A dynamic rifting model of the Caroline Ridge, West Pacific

doi:10.1016/j.jseaes.2024.106218

IOCAS-IR > 海洋地质与环境重点实验室

	A dynamic rifting model of the Caroline Ridge, West Pacific
	Zhang, Zhengyi 1,2,4; Dong, Dongdong3,5 ; Li, Sanzhong 1,2,4; Perez-Gussinye, Marta 6; Wang, Xiujuan 1,2,4; Fan, Jianke 3,5; Li, Cuilin 3,5
	2024-07-15
发表期刊	JOURNAL OF ASIAN EARTH SCIENCES
ISSN	1367-9120
卷号	271 页码:16
通讯作者	Zhang, Zhengyi([email protected]) ; Dong, Dongdong([email protected])
摘要	The dynamic rifting model of the Caroline Ridge, an oceanic plateau in the West Pacific, remains unclear. Previous studies have revealed that the crustal width of the Caroline Ridge clearly varies from the northwest to the southeast. Here, we investigate Caroline Ridge rifting using numerical simulation and reveal the relationships between different plateau sizes and rifting. For small-scale oceanic plateaus, the initial rift migration forms a symmetric structure. The strain transfers toward one side of the margin. The rifting manifests as a process from landward migration to seaward migration, accompanied by a transition from a symmetric to an asymmetric structure. With larger initial lithospheric thinning, larger ranges of crustal deformation appear with less basement tectonic subsidence. For large-scale oceanic plateaus, basement tectonic subsidence occurs within narrower ranges. The proximal half-graben structures rapidly abandon with relatively horizontal basement and small fault offsets on the rift flank, leading to a symmetric structure during breakup. With larger initial lithospheric thinning, crustal deformation occurs within a narrower region during the early stage. Landward rift migration dominates the deformation, resulting in an asymmetric structure. On the basis of these results, for the large-scale section of the Caroline Ridge, NW-trending normal faults originated from the landward rift migration. At present, seaward rift migration dominates the Caroline Ridge deformation, forming a relatively symmetric structure. For the small-scale section of the Caroline Ridge, the initial landward rift migration occurred. Larger initial lithospheric thinning may exist beneath the Caroline Ridge during the initiation of Miocene rifting.
关键词	Oceanic plateau Rifting model Caroline Ridge West Pacific
DOI	10.1016/j.jseaes.2024.106218
收录类别	SCI
语种	英语
资助项目	National Natural Science Foundation of China[42376081]; National Natural Science Foundation of China[42106064]; National Natural Science Foundation of China[41976051]; Strategic Priority Research Program of the Chinese Academy of Sciences[XDB42000000]; Science and Technology Innovation Project of Laoshan Laboratory[LSKJ202204400]; Taishan Scholars Program[tsqn202306283]; State Key Laboratory of Marine Geology, Tongji University[MGK202106]
WOS研究方向	Geology
WOS类目	Geosciences, Multidisciplinary
WOS记录号	WOS:001257686500001
出版者	PERGAMON-ELSEVIER SCIENCE LTD
WOS关键词	LARGE IGNEOUS PROVINCES ; OCEANIC PLATEAU FORMATION ; YAP TRENCH ; KERGUELEN PLATEAU ; INDIAN-OCEAN ; TECTONIC EVOLUTION ; CRUSTAL STRUCTURE ; MANTLE PLUME ; LITHOSPHERE ; SUBDUCTION
引用统计
文献类型	期刊论文
条目标识符	http://ir.qdio.ac.cn/handle/337002/186375
专题	海洋地质与环境重点实验室
通讯作者	Zhang, Zhengyi; Dong, Dongdong
作者单位	1.Ocean Univ China, MOE, Frontiers Sci Ctr Deep Ocean Multispheres & Earth, Key Lab Submarine Geosci & Prospecting Tech, Qingdao 266100, Peoples R China 2.Ocean Univ China, Coll Marine Geosci, Qingdao 266100, Peoples R China 3.Chinese Acad Sci, Inst Oceanol, CAS Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China 4.Qingdao Marine Sci & Technol Ctr, Lab Marine Mineral Resources, Qingdao 266237, Peoples R China 5.Qingdao Marine Sci & Technol Ctr, Lab Marine Geol, Qingdao 266237, Peoples R China 6.Univ Bremen, Marum Ctr Marine Environm Sci, Bremen, Germany
通讯作者单位	中国科学院海洋研究所
推荐引用方式 GB/T 7714	Zhang, Zhengyi,Dong, Dongdong,Li, Sanzhong,et al. A dynamic rifting model of the Caroline Ridge, West Pacific[J]. JOURNAL OF ASIAN EARTH SCIENCES,2024,271:16.
APA	Zhang, Zhengyi.,Dong, Dongdong.,Li, Sanzhong.,Perez-Gussinye, Marta.,Wang, Xiujuan.,...&Li, Cuilin.(2024).A dynamic rifting model of the Caroline Ridge, West Pacific.JOURNAL OF ASIAN EARTH SCIENCES,271,16.
MLA	Zhang, Zhengyi,et al."A dynamic rifting model of the Caroline Ridge, West Pacific".JOURNAL OF ASIAN EARTH SCIENCES 271(2024):16.