paralic facies

基本解释

The bauxite deposits are formed in shallow paralic environment and belong to transgressive and regressive alternating facies.
成矿作用系多期、多阶段、多成因，属海进海退交互期浅滨海环境形成的沉积铝土矿床。
The Carboniferous Formation of paralic facies in the north margin of Qaidam Basin was drilled in the Gaqiu-1 Well for the first time.
在柴达木盆地北缘，尕丘1井首次钻遇了石炭系海陆交互相地层。
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During the Middle-early Late Permian the epicontinental sea contracted and evolved into a paralic inland depression in the study area and alluvial fan, river, delta and lake facies were formed.
中二叠世至晚二叠世早期陆表海萎缩，本区演变为近海内陆坳陷充填，形成冲积扇、河流、三角洲、湖泊沉积；