构造的
- 与 构造的 相关的网络例句 [注:此内容来源于网络,仅供参考]
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The fold-and-thrust structure in the northwestern margin of the Junggar Basin is composed of the northern monocline belt,the middle syncline belt,the Ke-Wu faulted belt and the frontal slope belt,and is divided into the upper and lower structural layers in vertical.
准噶尔盆地西北缘冲断构造自西向东由北部单斜带、中部向斜带、克—乌断裂带和前缘斜坡带4个部分组成,在纵向又可划分为上、下两个构造层,上构造层的冲断序列要先于下构造层。
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Wuxia area was located on the eastern of northwest Junggar basin, it was a zone of bruchfalten affected by multiphase tectonic activity, have many faults and its fold morphology were very complicated, underwent three large structural activities, which happened in the late Hercynian movement, Indo-Chinese movement, and the Yanshan movement, by this,strata of Wuxia area can be divided into two primary tectonic sequences and seven secondary tectonic sequences, on plane, Wuxia area can be divided into three secondary structural units from north to south,they are foreland thrust belt, Wuxia fault fold belt and monocline belt, further, from west to east Wuxia fault fold belt can be divided into four fault fold belts.
乌夏断裂带位于准噶尔盆地西北缘冲断带东段,是一个受多期构造叠加影响的断褶带,断裂发育,褶皱形态复杂,自成盆期以来经历了海西、印支、燕山和喜马拉雅等多期构造运动,可划分为2个一级构造层序和7个亚构造层序,可划分出山前冲断带、乌夏断褶带、南部单斜带三个次级构造单元和四个更次一级的构造单元。
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The influence on oil and gas,combination types, tectonic origin mechanism ,orogenic zone thrust-nappe tectonics and benching thrust-nappe tectonics are summaried in this paper.
本文概述了逆冲推覆构造对油气的影响,组合类型,构造成因机制,造山带逆冲推覆构造和台阶式逆冲推覆构造。
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By the analysis to the chronogenesis of NE、NW、EW structure in the Northeast of Sishuan ,and the compound analogy of Daba mountain structure belt with West Xiang'E structure belt, three stages which were Indo-chinese stage, Yanshan stage and Himalayan stage could be separated in the studied area.
通过对川东北地区NE、NW、EW 向构造相互形成时序关系分析,并与大巴山构造带及湘鄂西构造带的交切复合类比,从而在研究区筛分出印支、燕山和喜山三期构造。
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Beiqinling is between Shangdan Fault and Baoji-Luonan-Luanchuan Fault, it have own particularities in structure, geochemistry, physical geography and stratigraphy, on the stand of tectonic, it's the real division between north China and south China, and the key region to study the evolution of Qinling erogenic belt during later Paleozoic-early Mesozoic.
北秦岭构造带夹持在宝鸡—洛南—栾川断裂带和商丹断裂带之间,其组成及结构构造既不象其北侧的华北板块南缘构造带那样与华北板块相似,也不象其南侧的南秦岭构造带那样与扬子板块相似,在地层、构造、地球化学和地球物理各方面均具有独特性,从大地构造意义上说,它才是中国大陆南北之间的真正分界带,也是解析秦岭晚古生代一早中生代演化的关键区段。
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There are enormous differences between the two sides of the tectonic zone in sedimentary formation, tectonic activity, geophysical fields and geotectonic development Hence the authors as...
提出在该延伸带两侧沉积建造、构造活动,地球物理场和大地构造发展上均有显著差异。并进一步探讨该断裂构造带在大地构造上的意义。
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In view of an analysis from lithospheric geoid, horizontal stress and existing seismic tomographic data and so on, they show that Chinese mainland and adjacent area is controlled by mantle dynamics of interaction, mutual influence and constraint by western Pacific ocean plate, Indian plate and circum-Siberian arc tectonics that formed after Paleo-Asian ocean closed, which consist of three tectonic areas, with on the base of the Tethyan tectonic realm. Overall tectonic framework of the Chinese mainland is outwards obduction along main tectonic borders within shallow crust and inwards subduction and convergence within deep lithospheric mantle from south-western, south-eastern and northern parts, respectively.
基于岩石圈大地水准面异常、水平应力场和地震层析等地球物理资料综合分析可知,中国大陆及其毗邻地区在特提斯构造基础上,处于西太平洋板块、印度板块和古亚洲洋及其闭合之后环西伯利亚弧形等三大全球构造体系域相互作用、相互影响和相互制约的地幔动力学控制之下,总体大地构造格局是浅部地壳分别沿主要构造边界向外仰冲,深部岩石圈地幔则从西南、东南和北部向中国大陆俯冲会聚,使之整体处于地幔会聚挤压的大地构造背景。
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Based on the equilibrium section principle and by decompaction correction, the profiles of the Cenozoic structural evolution in the north of the Dongying Sag, the Bohaiwan Basin and the paleostructural map s of the subface of the Sha-3 Member before the sedimentation of the Sha-1 Member and the Guantao Formation were compiled.
根据平衡剖面原理、经过去压实校正编制了渤海湾盆地东营凹陷北部地区新生代构造演化剖面图以及沙一段沉积前和馆陶组沉积前的沙三段底面古构造图,并从演化剖面和平面古构造两方面入手进行研究,较系统地总结了该区新生代构造演化特征。
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Selecting two ophiolite zones (namely Hongliugou-Lapeiquan ophiolite zone and Sulamutage ophiolite zone) respectively located within the southern and northern part of the Altyn fault and based on analysis of field geology characteristics and geochemistry, this paper recognized the rock types (mainly mafic and ultramafic rocks) within the melanges and subdivided each lithological unit based on tectonic environment.
本文以阿尔金断裂带南、北两条蛇绿混杂带(即红柳沟-拉配泉带和茫崖-苏拉木塔格带)为研究对象,根据野外地质特征和地球化学分析,鉴定混杂堆积的岩石种类,以构造环境划分各岩石单元,最后用大地构造相研究方法恢复阿尔金地区古构造格局,以碰撞造山带理论讨论其古构造演化。
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Analysis on the stress status of sprayed porcelain coatings;2. Earthquakes in the Shanxi-Reservoir,Zhejiang Province:source parameters determining and description of the tectonic fault and static stress status ;3. From the result,the stress status evaluation based on geology dynamic division has important significance for the design and implementation of coal mining engineeri.
为了研究矿区岩体应力状态,利用地质动力区划方法研究了区域地质构造,建立了区域地质模型,计算了构造应力场并划分出高构造应力区和高构造应力梯度区,分析了岩体应力状态与巷道稳定性、开采沉陷、矿山压力显现等的关系。
- 推荐网络例句
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They weren't aggressive, but I yelled and threw a rock in their direction to get them off the trail and away from me, just in case.
他们没有侵略性,但我大喊,并在他们的方向扔石头让他们过的线索,远离我,以防万一。
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In slot 2 in your bag put wrapping paper, quantity does not matter in this case.
在你的书包里槽2把包装纸、数量无关紧要。
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Store this product in a sealed, lightproof, dry and cool place.
密封,遮光,置阴凉干燥处。