lacustrine climate

基本解釋

Provenance, climate and the feature of palaeogeomorphology combined to effect the lacustrine sedimentation.
湖相沉積主要由物源、氣候和區(qū)域的古地貌特征共同決定。
The studies of Mongolian Holocene climate changes mainly focused on the records of tree-rings, eolian sediments and lacustrine sediments.
矇古全新世氣候變化研究側重於對樹輪、風成沉積和湖泊沉積物的研究。
It shows that Shashi Formation composite of shallow lacustrine and continent source clastic rock and salt deposits that sedimented and developed in the half draught climate.
認爲沙市組是形成於半乾旱氣候條件下的淺湖陸源碎屑巖和鹽湖沉積。