lacustrine climate

基本解释

Provenance, climate and the feature of palaeogeomorphology combined to effect the lacustrine sedimentation.
湖相沉积主要由物源、气候和区域的古地貌特征共同决定。
The studies of Mongolian Holocene climate changes mainly focused on the records of tree-rings, eolian sediments and lacustrine sediments.
蒙古全新世气候变化研究侧重于对树轮、风成沉积和湖泊沉积物的研究。
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.
认为沙市组是形成于半干旱气候条件下的浅湖陆源碎屑岩和盐湖沉积。