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The marginal ocean basin's formation and evolution model may be as follows: early Triassic, rift was formed by extension and splitting in India (Gondwana) continental margin during it was drifting southward; late Triassic, the rift had been joined in the |
中文意思: 洋盆的演化模式是:早三叠世,随着印度(冈瓦纳)大陆向南漂移,其北部边缘因引张裂解产生裂谷,于晚三叠世向东开口与新特提斯洋主体连通,洋盆初具洋壳性质,北侧形成阿依拉-仲巴微陆块。 |
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