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sedimentary paleogeography of the South China Sea
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sedimentary paleogeography of the South China Sea
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理学
南海沉积古地理
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sedimentary paleogeography of the South China Sea
南海沉积古地理
南海经历了晚白垩世到始新世的裂谷阶段、渐新世-中中新世海底扩张阶段,以及中中新世以来关闭俯冲阶段,最终形成亚洲大陆南缘最重要的半封闭边缘海,留下了多样的沉积记录。
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更新时间:2025/12/8 13:19:35