halite造句

• Gypsum and halite are simply thinned or removed altogether .
  石膏与岩盐则逐渐变薄或完全被溶解掉。
• Experimental work indicates that about 14% of the bromide in sea water precipitates with the halite as sea water evaporates .
  实验工作证明，当海水蒸发时，海水中约有14的溴化物与石盐同时沉淀。
• Under the circumstances, gypsum or anhydrite could accumulate to form beds many meters thick, without any co-precipitation of halite .
  在这种环境下，石膏或硬石膏可以堆积成许多米厚的岩层，而没有任何石盐伴生沉淀。
• Salt and halite deposit
  盐和石盐矿床
• The geological characteristics qingjiang halite deposit and its forming mechanism in jiangxi province
  江西省清江岩盐矿床地质特征与成盐机理
• Rock salt , or halite , is mined from natural deposits formed by the shrinking of seas during geological periods
  岩盐或岩盐，被开采自然沉淀在地质学的期间。
• Table salt is halite that has been purified by a chemical process that prevents the mineral from absorbing moisture
  食用盐是一个由化学过程净化了避免吸引湿气的矿物的岩盐。
• Most typically they are gypsum , but can be composed of a variety of other mineral salts like epsomite or halite
  一般来说主要是石膏，但是还包括很多其他矿物盐例如泻利盐或是岩盐。
• Dongpu sag is of the superior geological conditions for forming deep gas pools , including two sets f premium source rocks , variety of sand bodies , sell developed porosity and thick halite and mudstone as cap rocks
  摘要东濮凹陷具有形成深层气的优越基础地质条件：两套优质烃源岩、多种类型的储集砂体和高异常孔隙发育、厚的岩盐和泥岩作为良好盖层。
• In middle and late periods of the early permian , the pre - caspian areas rose successively , the climate became dry , and the environment turned to be supratidal zone ( evaporitic environment ) , resulting in the spread sedimentation of salts and the formation of the salt sediment group ( the upper part of the lower permian ) which consists mainly of halite and anhydrite
  早二叠世中后期由于持续构造抬升，盆地气候变得乾旱，海水变浅，潮上带蒸发环境发育，以致这一时期广泛发育盐类沉积，形成含盐层系，主要由盐岩和硬石膏层构成，并形成许多大小不等的盐丘构造。
• According to these results combined with exploration practice , foot favorable exploration zones are selected , these are the integrated anticline traps below the tertiary gypsum halite , gypsum mudstone in kuqa foreland thrust belts , the second and the third row structural bells in southern junggar foreland thrust belt , the unconventional natural gas pools in die yanshan palaeohigh in north and south of western sichuan basin , the gentle fold structural belt in central sichuan basin and the deep depression in sichuan basin , and the cold take and nanbaxian structural belt in northern margin of qaidam basin
  依据理论分析及勘探实践，优选出4个有利的勘探区带，它们是：库车前陆冲断带古近系、新近系膏盐岩、膏泥岩之下的完整背斜圈闭；准南前陆冲断带第二、第三排构造带；川西北部及南部燕山运动期古隆起、川中平缓褶皱构造带以及深坳陷内部的非常规天然气；柴北缘冷湖南八仙构造带。