南海中部地质-地球物理特征与南海海盆演化探讨
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摘要: 本文根据6万千米重、磁、水深测量资料,结合前人工作,对南海中部基底、断裂、岩浆活动进行了分析和推断,并就南海海盆的成因演化进行了初步探讨,认为除中渐新世—早中新世南北向扩张之外,南海尚发生过更早一期的扩张。
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任纪舜等,中国大地构造及其演化.科学出版社.1980, 61-62. 杨森楠等,中国区域大地构造学,地质出版社.1985, 218-238. 中国科学院南海海洋研究所地质构造室.南海中部和北部地质构造的基本特征,南海海区综合调查研究报告(一),科学出版社,1982, 1-21. Kadrass,H. R.,M. Wiedicke, P. Cepek, H. Kreuzer and P. Miiller, Mesozoic and Cainozoic rocks dredged from the South China Sea (Reed Bank area) and Sulu Sea and their significance for plate-tectonic reconstruction, Marine and Petroleum Geology, 3(1986),2:19-30. 张文佑,断块构造导论.石油工业出版社.1984, 101-102. Taylor, B. and D. E. Hayes, Origin and history of the South China Sea Basin, The Teclonic and Geologic Evolution of Southeast Asian Seas and Island, Part 2, American Geophysical Union Geophysical Monograph 27.1982, 23-56. 吕文正等,南海中央海盆条带磁异常特征及构造演化,海洋学报.8 (1987),1:69-78. Holloway,N. H.,North Palnwan Block,Philippines——Its relation to Asian Mainland and role in evolution of South China Sea, AAPG Bull.,66 (1982),9:1355-1383. -
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