IOCAS-IR  > 海洋地质与环境重点实验室
Investigation of an oceanic plateau formation and rifting initiation model implied by the Caroline Ridge on the Caroline Plate, western Pacific
Zhang, Zhengyi1,2,3,4,5; Dong, Dongdong1,2,4; Sun, Weidong2,4,5; Zhang, Guangxu1; Bai, Yongliang6
2020-01-04
发表期刊INTERNATIONAL GEOLOGY REVIEW
ISSN0020-6814
页码15
通讯作者Dong, Dongdong(dongdongdong@qdio.ac.cn) ; Sun, Weidong(weidongsun@qdio.ac.cn)
摘要The rifting of oceanic plateaus is an important mechanism for initiating lithospheric break-up and subsequent seafloor spreading. In this study, we present the latest multichannel seismic data investigating the Caroline Ridge and provide one of the typical cases for initial oceanic plateau evolution. We reveal that a smooth basement reflector (R2), as the top of the lava flows, is subparallel to the sediments with horizontal seismic reflections over the surface of the Caroline Ridge. Thick layer-parallel lava flows beneath the R2 appear within the crust. Large seamounts in the Sorol Trough possess abundant saucer-shaped intracrustal reflectors, and the overlying sediments were destroyed by intrusive bodies. The overlying sedimentary sequences, basement, and thick lava flows on the Caroline Ridge flanks were faulted by opposing normal fault sets, and the eruptions of the seamounts deformed the strata. A widespread bright horizontal reflector (R1), as an unconformity inside the Caroline Ridge sediments, truncates the lower tilted sediment layers and is itself cut by normal faults in the flank strata. Furthermore, we propose that subaerial lava flows extended laterally from the hotspot magmatism localizing in the Sorol Trough and led to Caroline Ridge formation. The initial rifting of the Caroline Ridge occurred during the Early-Middle Miocene. Limited volcanoes concentrate only in the Sorol Trough due to the attenuated thermal effect. It is suggested that dome uplifting and far-field force could have jointly caused initial rifting process of the Caroline Ridge.
关键词Caroline Ridge Sorol Trough Oceanic plateau rifting Hotspot Seismic profile Sedimentary sequence Crustal structure
DOI10.1080/00206814.2019.1707126
收录类别SCI
语种英语
资助项目National Natural Science Foundat-ionof China[41976051] ; National Natural Science Foundat-ionof China[91958211] ; National Programon Global Change and Air-Sea Interaction[GASI-GEOGE01] ; Key Research Program of Center for Ocean Mega Scienceof CAS[KEXUE2018G10] ; National Natural Science Foundat-ionof China[41976051] ; National Natural Science Foundat-ionof China[91958211] ; National Programon Global Change and Air-Sea Interaction[GASI-GEOGE01] ; Key Research Program of Center for Ocean Mega Scienceof CAS[KEXUE2018G10]
WOS研究方向Geology
WOS类目Geology
WOS记录号WOS:000505456700001
出版者TAYLOR & FRANCIS INC
引用统计
被引频次:9[WOS]   [WOS记录]     [WOS相关记录]
文献类型期刊论文
条目标识符http://ir.qdio.ac.cn/handle/337002/164161
专题海洋地质与环境重点实验室
通讯作者Dong, Dongdong; Sun, Weidong
作者单位1.Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Geol & Environm, Qingdao, Shandong, Peoples R China
2.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao, Shandong, Peoples R China
3.Univ Chinese Acad Sci, Beijing, Peoples R China
4.Chinese Acad Sci, Ctr Ocean Megasci, Qingdao, Shandong, Peoples R China
5.Chinese Acad Sci, Ctr Deep Sea Res, Inst Oceanol, Qingdao, Shandong, Peoples R China
6.China Univ Petr, Sch Geosci, Qingdao, Shandong, Peoples R China
第一作者单位中国科学院海洋研究所;  中国科学院海洋大科学研究中心
通讯作者单位中国科学院海洋研究所;  中国科学院海洋大科学研究中心
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Zhang, Zhengyi,Dong, Dongdong,Sun, Weidong,et al. Investigation of an oceanic plateau formation and rifting initiation model implied by the Caroline Ridge on the Caroline Plate, western Pacific[J]. INTERNATIONAL GEOLOGY REVIEW,2020:15.
APA Zhang, Zhengyi,Dong, Dongdong,Sun, Weidong,Zhang, Guangxu,&Bai, Yongliang.(2020).Investigation of an oceanic plateau formation and rifting initiation model implied by the Caroline Ridge on the Caroline Plate, western Pacific.INTERNATIONAL GEOLOGY REVIEW,15.
MLA Zhang, Zhengyi,et al."Investigation of an oceanic plateau formation and rifting initiation model implied by the Caroline Ridge on the Caroline Plate, western Pacific".INTERNATIONAL GEOLOGY REVIEW (2020):15.
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