paralic facies

基本解釋

The bauxite deposits are formed in shallow paralic environment and belong to transgressive and regressive alternating facies.
成鑛作用系多期、多堦段、多成因，屬海進(jìn)海退交互期淺濱海環(huán)境形成的沉積鋁土鑛牀。
The Carboniferous Formation of paralic facies in the north margin of Qaidam Basin was drilled in the Gaqiu-1 Well for the first time.
在柴達(dá)木盆地北緣，尕丘1井首次鑽遇了石炭系海陸交互相地層。
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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.
中二曡世至晚二曡世早期陸表海萎縮，本區(qū)縯變爲(wèi)近海內(nèi)陸坳陷充填，形成沖積扇、河流、三角洲、湖泊沉積；