Geochemistry of Oligocene Huagang Formation clastic rocks, Xihu Sag, the East China Sea Shelf Basin: Provenance, source weathering, and tectonic setting
文献类型:期刊论文
作者 | Hao, Lewei1; Wang, Qi1; Tao, Huifei1; Li, Xiaoyan2; Ma, Dongxu1,3; Ji, Hongjie1,3 |
刊名 | GEOLOGICAL JOURNAL
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出版日期 | 2018 |
卷号 | 53期号:1页码:397-411 |
关键词 | Huagang Formation Provenance Analysis Sedimentary Geochemistry Tectonic Setting Xihu Sag |
ISSN号 | 0072-1050 |
DOI | 10.1002/gj.2906 |
文献子类 | Article |
英文摘要 | The East China Sea Shelf Basin (ECSSB) is an important tectonic unit of the western Pacific active continental margin. It is divided further into a series of sags and basement ridges. The Xihu Sag on the east margin of the ECSSB is an important hydrocarbon exploration area and contains significant petroleum resources. The Huagang Formation is the major reservoir in Xihu Sag, and its provenance has been the focus of debate at all times. The major and trace elements (including rare earth elements) compositions were analyzed for the Oligocene Huagang Formation sandstone and mudstone samples in the Xihu Sag. The provenance and tectonic setting of these clastic rocks are discussed. The Chemical Index of Alteration value and A-CN-K diagrams suggest low to moderate weathering in the source areas of the Huagang Formation. The mudstones have lower index of compositional variation values (<1), indicating that the mudstone samples are compositionally mature, whereas the index of compositional variation values for the sandstone samples (0.59 to 1.87) indicate that the sandstones are compositionally immature and mature. The major and trace element composition and ratios of the clastic rock samples indicate that mudstones are mainly from Late Mesozoic igneous rocks in SE China, which is dominated by the acidic volcanic rock. The provenance of sandstones is from two different directions, the Central Uplift Group of ECSSB and the Taiwan-Sinzi Fold Belt with more mafic volcanic rock. Based on the geochemical analysis of the clastic rock samples, the tectonic setting of Xihu Sag was Japanese-type continental margin during the Huagang Formation deposition time (Oligocene). |
WOS关键词 | RARE-EARTH-ELEMENT ; SEDIMENTARY-ROCKS ; CRUSTAL EVOLUTION ; MAJOR-ELEMENT ; VOLCANIC-ROCKS ; WET MOUNTAINS ; SOUTH CHINA ; SANDSTONES ; SHALES ; PETROGENESIS |
WOS研究方向 | Geology |
语种 | 英语 |
WOS记录号 | WOS:000419785900022 |
出版者 | WILEY |
资助机构 | National Natural Science Foundation of China(41502110 ; National Natural Science Foundation of China(41502110 ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; 41502142) ; 41502142) ; National Natural Science Foundation of China(41502110 ; National Natural Science Foundation of China(41502110 ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; 41502142) ; 41502142) ; National Natural Science Foundation of China(41502110 ; National Natural Science Foundation of China(41502110 ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; 41502142) ; 41502142) ; National Natural Science Foundation of China(41502110 ; National Natural Science Foundation of China(41502110 ; Youth Innovation Promotion Association CAS ; Youth Innovation Promotion Association CAS ; 41502142) ; 41502142) |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/82576] ![]() |
专题 | 中国科学院地质与地球物理研究所 |
通讯作者 | Hao, Lewei |
作者单位 | 1.Chinese Acad Sci, Key Lab Petr Resources, Gansu Prov Key Lab Petr Resources Res, Inst Geol & Geophys, Lanzhou, Gansu, Peoples R China 2.Chinese Acad Sci, Lanzhou Lib, Lanzhou, Gansu, Peoples R China 3.Univ Chinese Acad Sci, Beijing, Peoples R China |
推荐引用方式 GB/T 7714 | Hao, Lewei,Wang, Qi,Tao, Huifei,et al. Geochemistry of Oligocene Huagang Formation clastic rocks, Xihu Sag, the East China Sea Shelf Basin: Provenance, source weathering, and tectonic setting[J]. GEOLOGICAL JOURNAL,2018,53(1):397-411. |
APA | Hao, Lewei,Wang, Qi,Tao, Huifei,Li, Xiaoyan,Ma, Dongxu,&Ji, Hongjie.(2018).Geochemistry of Oligocene Huagang Formation clastic rocks, Xihu Sag, the East China Sea Shelf Basin: Provenance, source weathering, and tectonic setting.GEOLOGICAL JOURNAL,53(1),397-411. |
MLA | Hao, Lewei,et al."Geochemistry of Oligocene Huagang Formation clastic rocks, Xihu Sag, the East China Sea Shelf Basin: Provenance, source weathering, and tectonic setting".GEOLOGICAL JOURNAL 53.1(2018):397-411. |
入库方式: OAI收割
来源:地质与地球物理研究所
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