sea[J].Continental Shelf Research, 2007, 27 (13) :1820-1834. doi: 10.1016/j.csr.2007.03.002
    [10]
    刘保华, 李西双, 赵月霞, 等.冲绳海槽西部陆坡碎屑沉积物的搬运方式:滑塌和重力流[J].海洋与湖沼, 2005, 36 (1) :1-9. doi: 10.3321/j.issn:0029-814X.2005.01.001

    LIU Baohua, LI Xishuang, ZHAO Yuexia, et al.Debris transport of the western continental slope of the Okinawa Trough:Slumping and gravity flowing[J].Oceanologia et Etlimnologia Sinica, 2005, 36 (1) :1-9. doi: 10.3321/j.issn:0029-814X.2005.01.001
    [11]
    杨作升, Milliman J D.长江入海沉积物的输送及其入海后的运移[J].山东海洋学院学报, 1983, 13 (3) :1-12.

    YANG Zuosheng, Milliman J D.Characteristics of sediment transport of Changjiang River and its depsotion in the East China Sea[J].Journal of Shandong College of Oceanology, 1983, 13 (3) :1-12.
    [12]
    翟世奎, 陈志华, 徐善民, 等.冲绳海槽北部稀土元素沉积地球化学研究[J], 海洋地质与第四纪地质, 1996, 16 (2) :47-56. doi: 10.1007/BF02029074

    ZHAI Shikui, CHEN Zhihua, XU Shanmin, et al.Geochemical characteristics of rare earth elements in the sediments of North Okinawa Trough[J].Marine Geology and Quaternary Geology, 1996, 16 (2) :47-56. doi: 10.1007/BF02029074
    [13]
    蒋富清, 李安春.冲绳海槽南部表层沉积物地球化学特征及其物源和环境指示意义[J].沉积学报, 2002, 20 (4) :680-686. doi: 10.3969/j.issn.1000-0550.2002.04.024

    JIANG Fuqing, LI Anchun.Geochemical characteristics and their implications to provenance and environment of surface sediments from the South Okinawa Trough[J].Acta Sedimentologica Sinica, 2002, 20 (4) :680-686. doi: 10.3969/j.issn.1000-0550.2002.04.024
    [14]
    李萍, 李培英, 张晓龙, 等.冲绳海槽沉积物不同粒级的磁性特征及其与环境的关系[J].科学通报, 2005, 50 (3) :262-268. doi: 10.3321/j.issn:0023-074X.2005.03.011

    LI Ping, LI Peiying, ZHANG Xiaolong, et al.Magnetic properties of different grain-sized particles of sediments from the Okinawa Trough and their relationships to sedimentary environment[J].Chinese Science Bulletin, 2005, 50 (3) :262-268. doi: 10.3321/j.issn:0023-074X.2005.03.011
    [15]
    Dou Y G, Yang S Y, Liu Z X, et al.Provenance discrimination of siliciclastic sediments in the middle Okinawa Trough since 30ka:Constraints from rare earth element compositions[J].Marine Geology, 2010, 275 (1-4) :212-220. doi: 10.1016/j.margeo.2010.06.002
    [16]
    Dou Y G, Yang S Y, Liu Z X, et al.Sr-Nd isotopic constraints on terrigenous sediment provenances and Kuroshio Current variability in the Okinawa Trough during the late Quaternary[J].Palaeogeography Palaeoclimatology Palaeoecology, 2012, 365-366 (9) :38-47. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=5597ec4764e737369b98412caa762c73
    [17]
    Dou Y G, Yang S Y, Shi X F, et al.Provenance weathering and erosion records in southern Okinawa Trough sediments since 28 ka:Geochemical and Sr-Nd-Pb isotopic evidences[J].Chemical Geology, 2016, 425:93-109. doi: 10.1016/j.chemgeo.2016.01.029
    [18]
    Wang J Z, Li A C, Xu K H, et al.Clay mineral and grain size studies of sediment provenances and paleoenvironment evolution in the middle Okinawa Trough since 17ka[J].Marine Geology, 2015, 366:49-61. doi: 10.1016/j.margeo.2015.04.007
    [19]
    Chen C T A, Kandasamy S, Chang Y P, et al.Geochemical evidence of the indirect pathway of terrestrial particulate material transport to the Okinawa Trough[J].Quaternary International, 2016, 441:51-61. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=237c2bb966dd73470278a215c385a400
    [20]
    秦蕴珊, 赵一阳, 等.东海地质[M].北京:科学出版社, 1987.

    QIN Yunshan, ZHAO Yiyang, et al.Geology of the East China Sea[M].Beijing:Science Press, 1987.
    [21]
    向荣, 李铁刚, 杨作升, 等.冲绳海槽南部海洋环境改变的地质记录[J].科学通报, 2003, 48 (1) :78-82. http://d.old.wanfangdata.com.cn/Periodical/kxtb200301020

    XIANG Rong, LI Tiegang, YANG Zuosheng, et al.Geological records of marine environmental changes in the southern Okinawa Trough[J].Chinese Science Bulletin, 2003, (2) :194-199. http://d.old.wanfangdata.com.cn/Periodical/kxtb200301020
    [22]
    McManus J.Grain size determination and interpretation[C]//In: Tucker M, ed.Techniques in sedimentology.Blackwell, Oxford, 1988: 63-85.
    [23]
    Biscaye P E.Mineralogy and sedimentation of recent deep-sea clay in the Atlantic Ocean and adjacent seas and oceans[J].GSA Bull, 1965, 76:803-832. doi: 10.1130/0016-7606(1965)76[803:MASORD]2.0.CO;2
    [24]
    Biscaye P E, Grousset F E, Revel M, et al.Asian provenance of glacial dust (stage 2) in the Greenland Ice Sheet Project 2Ice Core, Summit, Greenland[J].Journal of Geophysical Research Oceans, 1997, 102:26765-26781. doi: 10.1029/97JC01249
    [25]
    Folk R L, Andrews P B, Lewis D W.Detrital sedimentary rock classification and nomenclature for use in New Zealand[J].New Zealand Journal of Geology & Geophysics, 1970, 13:937-968.
    [26]
    范德江, 杨作升, 毛登, 等.长江与黄河沉积物中黏土矿物及地化成分的组成[J].海洋地质与第四纪地质, 2001, 21 (4) :7-12. http://www.cnki.com.cn/Article/CJFDTotal-HYDZ200104001.htm

    FAN Dejiang, YANG Zuosheng, MAO Deng, et al.Clay minerals geochemistry of the sediments from the Yangtze and Yellow River[J].Marine Geology and Quaternary Geology, 2001, 21 (4) :7-12. http://www.cnki.com.cn/Article/CJFDTotal-HYDZ200104001.htm
    [27]
    Yang S Y, Jung H S, Lim D, et al.A review on the provenance discrimination of sediments in the Yellow Sea[J].Earth-Science Reviews, 2003, 63:93-120. doi: 10.1016/S0012-8252(03)00033-3
    [28]
    Li C S, Shi X F, Kao S J, et al.Clay mineral composition and their sources for the fluvial sediments of Taiwanese rivers[J].Chinese Science Bulletin, 2012, 57 (6) :673-681. doi: 10.1007/s11434-011-4824-1
    [29]
    Liu Z, Zhao Y, Colin C, et al.Chemical weathering in Luzon, Philippines from clay mineralogy and major-element geochemistry of river sediments[J].Applied Geochemistry, 2009, 24:2195-2205. doi: 10.1016/j.apgeochem.2009.09.025
    [30]
    Gao S, Collins M B.Analysis of grain size trends, for defining sediment transport pathways in marine environments[J].Journal of Coastal Research, 1994, 10 (1) :70-78. doi: 10.1142/S0218127494001350
    [31]
    李粹中.南海中部沉积物的粒度结构和沉积环境[J].东海海洋, 1987, 5 (1-2) :109-116.

    LI Cuizhong.Grain-size parameters and depositional environment of modern sediments in Central South China Sea[J].Donghai Marine Science, 1987, 5 (1-2) :109-116.
    [32]
    杨光复, 董太禄徐善民等东海大陆架南部更新世末期以来的沉积特征[C]//中国科学院海洋研究所海洋地质研究室.黄东海地质.北京: 科学出版社, 1982: 67-81.

    YANG Guangfu, DONG Tailu, XU Shanmin, et al.Sedimentary characteristics on the southern shelf of the East China Sea since late stage of middle Pleistocene[C]//Research Laboratory of Marine Geology in Institute of Oceanology, Chinese Academy of Sciences (ed.).Geology of the Yellow Sea and the East China Sea.Beijing: SciencePress, 1982: 67-81.
    [33]
    王中波, 杨守业, 张志珣, 等.东海陆架中北部沉积物粒度特征及其沉积环境[J].海洋与湖沼, 2012, 43 (6) :1039-1049. http://d.old.wanfangdata.com.cn/Periodical/hyyhz201206003

    WANG Zhongbo, YANG Shouye, ZHANG Zhixun, et al.The grains size compositions of the surface sediments in the East China Sea:Indication for sedimentary environments[J].Oceanologia et Limnologia Sinica, 2012, 43 (6) :1039-1049. http://d.old.wanfangdata.com.cn/Periodical/hyyhz201206003
    [34]
    Yoo D G, Lee C W, Kim S P, et al.Late Quaternary transgressive and highstand systems tracts in the northern East China Sea mid-shelf[J].Marine Geology, 2002, 187:313-328. doi: 10.1016/S0025-3227(02)00384-5
    [35]
    Goff J A, Swift D J P, Duncan S C, et al.High-resolution swath sonar investigations of sand ridge, dune and ribbon morphology in the offshore environment of the New Jersey margin[J].Marine Geology, 1999, 161:307-337. doi: 10.1016/S0025-3227(99)00073-0
    [36]
    Duncan C S, Goff J A, Austin J.Tracking the last sea-level cycle:seafloor morphology and shallow stratigraphy of the latest Quaternary New Jersey middle continental shelf[J].Marine Geology, 2000, 170:395-424. doi: 10.1016/S0025-3227(00)00082-7
    [37]
    徐刚, 刘健, 温春, 等.南黄海西部陆架区表层沉积特征与物源分析[J].海洋地质与第四纪地质, 2010, 30 (4) :49-56. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz201004007

    Xu Gang, Liu Jian, Wen Chun, et al.Sedimentary characteristics and provenance of surficial sediments in the west South Yellow Sea[J].Marine Geology and Quaternary Geology, 2010, 30 (4) :49-56. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz201004007
    [38]
    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, 4:37-45. doi: 10.1016/0278-4343(85)90020-2
    [39]
    沈华悌.东海陆架残留沉积时代和成因模式[J].海洋学报, 1985, 7 (1) :67-77. http://www.hyxb.org.cn/aos/ch/reader/view_abstract.aspx?flag=1&file_no=19850108&journal_id=aos

    SHEN Huati.The residual sedimentary age and genetic model of the East China Sea shelf[J].Acta Oceanologica Sinica, 1985, 7 (1) :67-77. http://www.hyxb.org.cn/aos/ch/reader/view_abstract.aspx?flag=1&file_no=19850108&journal_id=aos
    [40]
    刘锡清.中国陆架的残留沉积[J].海洋地质与第四纪地质, 1987, 7 (1) :1-14. http://www.cnki.com.cn/Article/CJFDTotal-HYDZ198701000.htm

    LIU Xiqing.Relict sediments in China continental shelf[J].Marine Geology and Quaternary Geology, 1987, 7 (1) :1-14. http://www.cnki.com.cn/Article/CJFDTotal-HYDZ198701000.htm
    [41]
    郑浚茂.陆源碎屑沉积环境的粒度标志[D].武汉地质学院北京研究生部, 1982.

    ZHENG Junmao.Granularity markers of terrestrial detrital sedimentary environment[D].Graduate Department of Beijing Institute of Geology, Wuhan, 1982.
    [42]
    李巍然, 杨作升, 王琦, 等.冲绳海槽陆源碎屑峡谷通道搬运与海底扇沉积[J].海洋与湖沼, 2001, 32 (4) :371-380. doi: 10.3321/j.issn:0029-814X.2001.04.004

    LI Weiran, YANG Zuosheng, WANG Qi, et al.Terrigenous transport through canyon and sedimentation of submarine fan in the Okinawa Trough[J].Oceanologia et Limnologia Sinica, 2001, 32 (4) :371-380. doi: 10.3321/j.issn:0029-814X.2001.04.004
    [43]
    袁迎如.冲绳海槽的浊流沉积物[J].地质论评, 1987, 33 (6) :499-505. doi: 10.3321/j.issn:0371-5736.1987.06.001

    YUAN Yingru.Turbidities in the Okinawa Trough[J].Geological review, 1987, 33 (6) :499-505. doi: 10.3321/j.issn:0371-5736.1987.06.001
    [44]
    Honda M, Kusakabe M, Nakabayashi S.Radiocarbon of sediment trap samples from the Okinawa Trough:lateral transport of 14C-poor sediment from the continental slope[J].Marine Chemistry, 2000, 68:231-247. doi: 10.1016/S0304-4203(99)00080-8
    [45]
    Oguri K, Matsumoto E, Yamada M, et al.Sediment accumulation rates and budgets of deposing particles of the East China Sea[J].Deep Sea Research Part Ⅱ, 2003, 50:513-528. doi: 10.1016/S0967-0645(02)00465-4
    [46]
    Iseki K, Okamura K, Kiyomoto Y.Seasonality and composition of downward particulate fluxes at the continental shelf and Okinawa Trough in the East China Sea[J].Deep Sea Research Part Ⅱ, 2003, 50:457-473. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=f469580e853f4132985ed1f276bfb911
    [47]
    杨作升, 郭志刚.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 (2) :81-90. doi: 10.1007/BF02677081

    YANG Zuosheng, GUO Zhigang.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 (2) :81-90. doi: 10.1007/BF02677081
    [48]
    梁小龙, 杨守业, 印萍, 等.黄海与东海周边河流及泥质区沉积物黏土矿物的分布特征和控制因素[J].海洋地质与第四纪地质, 2015, 35 (6) :1-15. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz201506001

    LIANG Xiaolong, YANG Shouye, YIN Ping, et al.Distribution of clay mineral assemblage in the rivers entering Yellow Sea and East China Sea and the muddy shelve deposits and control factors[J].Marine Geology and Quaternary Geology, 2015, 35 (6) :1-15. http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=hydzydsjdz201506001
    [49]
    王亮, 范德江, 李巍然, 等.东海内陆架泥质区百年来黏土矿物组成变化及其环境意义[J].海洋学报, 2015, 37 (5) :87-100. doi: 10.3969/j.issn.0253-4193.2015.05.009

    WANG Liang, FAN Dejing, LI Weiran, et al.The variation of clay minerals contents on the inner shelf of the East China Sea in the last one hundred years and its environmental implications[J].Acta Oceanologica Sinica, 2015, 37 (5) :87-100. doi: 10.3969/j.issn.0253-4193.2015.05.009
    [50]
    Liu Z, Tuo S, Colin C, et al.Detrital fine-grained sediment contribution from Taiwan to the northern South China Sea and its relation to regional ocean circulation[J].Marine Geology, 2008, 255 (3-4) :149-155. doi: 10.1016/j.margeo.2008.08.003
    [51]
    Xu Z K, Li T G, Wan S M, et al.Evolution of East Asian Monsoon:Clay mineral evidence in the western Philippine Sea over the past 700kyr[J].Journal of Asian Earth Sciences, 2012, 60:188-196. doi: 10.1016/j.jseaes.2012.08.018
    [52]
    赵德博, 万世明.冲绳海槽沉积物物源示踪研究进展[J].海洋地质前沿, 2015, 31 (2) :32-41. http://d.old.wanfangdata.com.cn/Periodical/hydzdt201502005

    ZHAO Debo, WAN Shiming.Research progress of tracing sediment sources in Okinawa Trough[J].Marine Geology Frontiers, 2015, 31 (2) :32-41. http://d.old.wanfangdata.com.cn/Periodical/hydzdt201502005
    • Related Articles

  • Related Articles

    [1]DUAN Haoyi, MAO Judong, CHENG Peng, REN Xiaolin, FAN Dejiang. Clay minerals and detrital minerals in clay fraction from the Changjiang River estuary and inner continental shelf of the East China Sea and their provenance indication[J]. Marine Geology & Quaternary Geology, 2024, 44(5): 119-128. DOI: 10.16562/j.cnki.0256-1492.2023092102
    [2]NING Ze, XU Lei, LIN Xuehui, MI Beibei, CONG Jingyi, ZHANG Yong, BI Shipu. Distribution and provenance of detrital minerals in surface sediments of the northeastern East China Sea[J]. Marine Geology & Quaternary Geology, 2022, 42(5): 58-69. DOI: 10.16562/j.cnki.0256-1492.2022062301
    [3]LI Feng, HE Xingliang, XU Gang, CHEN Lilei, LIU Jian. COMPOSITION, DISTRIBUTION AND SOURCE OF FATTY ACIDS AND FATTY ALCOHOLS IN MARINE SURFACE SEDIMENTS OF THE EAST CHINA SEA[J]. Marine Geology & Quaternary Geology, 2016, 36(4): 13-18. DOI: 10.16562/j.cnki.0256-1492.2016.04.002
    [4]LIANG Xiaolong, YANG Shouye, YIN Ping, ZHAO Yun. DISTRIBUTION OF CLAY MINERAL ASSEMBLAGES IN THE RIVERS ENTERING YELLOW SEA AND EAST CHINA SEA AND THE MUDDY SHELVE DEPOSITS AND CONTROL FACTORS[J]. Marine Geology & Quaternary Geology, 2015, 35(6): 1-15. DOI: 10.16562/j.cnki.0256-1492.2015.06.001
    [5]WANG Shutian, LI Bin. NEOTECTONIC FEATURES AND MOVEMENT IN THE EAST CHINA SEA[J]. Marine Geology & Quaternary Geology, 2010, 30(4): 141-150. DOI: 10.3724/SP.J.1140.2010.04141
    [6]GE Qian, CHU Fengyou, LIU Jingpu, DU Yuansheng, XUE Zuo, FANG Yinxia. DISTRIBUTION OF THE CLAY MINERALS IN SURFACE SEDIMENTS OF THE SOUTH CHINA SEA AND THEIR PROVENANCE[J]. Marine Geology & Quaternary Geology, 2010, 30(4): 57-66. DOI: 10.3724/SP.J.1140.2010.04057
    [7]HAN Bo, ZHANG Xunhua, MENG Xiangjun. MAGNETIC FIELD AND BASEMENT FEATURES ANALYSIS IN THE EAST CHINA SEA[J]. Marine Geology & Quaternary Geology, 2010, 30(1): 71-76. DOI: 10.3724/SP.J.1140.2010.01071
    [8]TIAN Shanshan, ZHANG Fuyuan, YAN Lini, XU Xuan. DISTRIBUTION CHARACTERISTICS OF GRANULARITIES OF SURFACE SEDIMENTS IN THE SOUTHWESTERN SHELF OF THE EAST CHINA SEA[J]. Marine Geology & Quaternary Geology, 2009, 29(5): 13-20. DOI: 10.3724/SP.J.1140.2009.05013
    [9]REN Hui-ru, KANG Jian-cheng, WANG Tian-tian, AN Yan. SPATIAL DISTRIBUTION OF WARM CORE OF KUROSHIO IN THE EAST CHINA SEA[J]. Marine Geology & Quaternary Geology, 2008, 28(5): 77-84.
    [10]WANG Ke, ZHENG Hong-bo, Maarten Prins, ZHENG Yan. HIGH-RESOLUTION PALEOENVIRONMENTAL RECORD OF THE MUD SEDIMENTS OF THE EAST CHINA SEA INNER SHELF[J]. Marine Geology & Quaternary Geology, 2008, 28(4): 1-10. DOI: 10.3724/SP.J.1140.2008.03001

Catalog

    Get Citation
    PDF
    XML
    Article views (2627) PDF downloads (36) Cited by()
    Turn off MathJax
    Article Contents
    Abstract
    References
    Related Articles

    Copyright © Marine Geology & Quaternary Geology Editorial Office;   Record No: 鲁ICP备15036216号-7

    Address: 62 Fuzhou South Road, Qingdao City    Post: 266237    Tel: 0532-85755823    E-mail: hydzdsjdz@163.com

    Supported by: Beijing Renhe Information Technology Co., Ltd. support: info@rhhz.net Baidu Analytics

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return