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层内砾岩
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层内砾岩
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理学
层内砾岩
释
intraformational conglomerate
层内砾岩
岩层在准同生期尚处于半固结状态时,经侵蚀破碎和再沉积形成砾石沉积物,再经成岩作用而成的砾岩。因层内砾岩的砾石属于内碎屑,故又称同生砾岩。
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