fault depression造句
例句与造句
- Characters of paleogene sequence stratigraphy and its sedimentary system in tangyuan fault depression
汤原断陷古近系层序地层及沉积体系分析 - Geological features and potential resources of coal bed methane in suibin fault depression of sanjiang basin
三江盆地绥滨断陷地质特征及煤层气资源潜力 - Sequence stratigraphy with fills of volcanic rocks in xujiaweizi faulted depression of songliao basin , northeast china
徐家围子断陷火山岩充填的层序地层 - Structural features and evolution of contemporaneous reversed faults in gas faulted depression in western qaidam basin
柴西地区尕斯断陷同生逆断裂构造特征与形成演化 - Application of curvature method to fissure forecast of the yingcheng formation stratum of xujiaweizi fault depression
曲率法在松辽盆地徐家围子断陷营城组地层裂缝预测中的应用 - It's difficult to find fault depression in a sentence. 用fault depression造句挺难的
- Hailar basin is a fault depression at the early forming stage , and becoming a depression at the end of yimin stage
海拉尔盆地为一走滑断陷型盆地，早期为断陷型盆地，伊敏组末期逐渐转变为坳陷型盆地。 - Chagan fault depression has favorable petroleum geology conditions , the evolution of its source rocks could be divided into three stages
查干凹陷具有较好的石油地质条件，烃源岩有机质演化在垂向上可划分为三个阶段。 - The northeast ehen secondary fault depression , maoxi fault - nose and maonan slope should be favorable places for prospecting in the near future
提出了额很洼陷东北部和毛西断鼻构造以及毛南斜坡，是近期首选的有利勘探目标区带。 - The structure units are redivided . the main structure style of chagan fault depression is summarized , in which the extensional structure are the principle part . its kinematics characteristics are analysed
对查干凹陷的构造单元重新进行了划分，总结了查干凹陷的主要构造样式，伸展构造是主体，并对其运动学特征进行了分析。 - The upper tertiary oil - type gas is mainly positioned in the east of the mangai depression , the aljin slope and the southwestern faulted depression , while the upper coal - type gas in the yiliping depression , the sanhu depression and the erboliang - yikeyawuru structural belt
上第三系油型气主要分布于茫崖凹陷东部、阿尔金斜坡和柴西南断陷区；上第三系煤型气主要分布于一里坪凹陷、三湖凹陷和鄂博梁伊克雅乌汝构造带。 - On the basis of the characteristics of sequence stratigraphy of the cenozoic in puwei sag , dongpu depression , the sequence stratigraphic framework of the cenozoic is set up , including two supersequence sets which is fault depression filling supersequence sets of the eocene , and depression filling supersequence sets of the tertiary
根据东濮凹陷濮卫洼陷新生界层序地层的发育特征，建立了濮卫洼陷新生界层序地层格架，将濮卫洼陷新生界概括为一个盆地充填序列，包括古近系凹陷充填超层序组和新近系坳陷充填超层序组。 - 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。 - Due to the multi - period tectonic movement and evolution of mechanical mechanism , syndeposition structures occur extensively in jiyang sag , the base of the sag subsided alternatively during the fault depression , which resulted in sinking of top bending and complicated block structure accordingly , reconstructed the syndeposition intensively , and produced the special structural landscape in combination with all levels of faults and sedimentary formations within it
摘要济阳坳陷由于受到多期构造运动的影响，在前第三系古地形高点背景上广泛发育同沉积背斜构造，然而由于坳陷在断陷期基底滚动式沉降，造成挠曲顶部的塌陷，形成复杂的块断结构，使本区同沉积构造发生强烈改造，往往与各次级断层或沉积地层相复合，表现出独特的构造景观。 - Yinggete - bagemaode metamorphic core complex belt with three - layer construction is put forward , which evolved from late jurassic to cretaceous . the extensional simple shear model of the chagan fault depression is established . the tectonic evolution and the dynamics character of chagan fault depression and its adjacent mesozoic - cenozoic basins are discussed : at the end of triassic continental orogeny increased crust thickness crust uplift and denudation were happened ; jurassic was a period of local partly extensional collapse of erogenic belt and cretaceous was a period of widely extensional collapse of postorogenic erogenic belt ; cenozoic was a period of the development of stable intracontinental depression with the character of long distant collision response and weaked compression flexure
讨论了查干凹陷及邻区中-新生代盆地构造演化及其地球动力学特征，三叠纪(印支期)为陆内造山作用与地壳增厚、隆升剥蚀阶段；侏罗纪(燕山早期)为造山后造山带的局部伸展垮塌阶段；白垩纪(燕山晚期)为造山期后大规模伸展垮塌作用与伸展盆地的发育阶段；新生代(喜山期)为远距离碰撞效应与弱挤压挠曲性质的稳定大陆内坳陷的发育阶段。 - It could be divided into six paleogeotemperature evolution stages from early cretaceous to recent based on the result of apatite fission - tracks analysis ; subsidence - buried history analysis shows that chagan experienced fault depression stage during early cretaceous bayingebi - suhongtu period , transional stage from fault depression to sag in yingen period , and sag stage since wulansuhai stage
磷灰石裂变径迹模拟分析结果认为早白垩世至今大致可分为6个古地温演化阶段；沉降?埋藏史模拟揭示查干凹陷经历了早白垩世巴音戈壁?苏红图期的断陷期、银根期的断?坳陷转化期和晚白垩世乌兰苏海期以来的坳陷期。
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