摘要
在多次赴冲绳海槽地球物理调查的基础上，综合国内外的调查研究成果，对冲绳海槽地质构造学研究的历史、已查明的地球物理场特征、海底构造特征和需要进一步探讨的问题作了系统的总结。阐明了ＯＤＰ在冲绳海槽钻探的重要意义。
The Okinawa Trough which develops at the east part of the East China sea is a activerifting basin and has a series of typical geological and geophysical features as a active mod-ern rifting valley,such as well-developed rift graben,very high heat-flow values and abun-dant thermal fluid activity,strong crust extension,frequent volcanic and earthquake activi-ty ,and a lot of submarine extensional faults. But up to now ,there have been many scien-tific problems which need deep drilling data to be finally solved. ODp’s drilling in the OKi-nawa Trough is of great scientific significance for China.
出处
《地球科学进展》
CAS
CSCD
1995年第3期240-245,共6页
Advances in Earth Science
基金
国家自然科学基金
