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Magnetic minerals in three Asian rivers draining into the South China Sea: Pearl, Red, and Mekong Rivers

文献类型：期刊论文

作者Kissel, Catherine1; Liu, Zhifei2; Li, Jinhua3; Wandres, Camille1
刊名GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
出版日期2016-05-01
卷号17期号:5页码:1678-1693
关键词river sediments magnetic mineralogy Southeast Asia
DOI10.1002/2016GC006283
文献子类Article
英文摘要The use of the marine sedimentary magnetic properties, as tracers for changes in precipitation rate and in oceanic water masses transport and exchanges, implies to identify and to characterize the different sources of the detrital fraction. This is of particular importance in closed and/or marginal seas such as the South China Sea. We report on the magnetic properties of sedimentary samples collected in three main Asian rivers draining into the South China Sea: the Pearl, Red, and Mekong Rivers. The geological formations as well as the present climatic conditions are different from one catchment to another. The entire set of performed magnetic analyses (low-field magnetic susceptibility, ARM acquisition and decay, IRM acquisition and decay, back-field acquisition, thermal demagnetization of three-axes IRM, hysteresis parameters, FORC diagrams, and low-temperature magnetic measurements) allow us to identify the magnetic mineralogy and the grain-size distribution when magnetite is dominant. Some degree of variability is observed in each basin, illustrating different parent rocks and degree of weathering. On average it appears that the Pearl River is rich in magnetite along the main stream while the Mekong River is rich in hematite. The Red River is a mixture of the two. Compared to clay mineral assemblages and major element contents previously determined on the same samples, these new findings indicate that the magnetic fraction brings complementary information of great interest for environmental reconstructions based on marine sediments from the South China Sea.
WOS关键词ISOTHERMAL REMANENT MAGNETIZATION ; ACQUISITION CURVES ; SUSPENDED SEDIMENT ; FLUVIAL SEDIMENTS ; NORTH-ATLANTIC ; HOLOCENE ; DELTA ; TRANSPORT ; DISCHARGE ; VIETNAM
WOS研究方向Geochemistry & Geophysics
语种英语
WOS记录号WOS:000379525100007
资助机构French INSU/LEFE-MONOCL project ; French INSU/LEFE-MONOCL project ; National Natural Science Foundation of China (NSFC)(41522402 ; National Natural Science Foundation of China (NSFC)(41522402 ; Open Project Support from the State Key Laboratory of Lithospheric Evolution (IGGCAS, Beijing) ; Open Project Support from the State Key Laboratory of Lithospheric Evolution (IGGCAS, Beijing) ; 41374004 ; 41374004 ; 91128206 ; 91128206 ; 91528304) ; 91528304) ; French INSU/LEFE-MONOCL project ; French INSU/LEFE-MONOCL project ; National Natural Science Foundation of China (NSFC)(41522402 ; National Natural Science Foundation of China (NSFC)(41522402 ; Open Project Support from the State Key Laboratory of Lithospheric Evolution (IGGCAS, Beijing) ; Open Project Support from the State Key Laboratory of Lithospheric Evolution (IGGCAS, Beijing) ; 41374004 ; 41374004 ; 91128206 ; 91128206 ; 91528304) ; 91528304)
源URL[http://ir.iggcas.ac.cn/handle/132A11/53388]  
专题地质与地球物理研究所_中国科学院地球与行星物理重点实验室
作者单位1.Univ Paris Saclay, Lab Sci Climat & Environm IPSL, CEA CNRS UVSQ, Gif Sur Yvette, France
2.Tongji Univ, State Key Lab Marine Geol, Shanghai, Peoples R China
3.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Earth & Planetary Phys, Beijing, Peoples R China
推荐引用方式
GB/T 7714		 Kissel, Catherine,Liu, Zhifei,Li, Jinhua,et al. Magnetic minerals in three Asian rivers draining into the South China Sea: Pearl, Red, and Mekong Rivers[J]. GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,2016,17(5):1678-1693.
APA Kissel, Catherine,Liu, Zhifei,Li, Jinhua,&Wandres, Camille.(2016).Magnetic minerals in three Asian rivers draining into the South China Sea: Pearl, Red, and Mekong Rivers.GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS,17(5),1678-1693.
MLA Kissel, Catherine,et al."Magnetic minerals in three Asian rivers draining into the South China Sea: Pearl, Red, and Mekong Rivers".GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS 17.5(2016):1678-1693.

入库方式： OAI收割

来源：地质与地球物理研究所

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