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protective belt相关的网络例句

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The Garzê-Litang fault belt has experienced a series of complex evolutionary processes since the Paleozoic and is a large-scale, structurally complex ophiolitic mélange belt that has been strongly reworked and dismembered by overthrusting and sinistral strike-slip shear during the Cenozoic Himalayan orogeny.

提要: 甘孜—理塘断裂带自古生代以来经历了一系列复杂的演化过程,为一规模宏大、结构复杂并受到新生代喜马拉雅期逆冲推覆和左行平移走滑剪切作用强烈改造肢解的蛇绿混杂岩带。

An ophiolitic melange belt is discontinuously exposed in Harihada- Chegendalai area to the south of Tuilamamiao in NE of Damaoqi. The ophiolitic mélange in the belt are mainly composed of metamorphic peridotites, metamorphic gabbros, metamorphic basic lavas and high-Mg diorites.

在达茂旗东北推喇嘛庙南15km的哈日哈达-车根达来地区,断续出露一套由变质橄榄岩、变质辉长岩、变质基性熔岩以及高镁闪长岩组成的蛇绿混杂岩。

The Qilian orogenic belt is an important tectonic and metallogenic belt in China.

摘要祁连山造山带是中国的一个重要构造成矿带。

Shenglihe oil shales orientating in NWW-SEE with about 30 kilometers in length are located in the transitional belt between north Qiangtang basin and central uplift belt. The oil shales deposited in Upper Jurassic-Lower Cretaceous marine carbonates and are overlain by tremendous gypsum-salt strata.

胜利河油页岩位于北羌塘盆地与中央隆起之间的过渡带上,呈北西西-南东东向展布,长约30 km,赋矿地层为上侏罗-下白垩统海相碳酸盐岩,其上被厚层膏岩盐覆盖。

In order to solve the important and basic problem of the petrogenesis of "Tiantangzhai migmatitic granite" in the core of Dabie orogenic belt, the detailed 1∶50000 regional geological surveying and the big scale dissection of important region (metamorphic rocks, granites and structure), were operated in about 900km〓 area near Tiantangzhai peak. On the bases of the petrology, mineral chemistry, geochemistry of rare earth element and microelement, isotope geochemistry and chronology, physicochemistry, magmatic dynamics, geodynamics, diagenetic simulation, and regional geophysical data, the theory of cooling age and historical geochemistry and the viewpoint of tectonic evolution are applied to study the petrogenesis of Yanshan epoch granites of this region. On the bases of above studies, the process of tectonomagmatic dynamics after indo-Chinese epoch in Dabie orogenic belt is discussed. The important conclusions are gotten

本文针对大别造山带核部&天堂寨混合花岗岩&成因这一重大基础地质问题,在天堂寨一带近900km〓的面积上进行了详细的1∶5万区域地质调查和大比例尺重点区解剖,通过对区内燕山期花岗岩进行岩石学、矿物化学、稀土微量元素地球化学、同位素地球化学和年代学、物理化学、岩浆动力学、地球动力学和成岩计算机模拟等研究的基础上,结合区域地球物理学资料,应用冷却年龄、历史地球化学理论和构造演化观,阐明区内燕山期花岗岩成因,并以此为基础进一步讨论了大别造山带自印支期以来的构造—岩浆动力学过程,取得了如下的重要认识

Company located in China's largest production base of wire mesh, wire mesh industrial zone Anping County, Hebei Province, the main contrast I have Product-type mesh belt, stainless steel square hole net, stainless steel I-type network, stainless steel Prodenia net filter chip, stainless steel rolling Flower net, stainless steel welded wire mesh, conveyor belt net product is the industry's oldest, largest and most species-wide enterprise, one of the screen now has advanced machinery as well as the corresponding equipment.

公司坐落于中国最大的丝网生产基地,河北省安平县丝网工业区,主要的产品有反差席型网带、不锈钢方孔网、不锈钢席型网、不锈钢斜纹网、滤网片、不锈钢轧花网、不锈钢电焊网、输送带网等产品,是同行业中资格最老,规模最大,品种最全的企业之一,现拥有先进的丝网机械以及相对应的设备。

Major conclusions are given in the end of this paper,that seismic statistical zone bases on the result of seismic belt delimiting,it only arises in and can be used in the especial PSHA method of China with considering spatially and termporally inhomogeneous seismic activities,and its concept should be clearly differentiated from the comcept of seismic belt.

文中最后指出,地震统计区划分是以地震带划分研究为基础,它产生并服务于考虑地震活动时空不均匀性的概率地震危险性分析方法,应将其与地震带概念加以明确区分,并加强其划分原则、理论和方法的研究。

To anatomy the supracrustal composition and structure of orogenic belt with the regional linear structures and their partitioned block and schistous geological masses as the macro-frame(in corresponding to structure units and structure segments) and with the rock masses, structure-rock assemblages, line-featured and belt-featured structures as well as penetrative and non-penetrative foliation (primary stratum and transposition layering) and folds as the texture and structure elements is the main contents of remote sensing analysis.

遥感解析以区域线状构造及由它划分的块状、片状地质体为宏观骨架(对应于构造解析划分的构造单元、构造均匀区段),以地质体中的岩体、构造岩石组合,线状、带状构造,透入性、非透入性面状和褶皱等构造作为解析的结构构造要素,以造山带表壳组成和结构构造解析研究为主要内容。

Finally, as a example of application, the triggering and delaying effect of different fault interaction on seismic potential of active fault along the Xianshuihe-Xiaojiang seismotectonic belt, especially the Xianshuihe fault belt, are studied and discussed.

最后,作为应用实例,对鲜水河-小江断裂带,特别是鲜水河断裂带不同断裂间相互作用的触震效应进行了探讨。

By studying reservoir rock characteristics, diagenesis and physical property, investigation showed that there were distributary channel, branch channel, mouth bar, distal bar, sand sheet, lakeshore, shallow lake and limestone flat . we concluded that the reservoir of N1~N21 is low porosity and permeability reservoir with the types of primary porosity and secondary intergranular porosity, which is in the early diagenetic stage B into the late diagenetic stage A subperiod. The role of effecting reservoir physical property is deposition, cementation, dissolution and tectonic rupture. After researching of reservoir, we divided it into three categories and division the favorable facies belt and relatively favorable. We think that the favorable facies belt is braided river delta front and partly shallow lake in east of the Fault Ⅶ. favorable reservoir is in the first and the second class.

进一步研究了本区碎屑岩储层的岩石学特征、成岩作用特征、物性特征,研究认为该区储集体类型有分流河道砂体、分支河道砂体、河口坝、远砂坝、席状砂砂体、滨湖砂滩、浅湖砂坝砂体及灰坪;N1层属于低孔、特低渗储层,孔隙类型以原生、次生粒间溶孔为主;分析了影响储层物性的因素主要为沉积作用、胶结作用、溶蚀作用和构造破裂作用;进行了储层评价与有利相带预测,将储层分为三类并划分了有利区带、较有利区带,认为Ⅶ号断层以东的辫状河三角洲前缘亚相和部分浅湖亚相是N1的有利储集相带,储层以Ⅰ、Ⅱ类为主。

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