The depositional environment of the late Cambrian in Luxi Block was interpreted as the storm-dominated carbonate ramp which includes outer-, mid-, and inner-ramp.
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释义
鲁西地块晚寒武世总的沉积环境被解释为以风暴作用为主的碳酸盐缓坡其中包括外缓坡、中缓坡和内缓坡环境。
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