2) weathering karstification
风化壳岩溶
1.
Based on lithology,geophysical data and test data,the authors divided karstification of northern Tarim Basin into three types(penecontemporaneous karstification,buried karstification,weathering karstification)and some subtypes.
本文以岩石学、地球物理资料及测试分析资料为基础,将塔北地区奥陶系碳酸盐岩古岩溶划分为准同生岩溶、埋藏岩溶、风化壳岩溶三大类及若干亚类。
3) karst weathering crust
岩溶风化壳
4) weathering crust reservoir
风化壳储层
1.
Weathering crust reservoir was developed in burried hill in DongpuDepression.
东濮地区第三系基底古潜山风化壳储层，发育有奥陶系的碳酸盐风化壳和石炭二迭系及中生界的碎屑岩风化壳。
2.
Studies suggest that the Ordovician karst weathering crust reservoir and insider karst reservoir developed in yingshan group and yijianfang group.
台地相发育的纯净碳酸盐岩、海西期构造运动导致地层的长期暴露剥蚀、断裂裂隙作用和晚期大气淡水淋溶等是控制塔北风化壳储层形成的重要因素;加里东期溶蚀作用和构造裂隙作用是塔北地区内幕岩溶有效储层形成的主要控制因素。
5) Paleo-weathering crust karst
古风化壳岩溶
6) red weathering crust on limestones
红色岩溶风化壳
补充资料：储层描述(见油气田储层评价)
储层描述(见油气田储层评价)
reseroir evaluation of oil and gas field
储层描述(reseroir evaluation of 011 and gasfield)见油气田储层评价。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条