GEOCHEMISTRY OF REE AND PROVENANCE OF SURFACE SEDIMENTS IN THE LITTORAL AREA OF THE NORTHEASTERN SHANDONG PENINSULA

KONG Xiang-huai; LIU Jian; LI Wei-ran; ZHANG Xian-jun; LIANG Yuan

Marine Geology & Quaternary Geology > 2007 > 27(3): 51-59.

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.

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GEOCHEMISTRY OF REE AND PROVENANCE OF SURFACE SEDIMENTS IN THE LITTORAL AREA OF THE NORTHEASTERN SHANDONG PENINSULA

1 Qingdao Institute of Marine Geology, Qingdao 266071, China;
2 College of Marine Geosciences, Ocean University of China, Qingdao 266100, China

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Received Date: January 25, 2006
Revised Date: March 25, 2007

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Abstract

Abstract

Analyses of REEs content and grain size of 306 surface sediment samples derived from the littoral area of the northeastern Shandong Peninsula were carried out to make a study of geochemical characteristics of REE and provenance of surface sediments in the study area. The results indicate that the distribution of gross amount of REE in surface sediments well corresponds to that of the sediment types. The high value area spreading from northwest to southeast in the form of a tongue approximately corresponds to silt area, and the low value area corresponds to sandy silt or silty sand area, showing that the grain size is the main factor controlling the distribution of REE in the study area. The chondrite-normalized and UCC-normalized patterns of REEs in the sediments of study area are very close to those of sediment loads discharged from the Yellow River. It is justified by the comparison based on the ratio of some stable elements that sediments derived from the study area and discharged from the Yelow River have the same provenance.
- surface sediments,
- rare earth element,
- provenance,
- geochemistry,
- the littoral area of the northeastern Shandong Peninsula

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[1]	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[J].自然科学进展,1999,10(9):930.[YANG Shou-ye,LI Cong-xian. Element component and tracing application in the Yangtze River and the Yellow River modern surface sediments[J]. Progress in Natural Science,1999 ,10(9):930.]
[2]	孔祥淮,刘健,李巍然,等.山东半岛东北部滨浅海区表层沉积物粒度及矿物成分[J]. 海洋地质与第四纪地质,2006,16(3):21-29. [KONG Xiang-huai,LIU Jian,LI Wei-ran,et al. Grain-size characters and mineral components of surface sediments in the offshore area of northeastern Shandong Peninsula[J]. Marine Geology and Quaternary Geology,2006,16(3):21-29.]
[3]	Greaves M J,Elderfield H,Sholkovitz E R. Aeolian sources of rare earth elements to the Western Pacific Ocean[J]. Marine Chemistry,1999,68:31-38.
[4]	Byrne R H,Sholkovitz E R. The Marine Chemistry and Geochemistry of the Lanthanides[M]//The Handbook of the Physics and Chemistry of Rare Earths.Elsevier,1996:497-593.
[5]	赵志根.不同球粒陨石平均值对稀土元素参数的影响[J].标准化报道,2000,21(3):16.[ZHAO Zhi-gen. Effect of different chondrite on the parameter of rare-earth elements[J]. Reporting of Standardization,2000 ,21(3):16.]
[6]	Taylor S R,Mclennan S M. The continental crust:Its composition and evolution[M]. 1985:312.
[7]	王金土.黄海表层沉积物稀土元素地球化学特征[J].地球化学,1990(1):44-53.[WANG Jin-tu. Geochemical characters of REEs in the Huanghai Sea surface sediments[J]. Geochimica,1990 (1):44-53.]
[8]	赵一阳,鄢明才. 中国浅海沉积物地球化学[M]. 北京:科学出版社,1994:130-150.[ZHAO Yi-yang,YAN Ming-cai. Geochemistry of Sediments of the China Shelf Sea[M]. Bejing:Science Press,1994:130 -150.]
[9]	Caggianelli A,Fiore S,Mongelli G,et al. REE distribution in the clay fraction of pelites from the southern Apennines,Italy[J]. Chemical Geology,1992, 99:253-263.
[10]	王中刚,于学元,赵振华,等.稀土元素地球化学[M].北京:科学出版社,1989:88-93.[WANG Zhong-gang,YU Xue-yuan, ZHAO Zhen-hua,et al. Geochemistry of Rare Earth Element[M].Beijing:Science Press,1989:88 -93.]
[11]	Nesbitt H W. Mobility and fractionation of rare earth elements during weathering of a granodiorite[J]. Nature,279:206-210.
[12]	亨德森. 稀土元素地球化学[M]. 北京:地质出版社,1989:201-203.[Henderson P. Geochemistry of Rare Earth Element[M]. Beijing:Geologic Publishing House,1989:201 -203.]
[13]	杨守业,李从先. REE示踪沉积物物源研究进展[J].地球科学进展,1999,14(2):166.[YANG Shou-ye,LI Cong-xian. Research progress in REE tracer for sediment source[J]. Advance in Earth Sciences,1999 ,14(2):166.]
[14]	陈丽蓉. 渤海、黄海、东海沉积物中矿物组合的研究[J]. 海洋科学,1989(2):1-8.[CHEN Li-rong. A study on mineral assemblages in sediments of the Bohai Sea, the Huanghai Sea and the East China Sea[J]. Marine Science,1989 (2):1-8.]
[15]	杨守业,李从先. 黄河沉积物中REE制约与示踪意义再认识[J]. 自然科学进展,2003,13(4):369.[YANG Shou-ye,LI Cong-xian. Recognition of restrict and trace significance of REE in the Huanghe River sediments[J]. Progress in Natural Science,2003 ,13(4):369.]
[16]	秦蕴珊,李凡.黄河入海泥沙对渤海和黄海沉积作用的影响[J].海洋科学集刊,1986,27:125-135.[QIN Yun-shan,LI Fan. Study on the influence of sediment loads discharged from Yellow River on sedimentation in the Bohai Sea and Huanghai Sea[J]. Studia Marine Sinica,1986 ,27:125-135.]
[17]	王爱萍,杨守业,李从先. 南京地区下蜀土元素地球化学特征[J].同济大学学报, 2001,29(6):660.[WANG Ai-ping,YANG Shou-ye,LI Cong-xian. Elemental geochemistry of the Nanjing Xiashu loess and the provenance study[J].Journal of Tongji University,2001 ,29(6):660.]
[18]	Yang S Y,Lim D I,Jung H S,et al. Geochemical composition and provenance discrimination of coastal sediments around Cheju in the southeastern Yellow Sea[J]. Marine Geology,2004(206):45.

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GEOCHEMISTRY OF REE AND PROVENANCE OF SURFACE SEDIMENTS IN THE LITTORAL AREA OF THE NORTHEASTERN SHANDONG PENINSULA