1) supergene karst
表生期岩溶
1.
The karst types are quite rich in the limestone reef or bank reservoir, including synsedimentary karst, pene-sedimentary karst, supergene karst and hydrothermal karst, and so does the dolomitization reef or bank reservoir.
其中,同生-准同生期岩溶的形成机制与礁滩沉积时高频层序旋回向上变浅序列的短暂暴露淋溶有关,表生期岩溶则受控于礁滩沉积后三级层序旋回Ⅰ型界面的暴露淋溶。
2) syn-sedimentary karstification
同生期岩溶
1.
The meteoric diagenesis of the Upper Ordovician carbonate rocks occurred in syn-sedimentary karstification in the No.1 belt of Northwestern Tazhong,Tarim basin——taking the Well Shun-2 as an example;
塔里木盆地塔中Ⅰ号带西北部上奥陶统碳酸盐岩同生期岩溶——以顺2井为例
3) epigenetic karst belt
表生岩溶带
1.
Most vugular stratums distribute beddingly in epigenetic karst belt and submerged flow belt,which form from further denudation of dissolved pores acorss beding.
表生岩溶带和潜流岩溶带的大部分孔洞是顺层分布,沿层面附近发育溶孔的基础上经过进一步溶蚀作用而形成,渗流岩溶带的孔洞则是呈窜洞分布,为淡水沿垂直或斜交层面的缝隙淋滤窜通沿层面发育的溶孔及溶洞进一步溶蚀而形成。
4) The interval karst in the course of sedimentary
同生期层间岩溶
5) pene-sedimentary karst
准同生期岩溶
1.
The karst types are quite rich in the limestone reef or bank reservoir, including synsedimentary karst, pene-sedimentary karst, supergene karst and hydrothermal karst, and so does the dolomitization reef or bank reservoir.
其中,同生-准同生期岩溶的形成机制与礁滩沉积时高频层序旋回向上变浅序列的短暂暴露淋溶有关,表生期岩溶则受控于礁滩沉积后三级层序旋回Ⅰ型界面的暴露淋溶。
6) Epigenic karstification
表生岩溶作用
1.
Epigenic karstification(EK) and burial dissolution(BD) that are the most important diagenesis in carbonate rocks are similar in undergoing effect of the inner factors such as petrology and composition but great different in effect of the outer controlling factors.
塔里木盆地塔北地区主要发育表生岩溶作用;塔中地区西北部不具备发育大规模表生岩溶的地质条件,以发育埋藏溶蚀作用为主。
补充资料：表生
1.妻子同其前夫所生的子女。
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