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作 者:关成尧 赵国春[2] 张厚和[3] 邱磊 高剑波 廖宗宝 GUAN Cheng-yao;ZHAO Guo-chun;ZHANG Hou-he;QIU Lei;GAO Jian-bo;LIAO Zong-Bao(Department of Earthquake Science,Institute of Disaster Prevention Science and Technology,Sanhe 065201,China;School of Earth Sciences and Resources,China University of Geosciences(Beijing),Beijing 100083,China;CNOOC Research Institute,Beijing 100028,China)
机构地区:[1]防灾科技学院地球科学学院,三河065201 [2]中国地质大学(北京)地球科学与资源学院,北京100083 [3]中海油研究总院,北京100028
出 处:《科学技术与工程》2020年第7期2515-2527,共13页Science Technology and Engineering
基 金:河北省高等学校人文社会科学研究重点项目(SD162001);中央高校基本科研业务费团队项目(ZY20180104);中央高校科研基本业务费项目(SD162001);中国地震局教师科研基金(20150103)。
摘 要: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。The main models of the South China Sea expansion in the more reference is summarized,and the advantages and disadvantages of those main models is classified and commentd on.The discussion involves 10 main types of active causes,7 passive classes,20 representative views.Each point has some strengths,being worth learned,There are drawbacks,they 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 active or passive relationship between the South China Sea and the surrounding blocks,the comparison of the response sequences of the southeast Asia basin is pointed out.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.Full consideration to the peripheral integration development history of south China Sea sould be given,and the Mesozoic lithospheric endowment and historical should be dissolved into the south China Sea which is an important direction of the genetic model of the South China Sea.
分 类 号:P548[天文地球—构造地质学]
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