蒸发岩

柴达木盆地西部第三系蒸发岩与生油岩共生沉积作用研究

Co-sedimentation of tertiary evaporites and oil source rocks in the western Qaidam Basin

蒸发岩的岩相古地理问题

Problems of Palaeogeography and lithofacies of evaporites

这些岩石的出现与蒸发岩有关，其突出特征是富含K、Na、B、Mg等组分。

These rocks are evaporite - related , and characterized by high K , Na , B and Mg .

在核桃园组沉积了碎屑和蒸发岩。

Clastic and evaporite rocks were deposited in the Hetaoyuan Formation .

相应的盖层有硬石膏、页岩、蒸发岩和灰质泥岩；

Seals are anhydrite , shale , evaporate and limerock .

云南中、新生代地质构造演化与蒸发岩建造

Geologic-tectonic evolution and evaporite formation of Mesozoic-Cenozoic era in Yunnan

蒸发岩成因的物理化学研究

A review of physicochemical study on the origin of evaporite

蒸发岩与油气生成、保存的关系

Study on the Relationship Between Evaporate and Hydrocarbon Generation

四川盆地三叠纪蒸发岩地层硫同位素的分布

Sulfur isotope distribution of Triassic evaporite and its geological significance in Sichuan Basin

碳酸盐组分在四川盆地三叠纪蒸发岩系中的分布及其成盐标志研究

Distribution of carbonate component as salt-forming mark in Triassic evaporite in Sichuan Basin

塔里木盆地蒸发岩岩性判别模型及其实现过程

The Evaporate Rock Lithology Discrimination Model for Tarim Basin and its Implementation Process

古构造-古地理背景是蒸发岩沉积的重要控矿条件之一。

The palaeotectonic and palaeogeographic settings are believed to be the important ore-controlling conditions .

中期发育完整碳酸盐&蒸发岩旋回，构成有利储层；

Reservoir rocks developed in carbonate-evaporite cycles in the middle stage during periods of subsidence ;

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 .

蒸发岩建造，包括其下的磨拉石建造构成了一个完整的层控铜、铅、锌矿床所必需的成矿系统。

Evaporite formation altogether with its underlying molasse formation forms a complete metallogenic system for strata-bound deposits .

现代陆相盐湖蒸发岩研究

On Modern Continental evaporites

试论湖北及其邻区印支期有利于形成蒸发岩的构造因素

On tectonic factors favorable to the formation of evaporites of Indosinian period in Hubei and its neighbouring areas

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 .

从早三叠世后期至晚三叠世中期，自东向西陆续有蒸发岩沉积。

Evapo-rite sediments of the Late Lower Triassic to Middle Upper Triassic have formed in succession from east to west .

迄今为止，江汉盆地是我国发现蒸发岩最发育的含油气盆地之一，其中有各种类型的盐构造。

Jianghan basin is one of the Tertiary-Cretaceous oil-bearing basins , in which evaporites are most developed , in China .

济阳坳陷下第三系沙河街组沉积早期，一些凹陷的蒸发岩系中发育了大套暗色泥岩。

On the early age of Paleogene Shahejie Formation , large set of dark mudstones develop in theevaporite in some depressions .

位于南威尔士和格洛斯特郡地区的暗绿色反映了与蒸发岩有关的高锶值。

The dark green tints in the south of Wales and the Gloucestershire area reflect high strontium values associated with evaporites .

新疆是我国现代盐湖主要分布区之一，蒸发岩矿物类型较全，现已发现有32种矿物，其中有近年新发现的数种矿物以及新类型盐湖&硝酸盐盐湖；

There are 30 evaporite minerals , including those found in recent years and in new-type-nitrate salt lakes newly discovered in Xinjiang .

邯邢地区中奥陶统蒸发岩特征及其对内生铁（硫）矿床的控制

Features of the Middle Ordovician evaporites and its control over the endogenic iron ( sulfur ) defosits in Han-xing district , hebei

世界上许多大型含油气盆地都有蒸发岩分布，蒸发岩与沉积盆地的含油气性有着非常密切的关系。

Evaporates normally occur in large-scale petroliferous basins in the world , so there exist closely relations between evaporates and petroliferous basins .

通过大量样品的分析测试和对这套蒸发岩沉积体系的研究，认为沙四中沉积时期湖盆充填呈现出欠补偿的饥饿状态，并建立了深水蒸发成盐的沉积模式。

Analysis of many samples and study on sedimentary system show that the lake basin was in an under-filling condition . A deep water evaporite formation model was established .

通过对该段地层沉积相的分段分析和不同韵律结构的划分以及含盐盆地沉积特征的研究，得出该含盐系地层的浅湖泻湖蒸发岩的沉积建造。

From section by section analyses of strata sedimentary facies , rhythmite division and study on salt basin sedimentary characteristics have recognized the sedimentary formation of shallow lacustrine lagoon evaporite .

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 .

这些蒸发岩在以后的地质历史中发生了复杂的变化，并且在含蒸发岩的碳酸盐岩地层中形成了许多盐类矿床及其它金属和非金属矿床。

Complicated changes have taken place in evaporite rocks in the later years . Yet , a series of nonmetallic and metallic deposits have formed in carbonate rocks bearing evaporite rocks .

这一研究成果表明，坪洲组是一盐系地层，大鹏湾盆地在晚白垩世&古近纪时期是一演化程度较高的硫酸盐型蒸发岩盆地。

This result suggests that the Pingchau Formation is a salt-bearing sequence , and that the Mirs Bay was once a highly saline evaporate basin during the late Cretaceous to Eogene .