在核桃园组沉积了碎屑和蒸发岩。
Clastic and evaporite rocks were deposited in the Hetaoyuan Formation.
矿床的含矿岩系大多含有蒸发岩。
蒸发岩、风成沉积物以及潮泛沉积物都是常见于潮上盐难的。
Evaporites, eolian deposits and tidal-flood deposits are common in sabkhas.
海水体系相平衡的研究是蒸发岩矿床成因研究的物理化学基础。
Phase equilibrium of sea water system forms the physicochemical basis of research on the origin of evaporite deposits.
另一种解释出现单矿物蒸发岩的假说是假定存在分隔的蒸发盆地。
Another hypothesis to the existence of monomineralic evaporites is to assume the existence of separate basins of evaporation.
其可溶抽提物中的生物标志化合物分布特征与碳酸盐岩和蒸发岩系很相似。
The distributive characteristics of biomarkers in their soluble extracts are very similar to those in carbonate rocks and evaporite rocks series'.
油气与蒸发岩共生的现象揭示蒸发岩与油气的生成、保存及成藏具有密切关系。
The symbiosis between hydrocarbon and evaporate indicate the affiliation of evaporate and generation of hydrocarbon.
蒸发岩夹层中的深灰色泥岩和页岩的地球化学特征充分体现了盐湖沉积环境标志。
The geochemical characteristics of dark gray mudstone and shale in evaporite layers record the sedimentary environment of salt lake.
根据煤和蒸发岩的地史分布等资料，说明一个海陆相对固定的大地构造模型更符合实际。
The distribution of coal and evaporite in geohistory suggests a geotectonic hypothesis of relatively fixed continents and oceans rather than a drifting model.
早奥陶世马家沟期，在鄂尔多斯东部的陕北地区沉积了近千米厚的碳酸盐岩-蒸发岩地层。
During the Early Ordovician, a suit of carbonate-evaporites had deposited in the east part of the Ordos, which is now known as the Majiagou Formation and up to approximately 1000 meters in thickness.
识别蒸发岩、尤其是变质蒸发岩的标志可以归纳为以下几点 ：（1）岩相及岩性组合 ；
Identification criteria of meta-evaporite could be summarized as: (1) lithologic association and facies;
晚期因周期性的海平面变化导致形成局限浅水盆地、蒸发岩沉积和深水盆地泥岩和重力流沉积。
Till the late stage, the periodic sea-level changes resulted in the formation of the evaporite deposits in restricted shallow-water basin and mudstones and gravity-flow deposits in deep-water basins.
通过分析了该地区蒸发岩地层的沉积特征和沉积条件，认为东营凹陷沙四段蒸发岩类的物质基础是深层卤水；
The evaporite rocks consisted of halite and anhydrite rocks mainly existed in north and centre of Dongying sag where the deep fractures developed.
由于砂岩、泥岩、页岩、蒸发岩、杂色岩等多种软硬岩层互层结构和工程活动等因素的影响，沿着软弱结构面易发生滑坡、差异风化等工程地质问题。
The interbedding natures exist not only between red sandstone, mudstone and shale but also between red beds with coal seam, magmatite, evaporite and varied rock, respectively.
白云岩成因的研究目前还处于假说阶段，主要包括蒸发、渗透回流、海水、混合水以及埋藏白云岩化作用五种模式。
The research on dolomite genesis is in postulation stage at present, which includes five models of vaporization, infiltration and circumfluence, sea water, mixing water and buried dolomitization.
飞仙关组蒸发台地为一套含硫酸盐的富白云岩的蒸发潮坪沉积层系。
The Feixianguan Formation of evaporative carbonate platform is a set of sulfate-bearing evaporative tidal sediments with aboundant dolomite.
上部为中薄层状富泥的含石膏质夹层的泥质泥晶灰岩、微晶白云岩组成的旋回性清楚的似蒸发潮坪层序。
The upper part is a set of evaporite quasi-tidal sequence with clear cycles which is made up of middle-thin-bedded, gypsum-bearing muddy limestone and dolomicrite.
蒸发台地云岩次之，储集性能一般。
Followed by evaporation platform dolomite, the reservoir ability is general.
该含油气构造带的断裂系统和高成熟的油气及其煤系烃源岩是导致蒸发分馏作用的主控因素。
The petroliferous faults in the reservoir and high maturity of hydrocarbon and coal-bearing source rocks are the main factors for controlling the evaporative fractionation.
接受碳酸盐岩沉积时气候相对干热，湖泊水文状况趋于封闭，火山活动频繁，古湖泊水体补给量小于蒸发量。
When the carbonate deposited, the climate was relatively dry and hot, the lake hydrology tended to close, volcanic activities were frequent and the lacustrine water supply was less than evaporation.
接受碳酸盐岩沉积时气候相对干热，湖泊水文状况趋于封闭，火山活动频繁，古湖泊水体补给量小于蒸发量。
When the carbonate deposited, the climate was relatively dry and hot, the lake hydrology tended to close, volcanic activities were frequent and the lacustrine water supply was less than evaporation.
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