Provenance Study of Core DGKS9617 in the East China Sea

YU Hua; LIU Zhen xia; XIONG Ying qian; LI Wei ran; WANG Kun shan

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Article Navigation > Acta Sedimentologica Sinica > 2004 > 22(4): 651-657

YU Hua, LIU Zhen xia, XIONG Ying qian, LI Wei ran, WANG Kun shan. Provenance Study of Core DGKS9617 in the East China Sea[J]. Acta Sedimentologica Sinica, 2004, 22(4): 651-657.

Citation:

YU Hua, LIU Zhen xia, XIONG Ying qian, LI Wei ran, WANG Kun shan. Provenance Study of Core DGKS9617 in the East China Sea[J]. Acta Sedimentologica Sinica, 2004, 22(4): 651-657.

Provenance Study of Core DGKS9617 in the East China Sea

1.
First Institute of Oceanography, State Oceanic Administration, Qingdao, Shandong 266061;
2.
Ocean University of China, Qingdao, Shandong 266003

Received Date: 2003-12-03
Rev Recd Date: 2004-02-23
Publish Date: 2004-12-10

Abstract

Piston Core DGKS9617, which is located in northern part of the East China Sea, is divided into two sedimentary facies: tidal shallow marine facies (55 851cm), in which tidal current played an important role in the sedimentation of this part, and shallow marine facies (0 55cm). Although the lower and the upper part has different sedimentary environment, the provenance of the whole core does not change. The character of heavy mineral assemblage, the results of discrimination function of Fe, Mn, V, Cr, Ni, Cu, Zn, carbonate analysis and Ba Sr Zn ternary diagram consistently show that the mineral and geochemical characteristics of Core DGKS9617 are similar to the Changjiang River sediment, implying that its sediment is mainly provided by the Changjiang River.
- East China Sea,
- provenance,
- heavy mineral,
- elementary geochemistry

References

[1]	许东禹, 刘锡清, 张训华, 等. 中国近海地质. 北京: 地质出版社, 1997. 62[Xu Dongyu, Liu Xiqing, Zhang Xunhua, et al. China Offshore Geology. Beijing: Geological Publishing House, 1997. 62]
[2]	秦蕴珊, 赵一阳, 陈丽蓉,等. 东海地质. 北京: 科学出版社, 1987. 134～136[Qing Yunshan, Zhao Yiyang, Chen Lirong, et al. Marine Geology of the East China Sea. Beijing: Science Press, 1987. 134～136]
[3]	牛作民. 东海沉积环境分区及其基本特征. 海洋地质与第四纪地质, 1985, 5(2): 27～36[Niu Zuomin. Deposition environment sub-division of the East China Sea and their basic features. Marine Geology and Quaternary Geology, 1985, 5(2): 27～36]
[4]	Milliman J D, Meade R H. World wide delivery of river sediment to the oceans. Journal of Geology, 1983, 91:1～21
[5]	Garver J I, Royce P R, Smick T A. Chromium and Nickel in shale of the Taconic Foreland: a case study for the provenance of fine-grained sediments with an ultramafic source. Journal of Sedimentary Research, 1996, 66(1): 100～106
[6]	Wronkiewcz D J, Condie K C. Geochemistry of Archean shales from the Witwaterstrand Supergroup, South Africa: Source-area weathering and provenance. Geochimica et Cosmochimica Acta, 1987, 51: 2401～2416
[7]	Grigsby J D. Chemical fingerprinting in detrital ilmenite: a variable alternative in provenance research? Journal of Sedimentary Petrology, 1992, 62(2): 331～337
[8]	杨守业, 李从先, 张家强. 苏北滨海平原全新世沉积物物源研究--元素地球化学与重矿物方法比较. 沉积学报, 1999, 17(3): 458-463[Yang Shouye, Li Congxian, Zhang Jiaqiang. Provenance study of Holocene sediments in Subei Coastal Plain-comparison between elemental geochemistry and heavy mineral methods. Acta Sedimentologica Sinica, 1999, 17(3): 458～463]
[9]	李珍, 王永吉, 刘振夏, 等. 东海沉积物中全新世中晚期气候变化的孢粉学证据. 海洋通报, 2001, 20(5): 1-9[Li Zhen, Wang Yongji, Liu Zhenxia, et al. Palynological evidence on climate changes in the East China Sea during the middle and late Holocene. Marine Science Bulletin, 2001, 20(5): 1～9]
[10]	李超, 蓝东兆, 方琦. 东海陆架晚第四纪沉积硅藻及其古海洋学意义. 台湾海峡, 2002, 21(8): 351-359[Li Chao, Lan Dongzhao, Fang Qi. Late Quaternary sedimentary diatom from East China Sea continental shelf and its paleoceanographical significance. Journal of Oceanography in Taiwan Strait, 2002, 21(8): 351～359]
[11]	中国人民共和国国家标准. 海洋调查规范: 海洋地质地球物理调查. 北京: 国家技术监督局, 1993. 27～28[People's Republic of China's standards, Specification for oceanographic survey: Marine geology and geophysics investigation. Beijing: National technology supervising office, 1993. 27～28]
[12]	Zhongyuan Chen, Zhenglou Chen. Quaternary Stratigraphy and Trace-Element Indices of the Yangtze Delta, Eastern China, with Special Reference to Marine Transgressions. Quaternary Research, 1997, 47: 181～191
[13]	Zhen Xia Liu. Yangtze shoal -a modern tidal sand sheet in the northwestern part of the East China Sea. Marine Geology, 1997, 137: 321～330
[14]	Katsuto Uehara, Yoshiki Saito, Kazuaki Hori. Paleotidal regime in the Changjiang (Yangtze) Estuary, the East China Sea, and the Yellow Sea at 6 ka and 10 ka estimated from a numerical model. Marine Geology, 2002, 183: 179～192
[15]	陈丽蓉, 徐文强, 申顺喜. 东海沉积物的矿物组合及其分布特征的研究. 见: 中科院海洋研究所海洋地质室. 黄东海地质. 北京: 科学出版社, 1982. 82-97[Chen Lirong, Xu Wenqiang and Shen Shunxi. Mineral assemblages and their distribution patterns in the sediments of the East China Sea. In: Department of Marine Geology, Institute of Oceanology, Chinese Academy of Sciences. The Geology of the Yellow Sea and the East China Sea. Beijing: Science Press, 1982. 82～97]
[16]	孙白云. 黄河、长江和珠江三角洲沉积物中碎屑矿物的组合特征. 海洋地质与第四纪地质, 1990, 10(3): 23～34[Sun Baiyun. The detrital mineral composes characteristics of the Yellow River, Changjiang and Zhujiang River sediments. Marine Geology and Quaternary Geology, 1990, 10(3): 23～34]
[17]	Liang Juting, Miao Yutian. Near-bottom Sediment Transport in the Changjiang Estuary and on its Adjacent Shelf. Proceedings of International Symposium on sedimentation on the continental shelf, with special reference to the East China Sea, 1983: 536～543
[18]	李双林, 李绍全, 孟祥君. 东海陆架晚第四纪沉积物化学成分及物源示踪. 海洋地质与第四纪地质, 2002, 22(4): 21～28[Li Shuanglin, Li Shaoquan, Meng Xiangjun. Chemical composition and source tracing of late Quaternary sediments in the East China Shelf. Marine Geology and Quaternary Geology, 2002, 22(4): 21～28]
[19]	赵一阳, 鄢明才. 中国浅海沉积物地球化学. 北京: 科学出版社, 1994. 22, 175[Zhao Yiyang, Yan Mingcai. Geochemistry of sediment of the China shelf sea. Beijing: Science Press, 1994. 22, 175]
[20]	Nolting R F, Ramkema A, Everaarts J M. The geochemistry of Cu, Cd, Zn, Ni and Pb in sediment cores from the continental slope of the Banc d'Arguin (Mauritania). Continental Shelf Research, 1999, 19: 665～691
[21]	杨守业, 李从先. 长江与黄河现代表层沉积物元素组成及其示踪作用. 自然科学进展, 1999, 9(10): 930～937[Yang Shouye, Li Congxian. Element composition of modern surface sediment of the Yangtze and Yellow Rivers and its tracing implication. Progress in Natural Science, 1999, 9(10): 930～937]
[22]	范德江, 杨作升, 王文正. 长江、黄河沉积物中碳酸盐组成及差异. 自然科学进展,2002,12(1): 60～64[Fang Dejiang, Yang Zuosheng, Wang Wenzheng. The carbonate composes and differences of the Changjiang and Huanghe Rivers. Progress in Natural Science, 2002,12(1): 60～64]

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通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

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Provenance Study of Core DGKS9617 in the East China Sea

1. First Institute of Oceanography, State Oceanic Administration, Qingdao, Shandong 266061;

2. Ocean University of China, Qingdao, Shandong 266003

Received Date: 2003-12-03

Rev Recd Date: 2004-02-23

Publish Date: 2004-12-10

Key words:

Abstract: Piston Core DGKS9617, which is located in northern part of the East China Sea, is divided into two sedimentary facies: tidal shallow marine facies (55 851cm), in which tidal current played an important role in the sedimentation of this part, and shallow marine facies (0 55cm). Although the lower and the upper part has different sedimentary environment, the provenance of the whole core does not change. The character of heavy mineral assemblage, the results of discrimination function of Fe, Mn, V, Cr, Ni, Cu, Zn, carbonate analysis and Ba Sr Zn ternary diagram consistently show that the mineral and geochemical characteristics of Core DGKS9617 are similar to the Changjiang River sediment, implying that its sediment is mainly provided by the Changjiang River.

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Reference (22)

[1]	许东禹, 刘锡清, 张训华, 等. 中国近海地质. 北京: 地质出版社, 1997. 62[Xu Dongyu, Liu Xiqing, Zhang Xunhua, et al. China Offshore Geology. Beijing: Geological Publishing House, 1997. 62]
[2]	秦蕴珊, 赵一阳, 陈丽蓉,等. 东海地质. 北京: 科学出版社, 1987. 134～136[Qing Yunshan, Zhao Yiyang, Chen Lirong, et al. Marine Geology of the East China Sea. Beijing: Science Press, 1987. 134～136]
[3]	牛作民. 东海沉积环境分区及其基本特征. 海洋地质与第四纪地质, 1985, 5(2): 27～36[Niu Zuomin. Deposition environment sub-division of the East China Sea and their basic features. Marine Geology and Quaternary Geology, 1985, 5(2): 27～36]
[4]	Milliman J D, Meade R H. World wide delivery of river sediment to the oceans. Journal of Geology, 1983, 91:1～21
[5]	Garver J I, Royce P R, Smick T A. Chromium and Nickel in shale of the Taconic Foreland: a case study for the provenance of fine-grained sediments with an ultramafic source. Journal of Sedimentary Research, 1996, 66(1): 100～106
[6]	Wronkiewcz D J, Condie K C. Geochemistry of Archean shales from the Witwaterstrand Supergroup, South Africa: Source-area weathering and provenance. Geochimica et Cosmochimica Acta, 1987, 51: 2401～2416
[7]	Grigsby J D. Chemical fingerprinting in detrital ilmenite: a variable alternative in provenance research? Journal of Sedimentary Petrology, 1992, 62(2): 331～337
[8]	杨守业, 李从先, 张家强. 苏北滨海平原全新世沉积物物源研究--元素地球化学与重矿物方法比较. 沉积学报, 1999, 17(3): 458-463[Yang Shouye, Li Congxian, Zhang Jiaqiang. Provenance study of Holocene sediments in Subei Coastal Plain-comparison between elemental geochemistry and heavy mineral methods. Acta Sedimentologica Sinica, 1999, 17(3): 458～463]
[9]	李珍, 王永吉, 刘振夏, 等. 东海沉积物中全新世中晚期气候变化的孢粉学证据. 海洋通报, 2001, 20(5): 1-9[Li Zhen, Wang Yongji, Liu Zhenxia, et al. Palynological evidence on climate changes in the East China Sea during the middle and late Holocene. Marine Science Bulletin, 2001, 20(5): 1～9]
[10]	李超, 蓝东兆, 方琦. 东海陆架晚第四纪沉积硅藻及其古海洋学意义. 台湾海峡, 2002, 21(8): 351-359[Li Chao, Lan Dongzhao, Fang Qi. Late Quaternary sedimentary diatom from East China Sea continental shelf and its paleoceanographical significance. Journal of Oceanography in Taiwan Strait, 2002, 21(8): 351～359]
[11]	中国人民共和国国家标准. 海洋调查规范: 海洋地质地球物理调查. 北京: 国家技术监督局, 1993. 27～28[People's Republic of China's standards, Specification for oceanographic survey: Marine geology and geophysics investigation. Beijing: National technology supervising office, 1993. 27～28]
[12]	Zhongyuan Chen, Zhenglou Chen. Quaternary Stratigraphy and Trace-Element Indices of the Yangtze Delta, Eastern China, with Special Reference to Marine Transgressions. Quaternary Research, 1997, 47: 181～191
[13]	Zhen Xia Liu. Yangtze shoal -a modern tidal sand sheet in the northwestern part of the East China Sea. Marine Geology, 1997, 137: 321～330
[14]	Katsuto Uehara, Yoshiki Saito, Kazuaki Hori. Paleotidal regime in the Changjiang (Yangtze) Estuary, the East China Sea, and the Yellow Sea at 6 ka and 10 ka estimated from a numerical model. Marine Geology, 2002, 183: 179～192
[15]	陈丽蓉, 徐文强, 申顺喜. 东海沉积物的矿物组合及其分布特征的研究. 见: 中科院海洋研究所海洋地质室. 黄东海地质. 北京: 科学出版社, 1982. 82-97[Chen Lirong, Xu Wenqiang and Shen Shunxi. Mineral assemblages and their distribution patterns in the sediments of the East China Sea. In: Department of Marine Geology, Institute of Oceanology, Chinese Academy of Sciences. The Geology of the Yellow Sea and the East China Sea. Beijing: Science Press, 1982. 82～97]
[16]	孙白云. 黄河、长江和珠江三角洲沉积物中碎屑矿物的组合特征. 海洋地质与第四纪地质, 1990, 10(3): 23～34[Sun Baiyun. The detrital mineral composes characteristics of the Yellow River, Changjiang and Zhujiang River sediments. Marine Geology and Quaternary Geology, 1990, 10(3): 23～34]
[17]	Liang Juting, Miao Yutian. Near-bottom Sediment Transport in the Changjiang Estuary and on its Adjacent Shelf. Proceedings of International Symposium on sedimentation on the continental shelf, with special reference to the East China Sea, 1983: 536～543
[18]	李双林, 李绍全, 孟祥君. 东海陆架晚第四纪沉积物化学成分及物源示踪. 海洋地质与第四纪地质, 2002, 22(4): 21～28[Li Shuanglin, Li Shaoquan, Meng Xiangjun. Chemical composition and source tracing of late Quaternary sediments in the East China Shelf. Marine Geology and Quaternary Geology, 2002, 22(4): 21～28]
[19]	赵一阳, 鄢明才. 中国浅海沉积物地球化学. 北京: 科学出版社, 1994. 22, 175[Zhao Yiyang, Yan Mingcai. Geochemistry of sediment of the China shelf sea. Beijing: Science Press, 1994. 22, 175]
[20]	Nolting R F, Ramkema A, Everaarts J M. The geochemistry of Cu, Cd, Zn, Ni and Pb in sediment cores from the continental slope of the Banc d'Arguin (Mauritania). Continental Shelf Research, 1999, 19: 665～691
[21]	杨守业, 李从先. 长江与黄河现代表层沉积物元素组成及其示踪作用. 自然科学进展, 1999, 9(10): 930～937[Yang Shouye, Li Congxian. Element composition of modern surface sediment of the Yangtze and Yellow Rivers and its tracing implication. Progress in Natural Science, 1999, 9(10): 930～937]
[22]	范德江, 杨作升, 王文正. 长江、黄河沉积物中碳酸盐组成及差异. 自然科学进展,2002,12(1): 60～64[Fang Dejiang, Yang Zuosheng, Wang Wenzheng. The carbonate composes and differences of the Changjiang and Huanghe Rivers. Progress in Natural Science, 2002,12(1): 60～64]

Provenance Study of Core DGKS9617 in the East China Sea

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