古喀斯特

良好的储层包括与不整合相关的古喀斯特、TST和HST的碳酸盐岩隆、生物碎屑滩和LST的浊积岩、LST底部和HST顶？

Favorable reservoirs are paleo karst related to regional unconformity , carbonate buildup and bioclastic limestone in TST and HST , turbidite in LST and dolostone or grainstone in lower LST and higher HST .

中国南方上震旦统灯影组中的古喀斯特洞穴磷块岩

Paleokarst Cave Phosphorites of the Upper Sinian Dengying Formation in Southern China

本文通过分析古喀斯特微型钟乳石的沉积特征和成因机制，认为是地表淡水渗流形成。

This paper thinks that the micro-stalactite is fresh-water sediments from which sedimentary features and genesis .

以第三纪为主要发育阶段的古喀斯特洞穴在数量上占明显优势。

In quantity , the old karst caves occupy a dominant position , which mainly grew in Tertiary period .

上扬子西部茅口组灰岩顶部古喀斯特地貌的厘定及地质意义

Paleo-karst landforms on top of limestone of the Maokou Formation in the west of the Upper Yangtze platform and its geological significance