1) The interval karst in the course of sedimentary
同生期层间岩溶
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) 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。
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) 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。
6) 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。
补充资料：围生期窒息
围生期窒息
perinatal period asphyxia
围生新生儿最常见的症状和主要死亡原因。凡能使血氧浓度降低的任何因素都可以引起窒息。各种影响母体与胎儿间血液循环、气体交换的原因，都会造成胎儿窘迫。它可以出现于妊娠期，但绝大多数出现在产程开始后，如缺氧严重而发生较早，则可死于宫内。如果缺氧发生在产程中，使胎儿血液中的二氧化碳刺激呼吸中枢，以致早期发生强烈呼吸动作，喉括约肌失去屏障功能而吸入大量羊水，则成为产时窒息或转成为娩出后的新生儿窒息，如胎儿呼吸中枢已麻痹，则娩出的新生儿即无呼吸。
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