Detrital zircon U-Pb age and provenance discrimination in sediments of the central mud area in the South Yellow Sea
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摘要:
对南黄海中部泥质区南侧4个表层沉积物和SYS90-1A孔中5个沉积物样品进行碎屑锆石U-Pb定年，具体分析了研究区表层沉积物物源差异及约1.0 Ma以来沉积物物源变化。结果显示，泥质区沉积物主要来自黄河，而泥质区外部南侧沉积物可能主要由长江供应。SYS90-1A孔主要记录了早更新世晚期以来的沉积记录，不同时期物源差异明显：中更新世早期以长江源物质为主，利用磁化率开展旋回地层学分析，根据天文年代调谐确定该时期具体时代为0.59～0.71 Ma；早更新世晚期至中更新世以及中更新世中期以来以黄河源物质为主。这一结果与前人关于南黄海早更新世以来沉积物以黄河源物质为主的认识不同，长江源物质对南黄海泥质区沉积物贡献需要重新认识。上述表层沉积物样品和钻孔沉积物样品碎屑锆石U-Pb年龄分布与朝鲜半岛河流沉积物完全不同，说明该区域自早更新世晚期以来沉积物主要来自中国大陆。
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关键词:
- 中部泥质区 /
- 碎屑锆石U-Pb年龄 /
- 物源判别 /
- 南黄海
Abstract:Detrital zircons taken from four surface sediments and five sediment samples from SYS90-1A borehole in the southern part of the central mud area of the South Yellow Sea was U-Pb dated and their provenances were discriminated, based on which the changes since about 1.0 Ma in the provenance of the sediment samples were analyzed. Results show that the sediments in the mud area are mainly from the Yellow River, and the sediments in the south of the mud area may be transported by the Yangtze River. The borehole SYS90-1A mainly records the deposits since the late Early Pleistocene, showing obvious provenance differences in different stages. In the early Middle Pleistocene, the sediments were mainly transported from the Yangtze River; and cyclic stratigraphy that was determined based on magnetic susceptibility and astronomical chronology tuning showed that the specific time of the stage is 590~710 ka. From the late early Pleistocene to the middle Pleistocene and since the middle Pleistocene, the sediments were mainly from the Yellow River. This result is different from the previous understanding that the sediments in the South Yellow Sea since the Early Pleistocene were mainly derived from the Yellow River, and the contribution of the sediments from the Yangtze River to the mud area needs to be re-recognized. The detrital zircon U-Pb age distribution of all samples is completely different from that of the fluvial sediments of the Korean Peninsula, indicating that the sediments in this area are mainly from mainland China since the late Early Pleistocene.
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表 1 沉积物样品位置及岩性信息
Table 1. Samples location and lithology information
序号 样品编号 位置 埋深/m 岩性 备注 1 SYB80 33°27′15″N、 123°17′46″E 0.20 粉砂 表层样 2 SYB86 33°05′40″N、124°24′17″E 0.20 粉砂 表层样 3 SYB198 33°05′40″N、124°44′02″E 0.20 粉砂 表层样 4 SYB256 33°05′40″N、124°03′48″E 0.20 粉砂 表层样 5 SYS90-1A-B709 33°48′49″N、 123°43′58″E 34.88 粉砂 钻孔样 6 SYS90-1A-C717 33°48′49″N、 123°43′58″E 56.20 细砂 钻孔样 7 SYS90-1A-D235 33°48′49″N、 123°43′58″E 68.88 粉砂 钻孔样 8 SYS90-1A-D275 33°48′49″N、123°43′58″E 69.68 粉砂 钻孔样 9 SYS90-1A-D945 33°48′49″N、123°43′58″E 85.66 粉砂 钻孔样 
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表 2 第一组样品不同年龄区间锆石比例
Table 2. The proportion of zircons in different ages of the first group of samples
% 样品编号 ＜100 Ma 100～300 Ma 300～500 Ma 600～1100 Ma 1300～1500 Ma 1800～2000 Ma 2300～2700 Ma SYS90-1A-C717 1 27 13 27 4 16 12 SYS90-1A-D235 4 26 11 35 2 6 17 SYB86 0 44 11 18 4 18 5 SYB198 3 54 13 21 2 5 2 SYB256 3 33 13 18 3 19 11
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表 3 第二组样品不同年龄区间锆石比例
Table 3. The proportion of zircons in different ages of the second group of samples
% 样品编号 ＜200 Ma 200～300 Ma 350～500 Ma 600～1100 Ma 1300～1500 Ma 1800～2000 Ma 2000～2600 Ma SYS90-1A-B709 4 21 11 23 6 23 13 SYS90-1A-D275 3 13 12 41 3 16 13 SYS90-1A-D945 2 22 13 26 2 22 15 SYB80 2 21 9 35 4 15 15
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[1] 石学法, 乔淑卿, 杨守业, 等. 亚洲大陆边缘沉积学研究进展(2011-2020)[J]. 矿物岩石地球化学通报, 2021, 40(2):319-336
SHI Xuefa, QIAO Shuqing, YANG Shouye, et al. Progress in sedimentology research of the Asian continental margin (2011-2020) [J]. Bulletin of Mineralogy, Petrology and Geochemistry, 2021, 40(2): 319-336.
[2] 杨守业. 亚洲主要河流的沉积地球化学示踪研究进展[J]. 地球科学进展, 2006, 21(6):648-655 doi: 10.3321/j.issn:1001-8166.2006.06.013
YANG Shouye. Advances in sedimentary geochemistry and tracing applications of Asian rivers [J]. Advances in Earth Science, 2006, 21(6): 648-655. doi: 10.3321/j.issn:1001-8166.2006.06.013
[3] 汪品先, 翦知湣. 探索南海深部的回顾与展望[J]. 中国科学:地球科学, 2019, 62(10):1473-1488 doi: 10.1007/s11430-019-9484-4
WANG Pinxian, JIAN Zhimin. Exploring the deep South China Sea: retrospects and prospects [J]. Science China Earth Sciences, 2019, 62(10): 1473-1488. doi: 10.1007/s11430-019-9484-4
[4] Shackleton N J, Hall M A, Pate D. Pliocene stable isotope stratigraphy of site 846 [J]. Proceedings of the Ocean Drilling Program, Scientific Results, 1995, 138: 337-355.
[5] Mix A C, Le J, Shackleton N J. Benthic foraminiferal stable isotope stratigraphy of Site 846: 0-1.8 Ma [J]. Proceedings of the Ocean Drilling Program, Scientific Results, 1995, 138: 839-856.
[6] 张勇, 姚永坚, 李学杰, 等. 中生代以来东亚洋陆汇聚带多圈层动力下的中国海及邻区构造演化及资源环境效应[J]. 中国地质, 2020, 47(5):1271-1309
ZHANG Yong, YAO Yongjian, LI Xuejie, et al. Tectonic evolution and resource-environmental effect of China Seas and adjacent areas under the multisphere geodynamic system of the East Asia ocean-continent convergent belt since Mesozoic [J]. Geology in China, 2020, 47(5): 1271-1309.
[7] 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(l-2): 93-120.
[8] 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 doi: 10.16562/j.cnki.0256-1492.1999.01.003
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): 13-24. doi: 10.16562/j.cnki.0256-1492.1999.01.003
[9] 刘健, 段宗奇, 梅西, 等. 南黄海中部隆起晚新近纪-第四纪沉积序列的地层划分与沉积演化[J]. 海洋地质与第四纪地质, 2021, 41(5):25-43
LIU Jian, DUAN Zongqi, MEI Xi, et al. Stratigraphic classification and sedimentary evolution of the late Neogene to Quaternary sequence on the Central Uplift of the South Yellow Sea [J]. Marine Geology & Quaternary Geology, 2021, 41(5): 25-43.
[10] 卢健, 李安春. 南黄海表层沉积物粒度特征季节变化及其影响因素[J]. 海洋科学, 2015, 39(3):48-58 doi: 10.11759/hykx20140527001
LU Jian, LI Anchun. Seasonal variations and influencing factors of the grain size characteristics of surface sediments in the South Yellow Sea [J]. Marine Sciences, 2015, 39(3): 48-58. doi: 10.11759/hykx20140527001
[11] 秦蕴珊, 赵一阳, 陈丽蓉, 等. 黄海地质[M]. 北京: 海洋出版社, 1989: 1-289
QIN Yunshan, ZHAO Yiyang, CHEN Lirong, et al. Geology of the Yellow Sea[M]. Beijing: Oceanic Publish House, 1989: 1-289.
[12] 魏建伟, 石学法, 辛春英, 等. 南黄海黏土矿物分布特征及其指示意义[J]. 科学通报, 2003, 48(1):7-11
WEI Jianwei, SHI Xuefa, XIN Chunying, et al. Clay mineral distributions in the southern Yellow Sea and their significance [J]. Chinese Science Bulletin, 2003, 48(1): 7-11.
[13] Milliman J D, Farnsworth K L. River Discharge to the Coastal Ocean: A Global Synthesis[M]. Cambridge: Cambridge University Press, 2011.
[14] Qiao S Q, Shi X F, Wang G Q, et al. Sediment accumulation and budget in the Bohai Sea, Yellow Sea and East China Sea [J]. Marine Geology, 2017, 390: 270-281. doi: 10.1016/j.margeo.2017.06.004
[15] Yao Z Q, Shi X F, Qiao S Q, et al. Persistent effects of the Yellow River on the Chinese marginal seas began at least ~ 880 ka ago [J]. Scientific Reports, 2017, 7(1): 2827. doi: 10.1038/s41598-017-03140-x
[16] 何梦颖, 梅西, 张训华, 等. 南黄海陆架区CSDP-1孔沉积物碎屑锆石U-Pb年龄物源判别[J]. 吉林大学学报:地球科学版, 2019, 49(1):85-95
HE Mengying, MEI Xi, ZHANG Xunhua, et al. Provenance discrimination of detrital zircon U-Pb dating in the core CSDP-l in the continental shelf of South Yellow Sea [J]. Journal of Jilin University: Earth Science Edition, 2019, 49(1): 85-95.
[17] Stevens T, Carter A, Watson T P, et al. Genetic linkage between the Yellow River, the Mu Us desert and the Chinese Loess Plateau [J]. Quaternary Science Reviews, 2013, 78: 355-368. doi: 10.1016/j.quascirev.2012.11.032
[18] Vermeesch P, Garzanti E. Making geological sense of 'Big Data' in sedimentary provenance analysis [J]. Chemical Geology, 2015, 409: 20-27. doi: 10.1016/j.chemgeo.2015.05.004
[19] Fedo C M, Sircombe K N, Rainbird R H. Detrital zircon analysis of the sedimentary record [J]. Reviews in Mineralogy and Geochemistry, 2003, 53(1): 277-303. doi: 10.2113/0530277
[20] Gehrels G E, Valencia V A, Ruiz J. Enhanced precision, accuracy, efficiency, and spatial resolution of U-Pb ages by laser ablation-multicollector-inductively coupled plasma-mass spectrometry [J]. Geochemistry, Geophysics, Geosystems, 2008, 9(3): Q03017. doi: 10.1029/2007GC001805
[21] Shaulis B, Lapen T J, Toms A. Signal linearity of an extended range pulse counting detector: applications to accurate and precise U-Pb dating of zircon by laser ablation quadrupole ICP-MS [J]. Geochemistry, Geophysics, Geosystems, 2010, 11(11): Q0AA11. doi: 10.1029/2010GC003198
[22] 许东禹, 刘锡清, 张训华, 等. 中国近海地质[M]. 北京: 地质出版社, 1997: 1-80
XU Dongyu, LIU Xiqing, ZHANG Xunhua, et al. China Offshore Geology[M]. Beijing: Geological Publishing House, 1997: 1-80.
[23] 刘忠臣, 刘保华, 黄振宗, 等. 中国近海及邻近海域地形地貌[M]. 北京: 海洋出版社, 2005: 1-96
LIU Zhongchen, LIU Baohua, HUANG Zhenzong, et al. Topography and Geomorphology of China's Offshore and Adjacent Areas[M]. Beijing: Oceanic Publish House, 2005: 1-96.
[24] 苏纪兰. 中国近海的环流动力机制研究[J]. 海洋学报, 2001, 23(3):1-16
SU Jilan. A review of circulation dynamics of the coastal oceans near China [J]. Acta Oceanologica Sinica, 2001, 23(3): 1-16.
[25] 梅西, 李学杰, 密蓓蓓, 等. 中国海域表层沉积物分布规律及沉积分异模式[J]. 中国地质, 2020, 47(5):1447-1462
MEI Xi, LI Xuejie, MI Beibei, et al. Distribution regularity and sedimentary differentiation patterns of China seas surface sediments [J]. Geology in China, 2020, 47(5): 1447-1462.
[26] 梅西, 张训华, 刘健, 等. 南黄海3.50Ma以来海陆环境演变的元素地球化学记录[J]. 吉林大学学报:地球科学版, 2019, 49(1):74-84
MEI Xi, ZHANG Xunhua, LIU Jian, et al. Elemental geochemical record of land and sea environmental evolution since 3.50 Ma in South Yellow Sea [J]. Journal of Jilin University:Earth Science Edition, 2019, 49(1): 74-84.
[27] 任纪舜. 新一代中国大地构造图: 中国及邻区大地构造图(1: 5000000)附简要说明: 从全球看中国大地构造[J]. 地球学报, 2003, 24(1):1-2 doi: 10.3321/j.issn:1006-3021.2003.01.001
REN Jishun. The new generation geotectonic map of China-geotectonic map of China and adjacent areas (1: 5000000) a brief description: Chinese geotectonics in a global view [J]. Acta Geoscientia Sinica, 2003, 24(1): 1-2. doi: 10.3321/j.issn:1006-3021.2003.01.001
[28] Shao L, Li C A, Yuan S Y, et al. Neodymium isotopic variations of the late Cenozoic sediments in the Jianghan Basin: implications for sediment source and evolution of the Yangtze River [J]. Journal of Asian Earth Sciences, 2012, 45: 57-64. doi: 10.1016/j.jseaes.2011.09.018
[29] 何梦颖, 郑洪波, 贾军涛. 长江现代沉积物碎屑锆石U-Pb年龄及Hf同位素组成与物源示踪研究[J]. 第四纪研究, 2013, 33(4):656-670 doi: 10.3969/j.issn.1001-7410.2013.04.04
HE Mengying, ZHENG Hongbo, JIA Juntao. Detrital zircon U-Pb dating and Hf isotope of modern sediments in the Yangtze River: implications for the sediment provenance [J]. Quaternary Sciences, 2013, 33(4): 656-670. doi: 10.3969/j.issn.1001-7410.2013.04.04
[30] 许志琴, 侯立玮, 王宗秀, 等. 中国松潘-甘孜造山带的造山过程[M]. 北京: 地质出版社, 1992
XU Zhiqin, HOU Liwei, WANG Zongxiu, et al. Orogenic Processes of the Songpan Ganze Orogenic Belt of China[M]. Beijing: Geological Publishing House, 1992.
[31] 岳保静, 廖晶. 黄河流域现代沉积物碎屑锆石U-Pb年龄物源探讨[J]. 海洋地质与第四纪地质, 2016, 36(5):109-119 doi: 10.16562/j.cnki.0256-1492.2016.05.011
YUE Baojing, LIAO Jing. Provenance study of Yellow River sediments by U-Pb dating of the detrital zircons [J]. Marine Geology & Quaternary Geology, 2016, 36(5): 109-119. doi: 10.16562/j.cnki.0256-1492.2016.05.011
[32] 林旭, 刘静, 吴中海, 等. 环渤海湾盆地主要河流碎屑锆石U-Pb年龄特征及其物源示踪意义[J]. 海洋地质与第四纪地质, 2021, 41(2):136-145 doi: 10.16562/j.cnki.0256-1492.2020062201
LIN Xu, LIU Jing, WU Zhonghai, et al. U-Pb age characteristics of major fluvial detrital zircons in the Bohai Bay Basin and their provenance implications [J]. Marine Geology & Quaternary Geology, 2021, 41(2): 136-145. doi: 10.16562/j.cnki.0256-1492.2020062201
[33] Choi T, Lee Y I, Orihashi Y, et al. The provenance of the southeastern Yellow Sea sediments constrained by detrital zircon U-Pb age [J]. Marine Geology, 2013, 337: 182-194. doi: 10.1016/j.margeo.2013.01.007
[34] Bintanja R, van de Wal R S W, Oerlemans J. Modelled atmospheric temperatures and global sea levels over the past million years [J]. Nature, 2005, 437(7055): 125-128. doi: 10.1038/nature03975
[35] Paton C, Woodhead J D, Hellstrom J C, et al. Improved laser ablation U-Pb zircon geochronology through robust downhole fractionation correction [J]. Geochemistry, Geophysics, Geosystems, 2010, 11(3): Q0AA06.
[36] Thompson J M, Meffre S, Danyushevsky L. Impact of air, laser pulse width and fluence on U-Pb dating of zircons by LA-ICPMS [J]. Journal of Analytical Atomic Spectrometry, 2018, 33(2): 221-230. doi: 10.1039/C7JA00357A
[37] Compston W, Williams I S, Kirschvink J L, et al. Zircon U-Pb ages for the Early Cambrian time-scale [J]. Journal of the Geological Society, 1992, 149(2): 171-184. doi: 10.1144/gsjgs.149.2.0171
[38] 吴元保, 郑永飞. 锆石成因矿物学研究及其对U-Pb年龄解释的制约[J]. 科学通报, 2004, 49(15):1554-1569 doi: 10.3321/j.issn:0023-074X.2004.16.002
WU Yuanbao, ZHENG Yongfei. Genesis of zircon and its constraints on interpretation of U-Pb age [J]. Chinese Science Bulletin, 2004, 49(15): 1554-1569. doi: 10.3321/j.issn:0023-074X.2004.16.002
[39] Vermeesch P. IsoplotR: a free and open toolbox for geochronology [J]. Geoscience Frontiers, 2018, 9(5): 1479-1493. doi: 10.1016/j.gsf.2018.04.001
[40] 贾军涛, 郑洪波, 杨守业. 长江流域岩体的时空分布与碎屑锆石物源示踪[J]. 同济大学学报:自然科学版, 2010, 38(9):1375-1380
JIA Juntao, ZHENG Hongbo, YANG Shouye. Rock types in Yangtze drainage and their implications for zircon U-Pb provenance study of Yangtze sediments [J]. Journal of Tongji University:Natural Science, 2010, 38(9): 1375-1380.
[41] Yang J, Gao S, Chen C, et al. Episodic crustal growth of North China as revealed by U–Pb age and Hf isotopes of detrital zircons from modern rivers [J]. Geochimica et Cosmochimica Acta, 2009, 73(9): 2660-2673. doi: 10.1016/j.gca.2009.02.007
[42] Liang Z W, Gao S, Hawkesworth C J, et al. Step-like growth of the continental crust in South China: evidence from detrital zircons in Yangtze River sediments [J]. Lithos, 2018, 320-321: 155-171. doi: 10.1016/j.lithos.2018.09.011
[43] 向芳, 杨栋, 田馨, 等. 湖北宜昌地区第四纪沉积物中锆石的U-Pb年龄特征及其物源意义[J]. 矿物岩石, 2011, 31(2):106-114 doi: 10.3969/j.issn.1001-6872.2011.02.015
XIANG Fang, YANG Dong, TIAN Xin, et al. LA-ICP-MS U-Pb geochronology of zircons in the Quaternary sediments from the Yichang area of Hubei Province and its provenance significance [J]. Journal of Mineralogy and Petrology, 2011, 31(2): 106-114. doi: 10.3969/j.issn.1001-6872.2011.02.015
[44] Li Z X, Li X H, Zhou H W, et al. Grenvillian continental collision in south China: new SHRIMP U-Pb zircon results and implications for the configuration of Rodinia [J]. Geology, 2002, 30(2): 163-166. doi: 10.1130/0091-7613(2002)030<0163:GCCISC>2.0.CO;2
[45] Zhang C L, Li M, Wang T, et al. U-Pb zircon geochronology and geochemistry of granitoids in the Douling Group in the eastern Qinling [J]. Acta Geologica Sinica, 2004, 78(1): 83-95.
[46] Vermeesch P. Multi-sample comparison of detrital age distributions [J]. Chemical Geology, 2013, 341: 140-146. doi: 10.1016/j.chemgeo.2013.01.010
[47] Yi L, Chen S L, Ortiz J D, et al. 1500-year cycle dominated Holocene dynamics of the Yellow River delta, China [J]. The Holocene, 2016, 26(2): 222-234. doi: 10.1177/0959683615596834
[48] Kong G S, Park S C, Han H C, et al. Late Quaternary paleoenvironmental changes in the southeastern Yellow Sea, Korea [J]. Quaternary International, 2006, 144(1): 38-52. doi: 10.1016/j.quaint.2005.05.011
[49] Zhou X, Sun L G, Huang W, et al. Relationship between magnetic susceptibility and grain size of sediments in the China Seas and its implications [J]. Continental Shelf Research, 2014, 72: 131-137. doi: 10.1016/j.csr.2013.07.011
[50] 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(1-4): 45-67. doi: 10.1016/j.margeo.2004.06.009
[51] 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
[52] Zhou X, Sun L G, Huang W, et al. Precipitation in the Yellow River drainage basin and East Asian monsoon strength on a decadal time scale [J]. Quaternary Research, 2012, 78(3): 486-491. doi: 10.1016/j.yqres.2012.07.008
[53] Zhou X, Jia N, Cheng W H, et al. Relocation of the Yellow River estuary in 1855 AD recorded in the sediment core from the northern Yellow Sea [J]. Journal of Ocean University of China, 2013, 12(4): 624-628. doi: 10.1007/s11802-013-2199-4
[54] 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(6-7): 667-695. doi: 10.1016/S0278-4343(00)00102-3
[55] 王飞飞, 刘健, 仇建东, 等. 南黄海中西部全新世中期以来泥质沉积厚度与成因[J]. 海洋地质与第四纪地质, 2014, 34(5):1-11
WANG Feifei, LIU Jian, QIU Jiandong, et al. 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.
[56] 李铁刚, 李绍全, 苍树溪, 等. YSDP102钻孔有孔虫动物群与南黄海东南部古水文重建[J]. 海洋与湖沼, 2000, 31(6):588-595 doi: 10.3321/j.issn:0029-814X.2000.06.002
LI Tiegang, LI Shaoquan, CANG Shuxi, et al. Paleo-hydrological reconstruction of the southern Yellow Sea inferred from foraminiferal fauna in core YSDP102 [J]. Oceanologia et Limnologia Sinica, 2000, 31(6): 588-595. doi: 10.3321/j.issn:0029-814X.2000.06.002
[57] 王利波, 杨作升, 赵晓辉, 等. 南黄海中部泥质区YE-2孔8.4 ka BP来的沉积特征[J]. 海洋地质与第四纪地质, 2009, 29(5):1-11
WANG Libo, YANG Zuosheng, ZHAO Xiaohui, et al. Sedimentary characteristics of core YE-2 from the central mud area in the South Yellow Sea during last 8400 years and its interspace coarse layers [J]. Marine Geology & Quaternary Geology, 2009, 29(5): 1-11.
[58] 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 - 10 sediments in the central Yellow Sea mud area and implications for provenance changes [J]. Acta Sedimentologica Sinica, 2021, 39(2): 383-394.
[59] 胡刚, 张勇, 孔祥淮, 等. 全新世中国大河三角洲沉积演化模式转化及其对人类活动的响应[J]. 海洋地质与第四纪地质, 2021, 41(5):77-89 doi: 10.16562/j.cnki.0256-1492.2020122201
HU Gang, ZHANG Yong, KONG Xianghuai, et al. Changes of evolution models of China's large river deltas since Holocene and their responses to anthropogenic activities [J]. Marine Geology & Quaternary Geology, 2021, 41(5): 77-89. doi: 10.16562/j.cnki.0256-1492.2020122201
[60] 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. 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
[61] 刘德政, 夏非. 江苏中部海岸晚第四纪沉积物的粒度与磁化率特征及其古环境意义[J]. 海洋地质与第四纪地质, 2021, 41(5):210-220 doi: 10.16562/j.cnki.0256-1492.2021051901
LIU Dezheng, XIA Fei. Characteristics of grain size and magnetic susceptibility of the Late Quaternary sediments from core 07SR01 in the middle Jiangsu coast and their paleoenvironmental significances [J]. Marine Geology & Quaternary Geology, 2021, 41(5): 210-220. doi: 10.16562/j.cnki.0256-1492.2021051901
[62] Zhang J, Wan S M, Clift P D, et al. History of Yellow River and Yangtze River delivering sediment to the Yellow Sea since 3.5 Ma: tectonic or climate forcing? [J]. Quaternary Science Reviews, 2019, 216: 74-88. doi: 10.1016/j.quascirev.2019.06.002
[63] 杨子赓. Olduvai亚时以来南黄海沉积层序及古地理变迁[J]. 地质学报, 1993, 67(4):357-366
YANG Zigeng. The sedimentary sequence and palaeogeographic changes of the South Yellow Sea since the Olduvai subchron [J]. Acta Geologica Sinica, 1993, 67(4): 357-366.
[64] 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(1-4): 54-76. doi: 10.1016/j.margeo.2010.09.003
[65] Liu J X, Liu Q S, Zhang X H, et al. Magnetostratigraphy of a long Quaternary sediment core in the South Yellow sea [J]. Quaternary Science Reviews, 2016, 144: 1-15. doi: 10.1016/j.quascirev.2016.05.025
[66] Liu J, Zhang X H, Mei X, et al. The sedimentary succession of the last~3.50 Myr in the western South Yellow Sea: paleoenvironmental and tectonic implications [J]. Marine Geology, 2018, 399: 47-65. doi: 10.1016/j.margeo.2017.11.005
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