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200字范文 > 南海西缘断裂带 western-edge faults of the South China Sea英语短句 例句大全

南海西缘断裂带 western-edge faults of the South China Sea英语短句 例句大全

时间:2019-02-03 23:46:47

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南海西缘断裂带 western-edge faults of the South China Sea英语短句 例句大全

南海西缘断裂带,western-edge faults of the South China Sea

1)western-edge faults of the South China Sea南海西缘断裂带

1.Geodynamic mechanism of dextral strike-slip of thewestern-edge faults of the South China Sea南海西缘断裂带右行走滑的地球动力学机制

英文短句/例句

1.Geodynamic mechanism of dextral strike-slip of the western-edge faults of the South China Sea南海西缘断裂带右行走滑的地球动力学机制

2.Geophysical features of the western-edge fault zone of the South China Sea and its significance of tectonic geology南海西缘断裂带的地球物理特征及其构造地质意义

3.Shule river fault zone is a buried deep basement fault zone, it locates in the Southof Beishan area in Gansu Province.疏勒河断裂带位于甘肃省北山地区南缘,为隐伏基底深断裂。

4.Geotransect from Xisha Trough in the northern continental slope of the South China Sea to Hengchun Peninsular in Taiwan南海北部陆缘西沙海槽—台湾恒春半岛地学断面

5.Wuxia fault belt in the eastern part of northwestern margin of Junggar basin is an important part in the thrust belt of the northwestern margin.乌夏断裂带位于准噶尔盆地西北缘的东部,是西北缘冲断带的一个重要组成部分。

6.The strain partition in the southern margin of the North China plate:A study of Luonan-Luanchuan fault belt and the strong deformation belt in the northern margin of the Qinling orogenic belt华北板块南缘的变形分解:洛南—栾川断裂带与秦岭北缘强变形带研究

7.GRAIN SIZE DISTRIBUTION AND MICROSTRUCTURE CHARACTERS OF THE FAULT UGE IN THE EAST SECTION OF NORTHERN EDGE OF WESTERN QINLING MOUNTAIN西秦岭北缘断裂带东段断层泥的粒度分布和显微构造特征

8.Study on tectonic properties in northwest fracture zone in Chaluhe fault depression of Yitong basin伊通盆地岔路河断陷西北缘断裂带构造特征研究

9.A Paleoeathquake Study on the Moxi Fault and Tarwan-Chijiaciwo Fault at the Margin of Tibetan Plateau;青藏高原东南缘磨西断裂和东北缘塔尔湾—池家刺窝断裂古地震研究

10.STRUCTURAL FEATURES AND TECTONIC EVOLUTION OF THE WEI-ZI-LUO FAULT ZONE IN SOUTHWESTERN GUIZHOU PROVINCE贵州西南部威-紫-罗断裂带构造特征及演化

11.Study on Deep Crustal Structure Along Onshore-offshore Seismic Profile Across the Littoral Fault Belt in NE South China Sea;南海东北部海陆地震联测与滨海断裂带深部结构研究

12.Geophysical Evidences of Some Important Faults in South China and Adjacent Marginal Seas Region华南及其相邻边缘海域一些重要断裂的地球物理证据

13.The distribution regularity and master control agency of the Permian oil play in the Wuxia fracture belt in Wuxia fracture belt,Zhunge"er Basin准噶尔盆地西北缘乌夏断裂带二叠系油气成藏组合

14.Discussion on controlling factors for Carboniferous hydrocarbon accumulation in the Ke-Bai fractured zone of the northwestern margin in Junggar Basin准噶尔盆地西北缘克-百断裂带石炭系油气成藏控制因素新认识

15.Study on the structural features and hydrocarbon accumulation modes of Wuxia fault belt in the northwest margin of Junggar Basin准噶尔盆地西北缘乌夏断裂带构造特征与油气成藏模式

16.A Study on Movement Characteristics and Mechanism of the Fault Zone Along the North Edge of West Qinling Mountains Since Late Epipleistocene Epoch西秦岭北缘断裂带晚更新世晚期以来断裂运动的基本特征及运动机理

17.The northern piedmont fault of the Liulengshan Range lies along the southern edge of Yangyuan basin.六棱山北麓断裂位于阳原盆地南缘,是一条总体走向北东东、倾向北北西的倾滑正断裂。

18.The Haiyuan fault zone and the Zhongwei-Tongxin fault zone are main faults in the northeastern corner of the Tibet Plateau.海原断裂带和中卫-同心断裂带是青藏高原东北隅二条主要断裂带。

相关短句/例句

South Altyn border faults zone南缘断裂带

3)north-west fault zone西北缘断裂带

1.By using outcrop,core,geophysical data,it is concluded thatnorth-west fault zone in Yitong Basin is compressive and reversed faults which are well developed.综合利用钻井、露头岩心及地球物理资料,确立了伊通盆地西北缘断裂带在古近纪右行走滑伸展之后、新近纪以来为挤压性质,并发育一系列逆断层及相关褶皱等构造。

4)littoral fault belt of South China华南滨海断裂带

1.Thelittoral fault belt of South China is an active fault belt having experienced several stages of activities.华南滨海断裂带是一条经历多期次活动的强活动断裂带,它控制着台湾海峡的地震活动和构造活动,也控制着台湾海峡的形成和演化。

5)Nansha Trough fault zone南沙海槽断裂带

1.Preliminary analysis of the activity of theNansha Trough fault zone南沙海槽断裂带活动性初步分析

6)western segment of Haiyuan fault zone海原断裂带西段

延伸阅读

断裂带亦称“断层带”。有主断层面及其两侧破碎岩块以及若干次级断层或破裂面组成的地带。在靠近主断层面附近发育有构造岩,以主断层面附近为轴线向两侧扩散,一般依次出现断层泥或糜棱岩、断层角砾岩、碎裂岩等,再向外即过渡为断层带以外的完整岩石。断层带的宽度以及带内岩石的破碎程度,决定于断层的规模、活动历史、活动方式和力学性质,从几米至几百米甚至上千米不等。一般压性活压扭性断层带比单纯剪切性质的断层带宽。在一些大型的断层带中,由于被后期不同方向的断层切错,和夹有一些未破碎的大型岩块,只是断层带的结构趋于复杂化,从而在近代的断层活动中容易形成运动的阻抗,是应力易于积累和发生地震的场所。

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