1) biokarst
生物岩溶
1.
Through biochemical and physical processes, they bore and corrode the substrate, thus producing distinct biokarst microforms.
并讨论和展望了生物岩溶微形态研究的前景,开拓生物岩溶研究新思路。
2.
The paper discusses the types and formation mechanisms of the erosional products of biokarst on limestione in Guilin area.
桂林岩溶区石灰岩表面生物岩溶溶蚀形态可分为四类:(1)微溶孔,包括壳状内生地衣微溶孔和藻类微溶孔;(2)溶孔,藻类成因的口小腹大的囊袋状溶蚀;(3)溶坑,藻类、地衣、苔藓及腐殖土成因的柱状、锥状、半球状溶蚀;(4)溶盆,各类生物及腐殖土共同作用而成的壁陡底平的盆状溶蚀。
2) karst deposit
生物岩溶沉积
3) biokarst processes
生物岩溶作用
4) syndepositional rock-dissolution
同生岩溶
1.
Three types of palaeokarst can be recognized in Ordovician non-marine carbonate in Tarim Basin,which are syndepositional rock-dissolution,weathering karstification and buried rock-dissolution.
在塔里木盆地奥陶系海相碳酸盐岩中识别出准同生岩溶、风化壳岩溶、埋藏岩溶3种不同类型的古岩溶作用。
5) 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
6) penecontemporaneous karstification
准同生岩溶
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。
补充资料：岩溶地貌
即“喀斯特地貌”(461页)。
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