助手标题  
全文文献 工具书 数字 学术定义 翻译助手 学术趋势 更多
查询帮助
意见反馈
   fault fold 的翻译结果: 查询用时:0.188秒
图标索引 在分类学科中查询
所有学科
地质学
更多类别查询

图标索引 历史查询
 

fault fold
相关语句
  断褶
     The maturity of the fault fold structure in Cenozoic controls the development of structural traps in the foothill belt and the formation of fissured gas pools.
     新生代断褶构造发育程度控制了山前带构造圈闭的发育和裂缝性气藏的形成。
短句来源
     In this paper, analysis has been made of each factor affecting the fracture development in the deep zone of Xujiaweizi fault depression (Yingcheng formation stratum ), including structural position where the strata are located, fault development, fault fold combination, physical properties of rock and curvature where the structure develops.
     分析了影响徐家围子断陷深部地层(营城组地层)裂缝发育程度的诸因素,包括地层所处的构造部位、断层发育状况、断褶组合、岩石物性及裂缝发育处曲率等,应用综合评判法确定了各因素对裂缝发育影响程度的权重;
短句来源
  “fault fold”译为未确定词的双语例句
     Under the earth force of the earth rotation and ocean extension in the stress environment with extrusion from south and north, the basin boundary and the margin of Aerjin and Qilian mountains fault fold belt locate is an earth force environment of extrusion and strike slip.
     在地球自转与大洋扩张的地球动力作用下 ,处于南北夹挤的应力环境中 ,使盆地北缘与阿尔金山断褶带及祁连山断褶带南缘舒勒山断裂的边界 ,处于挤压走滑的地球动力环境中。
短句来源
     The contrast of the model description and processing effect for fault, fold and rock characteristics base on some satellite remote sensing images processing project was studied.
     用部分研究项目的卫星遥感图像进行断裂、褶皱、岩性等信息模型描述和处理效果的对比。
短句来源
     The natural mineral springs are obviously controlled by fault, fold and structural alteration zone and the water circulates along deep fracture zone and moves along interlayer faults or tectonic fissures, finally, wells out under an artesian condition.
     矿泉水受构造断裂、活动断裂构造蚀变带及褶皱控制明显,或沿深大断裂深部循环,或沿褶皱层间裂隙、构造裂隙向倾伏方向富集、运移、承压出露。
短句来源
     There are 36 registered tracts with an area of 143 701.4 km 2 controlled by Sinopec in Talimu Basin. According to a comprehensive analysis of various factors as petroleum geological conditions,the degree of exploration,and risk assessment,it is thought that the favourable gas exploration trends should be concentrated at the southeast limb of Akekule Arch,the Dayoudusi-Yaken Structural Belt of Yakela Fault Arch,the Manan Fault Fold Belt of Maigaiti Slope and the Kongquehe Slope.
     中石化在塔里木盆地拥有登记区块 36个、勘探面积 14 370 1.4km2 ,根据油气地质条件、勘探程度及风险评价等多种因素综合分析 ,天然气勘探的有利方向及领域为阿克库勒凸起东南翼、雅克拉断凸大尤都斯—亚肯构造带、麦盖提斜坡玛南断褶带和孔雀河斜坡
短句来源
     Chaidam Basin locates in the triangle region that consists of Aerjin mountain, Qilian mountain and Kunlun mountain fault fold belt in the earth structure of China.
     柴达木盆地在中国大地构造格局中 ,处于阿尔金山、祁连山与昆仑山断褶带组成的三角区域。
短句来源
更多       
查询“fault fold”译词为用户自定义的双语例句

    我想查看译文中含有:的双语例句
例句
没有找到相关例句


The authors make an all-around and systematic study of the funda mental characteristics of Mesozoic-Cenozoic crustal development in the Changbai-Xingan region on the basis of the results of the previous researches and practical -work according to diwa(geodepression) theory.It is concluded that the crustal movement has been gradually increasing its intensity since the Iate Trias and up to the highest point in the middle-upper Jurassic. Under such geological condition of crustal movement a lot of arched fracture-type...

The authors make an all-around and systematic study of the funda mental characteristics of Mesozoic-Cenozoic crustal development in the Changbai-Xingan region on the basis of the results of the previous researches and practical -work according to diwa(geodepression) theory.It is concluded that the crustal movement has been gradually increasing its intensity since the Iate Trias and up to the highest point in the middle-upper Jurassic. Under such geological condition of crustal movement a lot of arched fracture-type and block-type diwa basins were formed. Huge thick Cathysian formations (Molasse strata) with certain terrestrial flysch rhythm were deposited and lots of eruptive rock formations were intercalated in these basins.Great changes took place widely following the strike in these sedimentary formations. One of the chief forms of the crustal movement was the regional fractures which were very active and developed into deep fractures with fault-fold zones distributed widely. In the arched fracture-type and block-type basins there were often formed open bra chyanticlines. Along the deep fracture zones and their adjacent areas the intrusive basic and ultrabasic rocks are widespread. Meta-alkali granite was intruded intensely in fault-fold zones. Magmatism occurred in the sequence from acid to basic-ultrabasic(or alkaline) and abundant mineral deposits were formed.The authors hold that the features of the Mesozoic crustal deve lopment in this region are obviously different from those peculiar to the underlying geosynclinal and platform structral layers. Therefore, a diwa stage indepedent of the platform structural stage should be established, and the region at the present stage must be attributed to diwa regions other than platform ones.

本文根据陈国达教授创立的地洼理论,在前人研究成果及其工作实践的基础上,对长白—兴安地区中新生代地壳发展阶段的基本特征,进行了比较全面系统的研究。认为该区自晚三叠世以来,地壳运动在逐渐增加,直到晚侏罗至早白垩世达到最高潮。在这样地壳运动的地质条件,区内广泛形成有拱曲型和块断型的地洼盆地。在这些盆地中沉积了巨厚层的、具有一定陆相复理式韵律的华夏式建造,并夹杂着大量的火山喷发岩建造。这些沉积建造,普遍的沿走向发生较大的变化。地壳运动的主要形式之一,是区域断裂构造活动强烈,而且形成较为发育的深大断裂构造,断褶带分布广泛。在拱曲型和块断型的地洼盆地中,往往形成开阔的短轴褶皱构造。沿着深大断裂带及其附近,普遍有基性,超基性岩侵入,在断褶带内偏碱性花岗岩浆活动强烈。岩浆侵入活动的顺序,为从酸性岩浆向基性、超基性岩浆(或碱性岩浆)方向演化。并形成有丰富的矿产。 笔者认为该区中新生代地壳发展的特点,与下伏基底地槽和地台构造层所代表的发展阶段的特点具有明显区别。因此,应当将它从区内由地台构造层代表的发展阶段划分出来;它是,一个新的阶段——地洼发展阶段。其现阶段的区域大地构造性质,不应当归入地台区,而是属于地洼区。

The type of the crust and upper mantle of the South China Sea belongs to a structural region of transitional crust from Continent to ocean. It is a diwa region of a new type continental margin sea. It has undergone four evolutional stages: compression swelling(T_3—K_1); tension fault-depression(K_2—E_3~1); tension fault-spreading (E_3~2—N_1); fault terraces-depression and upthrow-fault folding (N_2—Q). The formation of the South China Sea and East Asian continental margin seas is related...

The type of the crust and upper mantle of the South China Sea belongs to a structural region of transitional crust from Continent to ocean. It is a diwa region of a new type continental margin sea. It has undergone four evolutional stages: compression swelling(T_3—K_1); tension fault-depression(K_2—E_3~1); tension fault-spreading (E_3~2—N_1); fault terraces-depression and upthrow-fault folding (N_2—Q). The formation of the South China Sea and East Asian continental margin seas is related to continental margin activation, The process of continental margin activation has undergone five evolutional stages: tensile fault blocks type continental crust diwa; tensile rift-valley type transitional crust diwa; tensile fault-spreading type oceanic crust diwa; compression upthrow-fault type transitional-continental crust diwa and compression collision type continental crust fault -folding zone; forming two big types of diwa zone——continental margin sea type and continental margin island are type, which have just been recognized as diwa regions, The evolution of stress field of Mesozoic-Cenozoic continental margin activation has undergone four stages: weak compression period (T-J_1); intense compression period (J_2—K_1~1); weak tension period (K_1~2—E_1); intense tension period and complex stress period (E_2—Q). The force source of continental margin activation is mainly related to swelling of diffusion action and subsidence of accumulation action of upper mantle matter.

南海地壳-上地幔类型属大陆-大洋过渡壳构造区,大地构造性质是一个新型陆缘海型地洼区 它经压性隆升(T_3-K_1),张性断陷(K_2-E_3~1)、张性断扩(E_3~2-N_1)、断阶陷落与逆冲断褶(N_2-Q)等四个演化阶段。南海和东亚陆缘海的形成与陆缘活化作用相关,陆缘活化的演化过程经历:张性块断型陆壳地洼、张性裂谷型过渡壳地洼、张性断扩型洋壳地洼、压性逆冲型过渡壳-陆壳地洼和压性碰撞型陆壳断褶带等五个阶段。并相应地形成陆缘海型、陆缘岛弧型两大类型地洼带,该两个带是新认识的地洼区。中、新生代陆缘活化的应力场经历弱挤压期(T-J_1)、强挤压期(J_2-K_1~1)和弱扩张期(K_1~2-E_1)、强扩张期和复杂应力期(E_2-Q)等四个演化阶段。陆缘活化的力源主要与上地幔物质隆升扩散和下降凝聚的作用相关。

There are five main seismic structural layers in Manite depression. The top structural layer, being shallow, only produces dense reflections at its bottom, there being an angular unconformity interface under it, Bayanhua layer is a cyclothem consisting of 2 zones with dense reflections and 2 reflection-free zones.In the east part of the depression, it lies on the underlying layer in an obvious angular unconformity. Badalahu structural layer, overlapping on the next one, produces no reflection in the upper part...

There are five main seismic structural layers in Manite depression. The top structural layer, being shallow, only produces dense reflections at its bottom, there being an angular unconformity interface under it, Bayanhua layer is a cyclothem consisting of 2 zones with dense reflections and 2 reflection-free zones.In the east part of the depression, it lies on the underlying layer in an obvious angular unconformity. Badalahu structural layer, overlapping on the next one, produces no reflection in the upper part and dense reflections in the low part. The pre-Badalahu layer on the bottom of the depression is characterized by chaotic reflections. The basement is reflection-free inside. These structural layers, demarcated by well data, reveal the sedimentary facies during each depositional stage,and the contacts between these layers record the following three stages of geological history of the depression. Ⅰ. During the early ahd mid Jurassic, the depression underwent drastic volcanism so that volcanic sequence was formed. Then in late Jurassic, stable river and lake facies formations were formed. Ⅱ. The upper Jurassic formation was eroded because of drastic fault-folding in early Cretaceous, and stable river facies and lake facies sediments were deposited on the eroded landform with new depositional center. Ⅲ. Because of its late subsidence, the different landforms in the south and north parts were unified into a simple depression, thus the late sedimentary formations were formed.

马尼特物陷内有五个地震反射构造层:拗陷顶部地震反射构造层因埋藏较浅,仅见底部密集反射,与下伏地震反射构造层为角度不整合;巴彦花地震反射构造层是空白反射段和密集反射段组成的四次韵律,在拗陷东部,它与下伏地震反射构造层的角度不整合关系明显;巴达拉胡地震反射构造层上部是空白反射段,下部是密集反射段,它超覆在下伏地震反射构造层之上;前巴达拉胡地震反射构造层具有杂乱反射特征,它填充在拗陷底部;基岩地震反射构造层以内部无反射为特征。经钻井标定的地震反射构造层揭示了各时期的沉积相,各构造层互相间的关系记载了马尼特拗陷地质发展历史的三个阶段:第一阶段拗陷经历了早、中侏罗世强烈火山活动,接受了一套火成岩沉积后,进入了晚侏罗世稳定的河、湖相沉积;第二阶段早白垩世强烈的断、褶运动使上休罗系遭到侵蚀,在改变沉积中心的地貌上,接受了稳定发展的河、湖相沉积;第三阶段晚白垩世拗陷回返,结束了南北分带的地貌,形成了统一的简单洼地,接受了拗陷末期的沉积。

 
<< 更多相关文摘    
图标索引 相关查询

 


 
CNKI小工具
在英文学术搜索中查有关fault fold的内容
在知识搜索中查有关fault fold的内容
在数字搜索中查有关fault fold的内容
在概念知识元中查有关fault fold的内容
在学术趋势中查有关fault fold的内容
 
 

CNKI主页设CNKI翻译助手为主页 | 收藏CNKI翻译助手 | 广告服务 | 英文学术搜索
版权图标  2008 CNKI-中国知网
京ICP证040431号 互联网出版许可证 新出网证(京)字008号
北京市公安局海淀分局 备案号:110 1081725
版权图标 2008中国知网(cnki) 中国学术期刊(光盘版)电子杂志社