论冲绳海槽的张裂运动

林长松; 王英

论冲绳海槽的张裂运动

林长松,
王英

国家海洋局第二海洋研究所, 杭州 310012

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出版历程
- 收稿日期: 1997-11-05
- 修回日期: 1999-04-05

The tension movement of the Okinawa Trough

Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012

摘要

摘要: 琉球岛弧系向海沟方向的旋张掀斜运动和岛弧-弧后地区地幔流的波动运动是冲绳海槽张裂运动的动力源.在张应力场作用下,自早第三纪以来,冲绳海槽长期为一负向构造.现代海槽是老海槽的继承性、阶段性发展的产物,晚中新世以来冲绳海槽的张裂运动增强与菲律宾海板块的俯冲作用增强密切相关,但它不可能形成大规模的扩张.
- 张裂运动 /
- 波动运动 /
- 旋张掀斜运动
Abstract: The tilt movement of the Ryukyu island-arc system toward the ocean trench and the waving movement of the mantle stream in the island-arc-back-arc area are the power source of the movement of the Okinawa Trough,The Okinawa Trough is a negative structure under the tension field after Tertiary,Modern trough inherits the old trough and develops in its staged style.From Later Miocene,the increase of tension movement of the Okinawa Trough is deeply related to the increment of subduction movement of the Philippine Sea Plate,but this movement cannot cause a large-scale spreading.
- Tension movement /
- waving movement /
- tilt movement

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参考文献(23)

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