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高校地质学报 ›› 2020, Vol. 26 ›› Issue (6): 680-690.DOI: 10.16108/j.issn1006-7493.2019084

• 其他学科 • 上一篇    下一篇

冲绳海槽构造演化及其与岩浆、热液和沉积作用的关系:研究进展与展望

刘 伟, 孙钰杰, 郑涵月, 辛孟燃, 何 炜,魏 桐, 郭诗岳,陈思放, 刘雯文, 冯雨歌   

  1. 南方科技大学 海洋科学与工程系,深圳 518055
  • 出版日期:2020-12-20 发布日期:2021-01-05

Research Progress and Prospect of the Tectonic Evolution of Okinawa Trough and Its Relationship with Magmatism, Hydrothermal Activities and Sedimentation

LIU Wei,SUN Yujie,ZHENG Hanyue,XIN Mengran,HE Wei,WEI Tong,GUO Shiyue,CHEN Sifang ,LIU Wenwen,FENG Yuge   

  1. Department of Ocean Science and Engineering, Southern University of Science and Technology, Shenzhen 518055, China
  • Online:2020-12-20 Published:2021-01-05

摘要: 冲绳海槽是西太平洋沟-弧-盆体系中典型的弧后盆地。其独特的大地构造位置,岩浆、热液活动与沉积记录一直是学术界研究的热点。基于前人的研究成果,本文综述了冲绳海槽的构造活动对岩浆、热液与沉积的控制作用。菲律宾海板块的俯冲导致了冲绳海槽的形成,并发生了弧岩浆、弧后岩浆和斜切弧后岩浆作用,这三种岩浆作用导致了热液活动在平面分布上的三种不同分区。岩浆的发育和菲律宾海板块俯冲造成的断裂系统为冲绳海槽热液的发育分别提供了热源和通道。在~416 ka发生的浙闽隆起带沉降,导致了冲绳海槽北部的沉积物由粗变细。最后针对冲绳海槽的研究现状,文章对未来的进一步研究作了展望。

关键词: 冲绳海槽, 构造, 岩浆, 热液, 沉积

Abstract: The Okinawa Trough is a typical back-arc basin in the western Pacific Trench Arc Back-Arc system. Its unique tectonic location, magmatism, hydrothermal activities and sedimentary records have been a focus of academic research. Based on previous research, we review the controls of magmatic, hydrothermal and sedimentary activities by tectonic evolution of the Okinawa Trough. The subduction of the Philippine Sea plate led to the formation of the Okinawa Trough and the occurrence of arc volcanism, back-arc volcanism and cross-back arc volcanism. These three types of volcanism resulted in three different zones of hydrothermal activity. The magmatism and fault system caused by subduction of Philippine Sea plate provide heat sources and channels for the development of hydrothermal fluid in the Okinawa Trough. The subsidence of Zhe -Min Uplift at ~416 ka brought about the sediments in the northern Okinawa Trough to change from coarse-to fine-grained. Finally, we also provide the outlook of further research based on the current research status of the Okinawa Trough.

Key words: Okinawa Trough, tectonic evolution, magmatism, hydrothermal, sedimentation

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