收稿日期: 1995-02-21
网络出版日期: 1995-06-01
基金资助
国家自然科学基金项目“东海地热异常区的热源机制与构造演化”(编号:49176267)资助.
ODP AND THE OKINAWA TROUGH
Received date: 1995-02-21
Online published: 1995-06-01
李乃胜 . 大洋钻探与冲绳海槽[J]. 地球科学进展, 1995 , 10(3) : 240 -245 . DOI: 10.11867/j.issn.1001-8166.1995.03.0240
The Okinawa Trough which develops at the east part of the East China sea is a active rifting basin and has a series of typical geological and geophysical features as a active modern rifting valley,such as well-developed rift graben,very high heat-flow values and abundant thermal fluid activity,strong crust extension,frequent volcanic and earthquake activity,and a lot of submarine extensional faults. But up to now,there have been many scientific problems which need deep drilling data to be finally solved .ODP's drilling in the Okinawa Trough is of great scientific significance for China.
Key words： Okinawa Trough; ODP; Geological structure.
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