沉没事件是碳酸盐岩台地发育、演化终止的一个重要标志,它具有特定的地质、地球化学及地震反射特征。
The drowning event is a key marker representing the termination of carbonate platform development and has some features of geology, geochemistry and seismic reflection.
沉没事件是碳酸盐岩台地发育、演化终止的一个重要标志,它具有特定的地质、地球化学及地震反射特征。
The drowning event is a key marker representing the termination of carbonate platform development and has some features of geology, geochemistry and seismic reflection.
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