deep-water evaporite

基本解釋

Analysis of many samples and study on sedimentary system show that the lake basin was in an under-filling condition. A deep water evaporite formation model was established.
通過大量樣品的分析測試和對這套蒸發(fā)巖沉積體系的研究，認(rèn)為沙四中沉積時期湖盆充填呈現(xiàn)出欠補償?shù)酿囸I狀態(tài)，并建立了深水蒸發(fā)成鹽的沉積模式。
Till the late stage, the periodic sea-level changes resulted in the formation of the evaporite deposits in restricted shallow-water basin and mudstones and gravity-flow deposits in deep-water basins.
晚期因周期性的海平面變化導(dǎo)致形成局限淺水盆地、蒸發(fā)巖沉積和深水盆地泥巖和重力流沉積。