【摘要】 本文最大的特点，就是对南海的地质成因研究，明确了一种新的思路，理顺了众多不同研究成果之间的关系。根据我国学者原创的洋壳流力学理论，分析新生代以来，亚洲南下洋壳流分别与自南向北运动的印度洋洋壳流、太平洋洋壳流对峙，造成亚洲南下洋壳流向西、东两个方向产生大分裂，形成众多的回旋、弧形洋壳流，导致印度尼西亚群岛、菲律宾群岛从华南大陆分裂并支离破碎，并产生多个圆弧形的陆缘海；绘出了亚洲南下洋壳流的基本运行路线。更多还原

【Abstract】 This paper clarifies a new way of thinking in the study of the geological genesis of the South China Sea and straightens out the relationship between many different research results. According to the mechanical theory of oceanic crust currents originated by Chinese scholars, it is analyzed that since the Cenozoic era, the southbound Asian oceanic crust currents have confronted the southbound Indian Ocean and Pacific Ocean currents moving from south to north respectively, resulting in a large split in the westward and easterly directions of the southbound Asian oceanic crust, resulting in numerous circumferencing and arc-shaped oceanic crust currents. The Indonesian Islands and the Philippine Islands were divided and fragmented from the South China Mainland, and several arc-shaped marginal seas were produced. The basic route of the southbound Asian oceanic crust current is mapped.更多还原