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According to drawing up isopach map of salt in The Kuche depression and isobath map of the top and bottom of salt bed, preliminarily determined the relationship between zhe distribution of the structure and thickness variation of zhe salt bed: the salt bed is relatively thin in the pocket basin, but thick in both sides of the structure belt.

通过编制库车坳陷盐层等厚度图及盐层顶、底面等深度图,初步确定了盐相关构造分布与盐层厚度变化之间的关系:盐层厚度在袖珍盆地较薄,而在两侧构造带厚度较大,盐层厚度较大的地区大致围绕袖珍盆地呈半环带状分布。

The underground gasstorage salt cavern is to artificially dissolve the thick salt layer or salt dome to form a storage cavern for natural gas. It's a main type of gas storage sites.

盐穴地下储气库是利用地下较厚的盐层或盐丘,采用人工方式在盐层或盐丘中水溶形成洞穴储存空间来存储天然气,是储气库的主要类型之一。

The main characteristics of formation are :the salt formation is so developed that may reach about to 3000 meter thickness in Permian above main area of salt dome .

肯基亚克盐下油田的主要地质特点是:下二叠系盐层发育,在盐丘主体部位钻井,盐层厚度可达 30 0 0m ;石炭系灰岩油层孔隙压力系数高达 1。

There are massive salt dome s of great thickness,which ranges from several dozen meters to 3,700 meters,in pre-salt Carboniferous carbonate reservoirs of the Pre-Caspian Basin.

由于盐丘和围岩间存在巨大的速度差异,因此导致盐体本身和下伏地层在常规地震资料中出现反射品质降低、构造失真、畸变(如盐下石炭系目的层地震反射层在盐丘部位出现构造上拉现象),消除盐层的影响是含盐油气盆地勘探的重要课题。

So, researching the influence to reflection wave features made by the factors, such as sand and mud thin-bedding seismic reflection feature, the thickness of single layer in the thin-bedding group, the thickness of subroutine structure, the number of layers in the thin-bedding group, type of incident wavelet, main frequency, sampling rated has the moment current significance and theoretical significance in the qualitative or quantitative seeking of single layer's thickness or thin layer group's thickness in the thin-bedding and forecast of the space distribution laws of thin reservoirs.

目前我国东部的石油勘探工作已进入精细勘探阶段,如何确定陆相地层中薄储层的空间展布规律及其性质已成为一个亟待解决的问题,由于我国东部的绝大多数中、新生代陆相含油盆地大都以薄层砂、泥岩沉积为主,夹有少量薄层碳酸盐岩、页岩及膏盐层,地层岩性和厚度横向变化均较大,而且这些地层的厚度远远低于常规地震勘探的垂向分辨率,因此,从理论上研究沙泥岩薄互层地震反射特征、薄互层组内的单层厚度、子结构厚度、互层组内层数、入射子波类型、主频、采样率等各种因素对反射波特征的影响,将对我们定性或定量求取薄互层组中各单层厚度或薄层组的厚度、预测薄储层的空间展布规律有一定的理论和现实意义。

The relative movement and thickness difference between the overburden and the subsalt were responsible for the disharmony of culminations in the two layers.

盐上沿盐层的滑脱和盐上、盐下层的厚度变化决定了盐上、盐下构造高点的不对应。

It was the salt layer that caused the disharmonic deformation and the leading edge difference between the overburden and the subsalt strata.

盐层的存在正是盐上、盐下不协调变形和盐上变形前缘比盐下更远的原因。

The physical chemistry properties of evaporite beds in Bachu area are analysed.On the basis of the feature of salt beds,the undersaturation salt water drilling fluid is determined.

塔里木盆地复合盐层地层分布广,在不同构造的钻探中都钻遇盐层盐层厚度一般几十米到几百米,岩性以盐岩与膏岩、泥岩、泥质粉砂岩等不等厚互层。

The big velocity difference between salt domes and surrounding rocks leads to poor reflection and distortion of salt bodies and substrata.

由于盐丘和围岩间存在巨大的速度差异,因此导致盐体本身和下伏地层在常规地震资料中出现反射品质降低、构造失真、畸变(如盐下石炭系目的层地震反射层在盐丘部位出现构造上拉现象),消除盐层的影响是含盐油气盆地勘探的重要课题。

By analysis of the insitu stresses field of multicompound saltrock in the Block X of the Kuqa depression, it is indicated that the horizontal stress of salt formation in the middle layer is the highest, while that of overlapping or underlying strata such as salt gypsum rock containing mudstone, mudstone containing salt gypsum rock and mudstone is decreasing in order.

采用该方法对库车坳陷某地区多套复合盐层的地应力场进行分析,结果表明,中间盐层的水平地应力最高,其上、下的膏盐岩含泥岩层、泥岩含膏盐岩层、泥岩层的水平地应力依次降低。

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