Geologically, the rock mass of the Mogao Grottoes is semi-binder calcirudite of the quaternary sediment of very loose structure.
莫高在地质学上属第四纪沙泥质、钙质半胶结砾,结十分松散。
Geologically, the rock mass of the Mogao Grottoes is semi-binder calcirudite of the quaternary sediment of very loose structure.
莫高在地质学上属第四纪沙泥质、钙质半胶结砾,结十分松散。
Mainly developed are fan - delta, deep lake turbidite and calcirudite deposit, and also alluvial fan deposit in early period.
各时期形成的砂和粒屑灰储集,储集提供了有利的场所。
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