thrust faulting造句
例句與造句
- Bedding - plane thrust fault
順層沖斷層 - Thrusting is the main character , so it was named as left - slip oblique - thrusting fault
但總體以逆沖為主。因此，將其稱為左行斜沖斷裂構(gòu)造。 - Thrust faulting and folding are main structures in the south piedmont of tian shan , they are migrating southward to talimu basin
天山山前主要為逆沖?褶皺活動帶，該帶不斷向塔里木盆地方向遷移。 - This paper discussed thrust fault - tolerant control technology for zhishui auv , designed at harbin engineering university
本文主要以哈爾濱工程大學(xué)研制的“智水”型水下機器人為對象，探討水下機器人推力器容錯控制技術(shù)。 - Structural characteristics of inversion structure , fold association style , thrust fault zone upright strata developed belt shown in great profiles were also discussed
對剖面中反映的構(gòu)造反轉(zhuǎn)、褶皺組合樣式、逆沖斷裂帶、直立地層發(fā)育帶的構(gòu)造特征進行了探討。 - It's difficult to find thrust faulting in a sentence. 用thrust faulting造句挺難的
- Muir wood r . , 1984 . problems of estimating earthquake recurrence from geological investigation in thrust fault terrains . proc . int . comp . on seismic microzonation , ech - cheliff algerea . 1 , 147 - 159
國家地震局地質(zhì)研究所, 1994 .廣東第三核電廠沙環(huán)廠址設(shè)計基準地面運動確定 - 2 . it is the first time to divide the structure of qianmiqiao buried hills into three structural layers : buried hills thrust fault block , paleogeomorphic relict mountain and lowland , tilting horst block
2首次將千米橋潛山構(gòu)造劃分為三層結(jié)構(gòu)：即潛山內(nèi)幕逆沖斷塊、古地貌殘山與低地和翹傾地壘塊。 - Different tectonic style exists in the upper and lower layers of the yanshanian boundary . the lower layers takes on the tectonic style of thrust fault and nappel . the upper layers hi step positive fault
2 、盆地燕山期構(gòu)造界面上下不同構(gòu)造層具有完全不同的構(gòu)造樣式，構(gòu)造界面下伏構(gòu)造層呈現(xiàn)沖斷褶皺、推覆構(gòu)造樣式，構(gòu)造界面上覆構(gòu)造樣式為階梯狀正斷層，整體呈現(xiàn)“雙層”結(jié)構(gòu)型式。 - According to the spread of nappe and relation between the nappe and depression , oblique - thrust fault zone was divided into three parts in this paper : sertengshan , lvliangshan and xitieshan . ( 3 ) according to macroscopic characteristics of fault zone , cleavage characters of fault zone , drag folds , the reverse " s " fold in the footwall , positive flower structures and small left strike - slip fault , the kinematics characters of fault zone of sertengshan - xitieshan are concluded : thrusting in section , left - slip fault in plane and the strike - slip displacement increasing from the west to the east
( 3 )根據(jù)斷裂斷裂帶的宏觀特征、斷層帶劈理特征、斷裂帶附近的牽引褶皺和斷層下盤的平面反“ s ”型褶皺以及斷層上盤剖面正花狀構(gòu)造和平面左行小型平移斷層，認為賽什騰-錫鐵山斷裂帶運動學(xué)主要表現(xiàn)為剖面上的逆沖、平面上的左行走滑特點，并且走滑量具有自西向東增大之勢。 - Firstly , based on the basin prototype , the triassic and jurassic mudstone and coal , the main source rocks of the basin , did not develop better in baicheng sag than in the northern thrust belt including keyi structural belt ; secondly , because of the thrusting happened in late cenozoic , the triassic and jurassic source rocks reach to a high to over high maturity and thus generate gas or condensate oil mainly . thirdly , the thrust faults compelled the natural gas to migrate from the north to the south or from the deep to the shallow . as a result , the keyi structural belt and the eastern qiulitage structural belt enriched in natural gas because they were not only located on the migration routines of the natural gas , but also developed simultaneously when the gas migration happened
從盆地構(gòu)造史研究的角度認為庫車盆地的天然氣主要來源于北部山前沖斷帶： 1受原型盆地構(gòu)造格局的制約，三疊系侏羅系烴源巖發(fā)育的最有利位置不是在拜城凹陷，而是在克依構(gòu)造帶及其以北的北部山前沖斷帶2晚第三紀以來的逆沖推覆作用使得烴源巖提早進入高過成熟階段，并以產(chǎn)氣和凝析油為主3逆沖推覆作用所產(chǎn)生的北傾逆斷層控制天然氣自下而上自北而南運移，位于運移路線上的克依構(gòu)造帶和秋里塔格構(gòu)造帶的東段與烴源巖的排氣期匹配較好，從而使這些地區(qū)最富集天然氣。 - ( 6 ) the geological significance of oblique - thrusting fault of sertengshan - xitieshan was discussed in this paper . the oblique - thrusting effect of sertengshan - xitieshan is the result of the long distance effction of himalayan orogenic belt intracontinent subducting , which is of great theory significance for studying regional structural framwork , relations between basins and mountains and oblique - thrusting effect of large - scale fault zone or orogen in northern qaidam basin . moreover , the result is of guidance significance for the forecast of combination gas , distributing and formation of nappe metal deposit in northern qaidam basin
( 6 )論文探討了賽什騰? ?錫鐵山斜向逆沖推覆構(gòu)造的地質(zhì)意義，認為賽什騰-錫鐵山斷裂斜沖作用是印度板塊與歐亞板塊碰撞、會聚的遠程效應(yīng)的結(jié)果，該認識對于研究柴北緣區(qū)域構(gòu)造格局、盆山關(guān)系以及更大尺度的斷裂帶或造山帶的斜向逆沖作用具有理論意義，對柴達木北緣的油氣預(yù)測、推覆體金屬礦床的分布、形成具有指導(dǎo)意義。 - ( 5 ) according to the study on seismicic data , sedimentary characteristics , contact relations , incision relation of the faults and strata related to the folds which are associated with the faults , this paper reached the conclusions : the oblique - thrusting structure of sertengshan - xitieshan in northern qaidam basin was formed in middle jurassic and the left - thrusting fault zone was established in the late pliocene of neogene
( 5 )根據(jù)地震質(zhì)料、沉積特征、地層的沉積接觸關(guān)系、斷裂切割地層關(guān)系以及與斷裂相關(guān)的褶皺卷入地層的研究，認為柴達木盆地北緣的賽什騰? ?錫鐵山逆沖推覆構(gòu)造形成于中侏羅世，而左行逆沖斷裂帶定型于新第三紀上新世末。 - The direction of migration was in east and northeast . ( 3 ) this paper introduced the balanced section into the early reservoir description in the sidaogou structure for the first time , and gave a new viewpoint that the sidaogou structure was a fault - bend fold formed by two step thrust fault . the structural stress direction came from the northeast of the hami depression
首次將平衡剖面技術(shù)引入了四道溝構(gòu)造早期油藏描述的構(gòu)造研究之中，并首次提出四道溝構(gòu)造是?至少由兩個階梯狀斷層組成的后傾雙重構(gòu)造疊加的斷層轉(zhuǎn)折褶皺，構(gòu)造應(yīng)力方向應(yīng)大致源于北東方向。