The rock types, climate patterns, lake basin and hydrological conditions in this region are contributory to the enrichment of trace elements in salt lake waters.
区域出露的岩性、气候、湖盆及水文等为盐湖水中富集痕量金属创造了有利条件。
There was a terrestrial facies lake basin in study area and mainly developed clastic rock during the late Trias.
研究区晚三叠系为陆相湖盆沉积，以发育陆源碎屑岩系为主。
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