The Mesozoic-Cenozoic igneous intrusions and related sediment-dominated hydrothermal activities in the South Yellow Sea Basin, the Western Pacific continental margin

doi:10.1016/j.jmarsys.2016.11.011

CORC > 海洋研究所 > 中国科学院海洋研究所

	The Mesozoic-Cenozoic igneous intrusions and related sediment-dominated hydrothermal activities in the South Yellow Sea Basin, the Western Pacific continental margin
	Pang Yumao1,2,3 ; Zhang Xunhua 2,3; Xiao Guolin 2,3; Shang Luning 4; Guo Xingwei 3; Wen Zhenhe 3
刊名	JOURNAL OF MARINE SYSTEMS
	2018-04-01
卷号	180 页码:152-161
关键词	Igneous intrusions Hydrothermal vent complexes South Yellow Sea Basin Western Pacific continental margin
ISSN号	0924-7963
DOI	10.1016/j.jmarsys.2016.11.011
通讯作者	Pang Yumao(pangyumao@126.com) ; Zhang Xunhua(xunhuazh@vip.sina.com)
英文摘要	Various igneous complexes were identified in multi-channel seismic reflection profiles from the South Yellow Sea Basin. It is not rare that magmatic intrusions in sedimentary basins cause strong thermal perturbations and hydrothermal activities. Some intrusion-related hydrothermal vent complexes have been identified and they are considered to originate from the deep sedimentary contact aureole around igneous intrusions and terminate in upper vents structures, and are linked by a vertical conduit system. The upper vent complexes are usually eye shaped, dome-shaped, fault-related, crater-shaped or pock-shaped in seismic profiles. A schematic model was proposed to illustrate the structures of different types of hydrothermal vent complexes. A conceptual conduit model composed of an upper pipe-like part and a lower branching part was also derived. Hydrothermal vent complexes mainly developed during the Middle-Late Cretaceous, which is coeval with, or shortly after the intrusion. The back-arc basin evolution of the area which is related to the subduction of the Paleo-Pacific plate during the Mesozoic-Cenozoic may be the principal factor for voluminous igneous complexes and vent complexes in this area. It is significant to study the characteristics of igneous complexes and related hydrothermal vent complexes, which will have implications for the future study of this area. (C) 2016 Elsevier B.V. All rights reserved.
资助项目	National Key Basic Research Program of China (973 program)[2013CB429701] ; Special Survey for Marine Geology from China Ministry of Land and Resources (MLR)[GZH201100202] ; AoShan science and technology innovation plan from Qingdao National Laboratory for Marine Science and Technology, China[2015ASKJ03] ; National Science Foundation for Young Scientists of China[41606050] ; Qingdao Institute of Marine Geology (QIMG), China
WOS研究方向	Geology ; Marine & Freshwater Biology ; Oceanography
语种	英语
出版者	ELSEVIER SCIENCE BV
WOS记录号	WOS:000429514700014
内容类型	期刊论文
源URL	[http://ir.qdio.ac.cn/handle/337002/158661]
专题	中国科学院海洋研究所
通讯作者	Pang Yumao; Zhang Xunhua
作者单位	1.Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China 2.Qingdao Natl Lab Marine Sci & Technol, Qingdao 266071, Peoples R China 3.Qingdao Inst Marine Geol, Qingdao 266071, Peoples R China 4.Ocean Univ China, Qingdao 266071, Peoples R China
推荐引用方式 GB/T 7714	Pang Yumao,Zhang Xunhua,Xiao Guolin,et al. The Mesozoic-Cenozoic igneous intrusions and related sediment-dominated hydrothermal activities in the South Yellow Sea Basin, the Western Pacific continental margin[J]. JOURNAL OF MARINE SYSTEMS,2018,180:152-161.
APA	Pang Yumao,Zhang Xunhua,Xiao Guolin,Shang Luning,Guo Xingwei,&Wen Zhenhe.(2018).The Mesozoic-Cenozoic igneous intrusions and related sediment-dominated hydrothermal activities in the South Yellow Sea Basin, the Western Pacific continental margin.JOURNAL OF MARINE SYSTEMS,180,152-161.
MLA	Pang Yumao,et al."The Mesozoic-Cenozoic igneous intrusions and related sediment-dominated hydrothermal activities in the South Yellow Sea Basin, the Western Pacific continental margin".JOURNAL OF MARINE SYSTEMS 180(2018):152-161.