Identification of the Caroline Plate boundary: constraints from magnetic anomaly
文献类型:期刊论文
作者 | Fu, Yongtao1,2,3; Zhang, Guoliang1,3,6; Wang, Wanyin2,3,4; Yang, An1,3; He, Tao2,4; Zhou, Zhangguo1,3![]() |
刊名 | ACTA OCEANOLOGICA SINICA
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出版日期 | 2024-08-01 |
卷号 | 43期号:8页码:1-12 |
关键词 | Caroline Plate magnetic anomaly normalized vertical derivative of the total horizontal derivative plate boundary Caroline Ridge Eauripik Rise |
ISSN号 | 0253-505X |
DOI | 10.1007/s13131-023-2272-9 |
通讯作者 | Fu, Yongtao(ytfu@qdio.ac.cn) ; Wang, Wanyin(wwy7902@iocas.ac.cn) |
英文摘要 | The Caroline Plate is located among the Pacific Plate, the Philippine Sea Plate, and the India Australia Plate, and plays a key role in controlling the spreading direction of the Philippine Sea Plate. The Caroline Submarine Plateau (or Caroline Ridge) and the Eauripik Rise on the south formed a remarkable T-shaped large igneous rock province, which covered the northern boundary between the Caroline Plate and the Pacific Plate. However, relationship between these tectonic units and magma evolution remains unclear. Based on magnetic data from the Earth Magnetic Anomaly Grid (2-arc-minute resolution) (V2), the normalized vertical derivative of the total horizontal derivative (NVDR-THDR) technique was used to study the boundary of the Caroline Plate. Results show that the northern boundary is a transform fault that runs 1 400 km long in approximately 28 km wide along the N8 degrees in E-W direction. The eastern boundary is an NNW-SSE trending fault zone and subduction zone with a width of tens to hundreds of kilometers; and the north of N4 degrees is a fracture zone of dense faults. The southeastern boundary may be the Lyra Trough. The area between the southwestern part of the Caroline Plate and the Ayu Trough is occupied by a wide shear zone up to 100 km wide in nearly S-N trending in general. The Eauripik transform fault (ETF) in the center of the Caroline Plate and the fault zones in the east and west basins are mostly semi-parallel sinistral NNW-SSE-trending faults, which together with the eastern boundary Mussau Trench (MT) sinistral fault, the northern Caroline transform fault (CTF), and the southern shear zone of the western boundary, indicates the sinistral characteristics of the Caroline Plate. The Caroline hotspot erupted in the Pacific Plate near the CTF and formed the west Caroline Ridge, and then joined with the Caroline transform fault at the N8 degrees. A large amount of magma erupted along the CTF, by which the east Caroline Ridge was formed. At the same time, a large amount of magma developed southward via the eastern branch of the ETF, forming the northern segment of the Eauripik Rise. Therefore, the magmatic activity of the T-shaped large igneous province is obviously related to the fault structure of the boundary faults between the Caroline Plate and Pacific Plate, and the active faults within the Caroline Plate. |
WOS关键词 | YAP TRENCH ; OCEANIC LITHOSPHERE ; TECTONIC EVOLUTION ; WESTERN PACIFIC ; FLOOD BASALTS ; MANTLE PLUME ; AYU TROUGH ; GRAVITY ; SEA ; SUBDUCTION |
资助项目 | Key Laboratory of Marine Geology and Environment, Chinese Academy of Sciences[MGE2022KG11] |
WOS研究方向 | Oceanography |
语种 | 英语 |
WOS记录号 | WOS:001339542500006 |
出版者 | SPRINGER |
源URL | [http://ir.qdio.ac.cn/handle/337002/199507] ![]() |
专题 | 海洋研究所_海洋地质与环境重点实验室 |
通讯作者 | Fu, Yongtao; Wang, Wanyin |
作者单位 | 1.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266237, Peoples R China 2.Natl Engn Res Ctr Offshore Oil & Gas Explorat, Beijing 100028, Peoples R China 3.Chinese Acad Sci, Inst Oceanol, Key Lab Ocean Observat & Forecasting, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China 4.Changan Univ, Inst Grav & Magnet Technol, Key Lab Western Chinas Mineral Resources & Geol En, Sch Geol Engn & Geomat,Minist Educ, Xian 710054, Peoples R China 5.Univ Chinese Acad Sci, Beijing 100049, Peoples R China 6.Chinese Acad Sci, Inst Oceanol, Ctr Deep Sea Res, Qingdao 266071, Peoples R China |
推荐引用方式 GB/T 7714 | Fu, Yongtao,Zhang, Guoliang,Wang, Wanyin,et al. Identification of the Caroline Plate boundary: constraints from magnetic anomaly[J]. ACTA OCEANOLOGICA SINICA,2024,43(8):1-12. |
APA | Fu, Yongtao.,Zhang, Guoliang.,Wang, Wanyin.,Yang, An.,He, Tao.,...&Han, Xiao.(2024).Identification of the Caroline Plate boundary: constraints from magnetic anomaly.ACTA OCEANOLOGICA SINICA,43(8),1-12. |
MLA | Fu, Yongtao,et al."Identification of the Caroline Plate boundary: constraints from magnetic anomaly".ACTA OCEANOLOGICA SINICA 43.8(2024):1-12. |
入库方式: OAI收割
来源:海洋研究所
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