1) the full Gamma-ray spectrometry
区分岩性
2) lithology differentiating
岩性区分
3) Grike partition
岩溶的分区性
4) paleokarst distribution
岩溶分区
1.
Based on paleohydrological geology, L11 reservoir paleokarstification and the influence of pale-ofluid chemistry and dissolution stage on the development of paleokarst are studied in detail,and then paleokarst distribution is also discussed.
应用古水文地质方法综合分析了L_1~1储层古岩溶发育特征,阐述了溶蚀期次对古岩溶发育程度的影响,并进行了岩溶分区。
5) Regional lithology
区域岩性
补充资料：连续性与非连续性(见间断性与不间断性)
连续性与非连续性(见间断性与不间断性)
continuity and discontinuity
11an父ux泊g四f“山。麻以角g、.连续性与非连续性(c。nt，n琳t:nuity一)_见间断性与不间断性。and diseo红ti-
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