南海成因模式述评

南海的构造演化与其周边的板块构造运动有密切关系,一直是地学研究的热点问题。现对中外学者关于南海成因模式的观点、模式进行综述分析,讨论涉及主动成因10种,被动类成因7种,涉及代表性观点20个,每一观点都能合理解释一些宏观地质现象,也都与另一些地质现象相悖,还需要进一步修正、发展或用新的资料来验证。这是南海研究日趋成熟的表现,未来将会逐渐各个学说融合发展。从史学的角度讨论了"南海观点"之演变,认为未来主要趋向是研究方法多元化、精细化、定量化,认为南海与周围地块之间主被动关系研究、东南亚盆地群响应序列之间对比、岩石圈结构学、区域岩石发展史、不同学说的动力学定量对比与评价是未来的主要研究关注点,并充分考虑外围被动因素,融合南海的发育历史,并将中生代南海的岩石圈禀赋及历史融于其中是南海成因模式研究的重要方向。

Reviews of genetic models of the South China Sea

This paper summarizes the main models of the South China Sea expansion in the more reference, and classifies and comments on the advantages and disadvantages of those main models. The discussion involves 10 main types of active causes, 7 passive classes, 20 representative views, Each point has some strengths, is worth learning, there are drawbacks, the need for critical development and validation.Which is the mature performance of the South China Sea study, the future will gradually integrate the development of various doctrines.The author discusses the views evolution of the South China Sea from the perspective of historiography and told the main trend is methods diversification ,intensification, quantitative in the future. The author points out that the active or passive relationship between the South China Sea and the surrounding blocks, the comparison of the response sequences of the Southeast Asia basin, the lithosphere structural, history of regional petrology, quantitative comparison and evaluation of the doctrine of different dynamic models are also the main trends of the future. Scholars should give full consideration to the peripheral integration development history of south China sea, and the Mesozoic lithospheric endowment and historical to dissolve into the south China sea which is an important direction of the genetic model of the south China sea.