Structure of weathered crust was controlled by lithofacies, paleoclimate, weathering time, paleotopography, tectonic structure, and later stage preservation.
风化壳结成受控于岩相、气候、时间、古地、、后期保存程度等6大因素;
Structure of weathered crust was controlled by lithofacies, paleoclimate, weathering time, paleotopography, tectonic structure, and later stage preservation.
风化壳结成受控于岩相、气候、时间、古地、、后期保存程度等6大因素;
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