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- W2384306161 abstract "How Taiwan Island was formed is a long - term unsolved problem. Based on principal geological features of Taiwan Island, and through its geological comparisons with both the coastal region of Southeast China and other adjoining areas, this paper proposes a new hypothesis about the forming process of Taiwan Island. In this hypothesis, Taiwan Island is a continental block separated gradually from Southeast China continent in late Mesozoic during the latter's dispersing, drafted counterclockwisely, then collided and combined with the mainland in Miocene in coastal Fujian Province." @default.
- W2384306161 created "2016-06-24" @default.
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- W2384306161 date "2000-01-01" @default.
- W2384306161 modified "2023-09-27" @default.
- W2384306161 title "Taiwan: A continental block drafting counterclockwisely from Eastern Guangdong province, China" @default.
- W2384306161 hasPublicationYear "2000" @default.
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