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1)  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。
2)  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。
3)  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。
4)  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
5)  The interval karst in the course of sedimentary
同生期层间岩溶
6)  penecontemporary doIostone
准同生白云岩
补充资料:法祥(唐同州)《净土往生传》
【法祥(唐同州)《净土往生传》】
释法祥。同州澄城人。童稚之岁。操志自立。周武之末。冠带僧徒。其间负明敏者。必录用之。祥以所负获升官路。隋复大化。祥乃陈表乞再为僧。寻住杨都大兴国寺三十年。潜思玄籍。罗总权实。开蒙指俗。动有饶益。每以饶益之善。助生安养。至于基一堂构一室。形器土木之为。必引愿之。唐武德七年有疾。至其增剧。弟子在祥之侧。闻祥称佛之声。继发于口。初未悟之。谓其病中念佛。以著愿想。寻回顾之。乃见其房之西壁有光焉。其光圆合。若诸宝镜。虽他国土毕亦现之。光中又有频伽之鸟鼓冀四来。祥指所见谓弟子曰。频伽诸鸟。汝徒见耶。见之他日净土必见吾也。旋而光隐。祥亦亡焉。于是用西域茶毗法。收舍利而葬焉。
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