构造作用 meaning in English
tectinization
tectogenesis
tectonic action
tectonic process
tectonism
tectonization
Examples
- The mechanical genesis of the complicated rock mass is because several times of tectonism in pro - period made the structure of rock mass in the right dam foundation damaged seriously and rock mass alteration made its mechanical character more anisotropy . after that the fractures in the right dam foundation slope were stretched at the beginning of the quaternary period because in the period yakouhoushan mountain quaquaversal dome was blowups quickly . at the same time , the valley trenching of lancang river reach to 800 - 1000 meter in altitude at the right bank in nuozadu dam site
导致右岸岩体复杂化的成因是，右岸岩体在早期遭受了多期构造作用和岩体蚀变的基础上，第四纪早期丫口后山穹隆的快速隆起与当时河谷下切至800m 1000m高程这一特殊因素组合引起了右岸岩体沿原有的断裂(裂隙)张开，使地下水等风化营力能够到达坡体较深部位，经过长期的风化卸荷作用，形成了右岸复杂岩体。 - This thesis studies each structural layer ' s feature : ( 1 ) structural layer of basement : it is a paleozoic folded basement , whose tectonic deformation and magma intrusion is fiercely , and it is affected by the early hercynian tectonic movement and related to the underthrust and closure ( c1 ) of zhungaer ocean basin and the areal pressing of continents ( c2 - 3 ) ; ( 2 ) structural layer of permian : due to the regional extending and fault depression role in mid - hercynian , it occurred to the combinations of structure and magma in santanghu basin and it ' s periphery area , such as a - granite ' s stock , batholiths and diabase ' s dike . there are many fault depressions possible
按照不同构造层，研究了各构造层的构造特征：基底构造层：受早海西期构造作用的影响，与准噶尔洋盆俯冲闭合、而后陆-陆碰撞的区域挤压构造作用有关，为一构造变形和岩浆侵入活动强烈的古生代褶皱基底。二叠系构造层：受中海西区域性伸展断陷作用的影响，盆地及其周缘地区发育与伸展构造有关的构造-岩浆组合，如呈岩株、岩基状侵位的a型花岗岩以及呈岩墙状侵位的辉绿岩等。 - Situated at the both e w sides of pamir , the s w tarim and tadjik basins have the similar evolution history of tectono sedimentary processes during cenozoic , i . e . steady subsidence with transgressive sequence in paleogene and speedy subsidence with continental molassetype sediments in strong compressive tectonic environment in neogene - quaternery . since neogene , for the effect of pamir and west kunlun s northward moving and thrusting , there is complicated tectonostructural deformation taking place in tadjik and sw tarim . neogene stratigraphic combination and later structural deformation of tadjik basin and southwestern tarim much resemble each other in terms of extent of transpressional processes . paleogene in tadjik basin is main oil - bearing sequence and many substantial oil - gas fields there have been found . so , it can be assured in comparison that there is oil - gas perspective also in southwestern tarim region
第四纪受强烈挤压快速沉降接受陆相磨拉石沉积。自新第三纪以来，受帕米尔西昆仑北移和隆升冲断的影响，塔西南和塔吉克盆地发生了复杂的褶皱冲断变形，其差异在于塔西南明显地受走滑为主的剪压构造作用，而塔吉克盆地是受挤压为主的剪压构造作用的影响。塔西南和塔吉克盆地下第三系岩相组合类似，后期构造变形也相似，塔吉克盆地下第三系是该盆地的主力油层，已有许多油气田发现，因此可以推断塔西南也应该有良好的油气前景。 - Especially interesting is the serpentinous peridotite in this belt occurred as lense blocks of various sizes , and superimposed with other geological masses with faults , and in combine to constitute the mixture . system in the belt . five tectonic stage can be discerned in this area : ( 1 ) south - north ward overthrust ; ( 2 ) sinistral strike - slip ( 3 ) dextral strike - slip ( 4 ) south - north ward overthrust ( 5 ) northeast , northwest late stage fault
本区上述的结构构造特征先后经历了五期构造作用，依次为： ( 1 )南北向逆冲推覆； ( 2 )左行走滑； ( 3 )右行走滑； ( 4 )南北向挤压推覆； ( 5 )北东向、北西向晚期断裂； - Directed by new theories and approaches of sedimentology , diagenesis and reservoir evaluation , focused on marine clastic reservoir of donghe sandstone member , in tarim basin , strata and depositional system of donghe sandstone member are classified ; typical depositional facies types , depositional model and horizontal distribution have been studied through depositional facies analysis of 17 single wells , combined with seismic data . major diagenetic events , stages and " four history " collaboration have been systematically analysesed , furthermore , the relation between reservoir diagenesis and porosity evolution has been built ; thorough studies on reservoir lithology , physical property and pore structure , reservoir development related to depositional envoironment , diagenesis and tectonic has been discussed ; reservoir has been evaluated and predicted by five influential parameters drawn from the results of the study on depositional facies , diagenesis and reservoir characteristic . in the end , favourable reservoir body distribution has been pointed out
本论文以沉积学、沉积岩石学、沉积成岩作用与储层地质学、储层评价技术的新理论新方法为指导，以塔里木盆地巴楚组东河砂岩段海相碎屑岩储层为主要研究对象，通过17口典型井的单井地层沉积相分析和成岩作用分析，结合地震资料，对东河砂岩段地层和沉积体系进行了详细划分，研究了东河砂岩段分布区的典型沉积相类型、沉积模式及其平面展布特征；系统分析了东河砂岩段碎屑岩储层的主要成岩事件、成岩期次及其四史配置关系，指出了储层成岩与孔隙演化的关系；深入研究了东河砂岩段碎屑岩储层的岩石学特征、物性分布、孔隙结构等特征，着重讨论研究了沉积环境、成岩作用和构造作用对储层发育的影响；运用“权重”评价法结合地层沉积相、成岩演化和储层特征研究的结果，选取了五个对储层发育有重要影响的参数对储层进行了整体的评价和预测，指出了塔里木盆地东河砂岩段储层有利储集体的分布状况。