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冲绳海槽断裂、岩浆构造活动和洋壳化进程

高金耀 张涛 方银霞 杨春国 汪俊 谭勇华 梅赛

高金耀, 张涛, 方银霞, 杨春国, 汪俊, 谭勇华, 梅赛. 冲绳海槽断裂、岩浆构造活动和洋壳化进程[J]. 海洋学报, 2008, 30(5): 62-70.
引用本文: 高金耀, 张涛, 方银霞, 杨春国, 汪俊, 谭勇华, 梅赛. 冲绳海槽断裂、岩浆构造活动和洋壳化进程[J]. 海洋学报, 2008, 30(5): 62-70.
GAO Jin-yao, ZHANG Tao, FANG Yin-xia, YANG Chuan-guo, WANG Jun, TAN Yong-hua, MEI Sai. Faulting, magmatism and crustal oceanization of the Okinawa Trough[J]. Haiyang Xuebao, 2008, 30(5): 62-70.
Citation: GAO Jin-yao, ZHANG Tao, FANG Yin-xia, YANG Chuan-guo, WANG Jun, TAN Yong-hua, MEI Sai. Faulting, magmatism and crustal oceanization of the Okinawa Trough[J]. Haiyang Xuebao, 2008, 30(5): 62-70.

冲绳海槽断裂、岩浆构造活动和洋壳化进程

基金项目: 国家重点基础研究发展计划项目资助(G2000046703;2007CB411702);我国近海海洋综合调查与评价专项(908-ZC-I-06)

Faulting, magmatism and crustal oceanization of the Okinawa Trough

  • 摘要: 讨论了冲绳海槽断裂、岩浆构造活动特征和它们之间的关系,认为雁行排列的地堑斜交于陆架外缘隆起带,海槽北段断块隆脊、龙王构造带和海槽南段"棉花构造带"可能保留了海槽各幕断陷前的火山岩浆活动特征,而现在活动的吐噶喇火山岛弧可沿海槽南段岛坡追踪到台湾。吕宋岛向台湾的碰撞挤压引起的旋张活动加强了海槽南段的地壳拉张,诱发了地堑内火山岩浆活动,在洋壳化进程中起关键作用,其中最典型的八重山地堑已经形成洋壳。断裂和岩浆活动主要是单向地向岛弧侧迁移,由洋中脊扩张产生的对称条带状磁异常模式难以解释冲绳海槽的洋壳化进程。
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  • 收稿日期:  2008-01-23
  • 修回日期:  2008-06-09

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