1) cave horizon
洞穴层
1.
Based on the principle that caves develop along the water table in a condensed carbonate land, cave horizons are correlated and caves identified from wells are reconstructed in paleogeomorphic sections.
洞穴层是识别多期次岩溶旋回的标志,是岩溶旋回连接沉积旋回及周期性海平面变化的纽带。
2) Cave layer
洞穴地层
3) multiplayer karst caves
层状洞穴
4) cave reservoir
洞穴型储层
1.
The types of reservoir are cave, fissure-dissolution pore and fissure , and the cave reservoir is the dominating reservoir.
储层类型主要有洞穴型、溶蚀孔隙-裂缝型和裂缝型储层3类,以洞穴型储层为主。
5) cavernous formation
洞穴性地层
6) Speleothem microlayer
洞穴碳酸盐微层
1.
Speleothem microlayers can be manifested .
近几年，在高分辨率气候－环境变化研究中，洞穴碳酸盐微层逐渐受到人们重视。
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