Post-rifting magmatism and the drowned reefs in the Xisha Archipelago domain
Wang, Hongli1,2; Zhao, Qiang3,4; Wu, Shiguo2,4,5; Wang, Dawei5; Wang, Bin6; Wu, Shiguo(Univ Chinese Acad Sci, Coll Earth Sci, Beijing 100049, Peoples R China)
2018-02-01
发表期刊JOURNAL OF OCEAN UNIVERSITY OF CHINA
卷号17期号:1页码:195-208
产权排序第1完成单位 ; 第2完成单位 ; 第3完成单位 ; 第4完成单位 ; 第5完成单位 ; 第6完成单位
摘要Fourteen isolated drowned reefs have been identified around the Xisha Uplift by multibeam and seismic data. The drowning processes of these reefs can be divided into three different stages, which correspond to three different accelerated tectonic subsidence periods. The drowning of the Xisha reefs is the result of the combined action of tectonic subsidence and sea level fluctuations, and the tectonic subsidence rate had to remain above 0.2 mm yr(-1) for a long time. Three abrupt accelerated tectonic subsidence events that occurred in the late Miocene, Pliocene and early Quaternary in the Xisha Uplift were closely related to the thermal subsidence processes after three stages of post-rifting magmatism. The magmatism of the middle Miocene and the following thermal subsidence resulted in the drowning of reefs in the northwestern Xisha uplift (Zone A). During the early Pliocene, massive magmatic intrusions and volcanic eruptions occurred in the Xisha Uplift. Then, the subsequent thermal subsidence started the drowning process of reefs in the northeastern and western regions of the Xisha Uplift (Zone B and C). During the early Quaternary, large-scale magmatism also occurred in the Xisha Uplift. The subsequent thermal subsidence resulted in a new rapid tectonic subsidence, which caused the reefs in the southern and southeastern regions of the Xisha Uplift to drown (Zone D and E).
文章类型Article
关键词Magmatism Tectonic Subsidence Drowned Reef Xisha Archipelago
WOS标题词Science & Technology ; Physical Sciences
DOI10.1007/s11802-018-3485-y
URL查看原文
收录类别SCI
语种英语
关键词[WOS]SOUTH CHINA SEA ; NORTHERN CONTINENTAL-MARGIN ; CARBONATE PLATFORMS ; TECTONIC SUBSIDENCE ; QIONGDONGNAN BASIN ; LATE MIOCENE ; LEVEL RISE ; HAWAII ; SEDIMENTATION ; ARCHITECTURE
WOS类目Oceanography
WOS记录号WOS:000419533800020
引用统计
被引频次:1[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.idsse.ac.cn/handle/183446/5264
专题深海科学研究部_深海地球物理与资源研究室
通讯作者Wu, Shiguo; Wu, Shiguo(Univ Chinese Acad Sci, Coll Earth Sci, Beijing 100049, Peoples R China)
作者单位1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
2.Univ Chinese Acad Sci, Coll Earth Sci, Beijing 100049, Peoples R China
3.SOA, Inst Oceanog 1, Key Lab Marine Sedimentol & Environm Geol, Qingdao 266061, Peoples R China
4.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Peoples R China
5.Chinese Acad Sci, Inst Deep Sea Sci & Engn, Lab Marine Geophys & Deep Sea Georesources, Sanya 572000, Peoples R China
6.PetroChina, Hangzhou Inst Petr Geol, Hangzhou 310023, Zhejiang, Peoples R China
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GB/T 7714
Wang, Hongli,Zhao, Qiang,Wu, Shiguo,et al. Post-rifting magmatism and the drowned reefs in the Xisha Archipelago domain[J]. JOURNAL OF OCEAN UNIVERSITY OF CHINA,2018,17(1):195-208.
APA Wang, Hongli,Zhao, Qiang,Wu, Shiguo,Wang, Dawei,Wang, Bin,&Wu, Shiguo.(2018).Post-rifting magmatism and the drowned reefs in the Xisha Archipelago domain.JOURNAL OF OCEAN UNIVERSITY OF CHINA,17(1),195-208.
MLA Wang, Hongli,et al."Post-rifting magmatism and the drowned reefs in the Xisha Archipelago domain".JOURNAL OF OCEAN UNIVERSITY OF CHINA 17.1(2018):195-208.
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