tectonic subsidence 中文意思是什麼

tectonic subsidence 解釋
構造沉降作用
  • tectonic : adj. 1. 構造的；建築的。2. 【生物學】構造的。3. 【地質學；地理學】地殼構造上的，起因於地殼運動的。
  • subsidence : n. 1. 沉澱；沉下，陷下。2. 平靜，平息；減退，衰耗。
  1. It is believed that three northeast - striking dextral slip fault zones, i. e. the baxian - shulu - handan fault zone, the huanghua - dezhou - dongming fault zone, and the linyi - huanghekou fault zone, are the result of the tectonic transform of paleogene extending to neogene - quaternary laterally slipping of north china plain rift systems, which extend along the central axis of rifts and accord with the quaternary centers of subsidence as the main seismic structures within the rifts

    認為壩縣束鹿邯鄲斷裂帶、唐山河間磁縣斷裂帶和黃驊德州東明斷裂帶3條北東向右旋走滑斷裂帶為華北平原裂谷系從早第三紀伸展拉張作用進入晚第三紀第四紀走滑剪切拉張作用的產物，這3條斷裂帶分別位於3個北東向坳陷帶中部，並構成了第四紀沉降中心，與營口濰坊斷裂帶起構成華北平原內的主要強震構造。
  2. The tectonic subsidence curves on the southeastern margin of the yangtze plate are drawn out using of backstripping method for the basin formation and evolution. the basins located in the southern margin of the yangtze plate, in the basin dynamic computer simulation, is explored and constituted to be a typical foreland basin which is of not rather high mountain and thermal situation to be lower in this older orogeny belt

    在沉積盆地分析方面，基本查明揚子板塊東南邊緣早古生代被動大陸邊緣沉積特徵及沉積構造演化，同時運用反剝法技術對揚子板塊東南大陸邊緣沉積盆地形成，演化的構造沉降動力學進行探討，運用計算機模擬方法，定量動力沉積學對揚子東南邊緣奧陶紀到志留紀前陸地進行計算機模擬分析，探索並建立這個古老造山帶前陸盆定量參數和動態定量模擬。
  3. One of the frontier recearch of basin analysis in recent years is to analyze the tectonic subsidence history of depositional basins which occur in orogens at different geohistory stage, and to discuss the geodynamic processes involved with the basins

    摘要對造山帶各地史階段的沉積盆地進行構造沉降分析，進而探討其地球動力學過程，是近年來盆地分析的前緣研究之一。
  4. Because of the collision of the terranes, the episodic tectonic activity occurred in the orogenic belt, resulting in the episodic subsidence of the basin

    受地體碰撞的影響，盆地西緣造山帶發生幕式構造運動，從而導致盆地沉降也發生幕式變化。
  5. Compared to the basins in east guangxi, the basin of north guangxi is characterized by lower depositional and tectonic subsidence rate during rifting, longer thermal subsidence, later inflexion point from rifting to foreland buckling, as well as later inflexion point separating stable stage from active stage during foreland - buckling

    但與桂東大瑤山地區相比，桂北興安地區在裂陷階段的沉積速率和構造沉降速率明顯偏低；熱沉降階段的持續時間偏長；裂陷階段與前陸撓曲階段的分界拐點偏晚；前陸撓曲階段，由構造寧靜期的緩慢沉降向構造活動期的快速沉降轉化的分界拐點也偏晚。
  6. The general structure of the basin is marked by the tectonic framework of compressional ramp of the east kunlun mountains and the qilian mountains toward and subsidence of the central part of the basin

    盆地的總體結構表現為東昆侖山和祁連山相向向盆地擠壓對沖，盆地中部沉降的構造格局。
  7. The formation and evolution of the sequence stratigraphy of the yanchang formation are governed by slow tectonic subsidence, warm humid climates, sediment supply and lake - level fluctuations

    延長組層序地層的形成與演化主要受控于當時緩慢的構造沉降、溫濕氣候、陸源碎屑物源供給及湖平面升降等地質因素。
  8. The different subsidence history not only demonstrates that the two areas have different tectonic settings, but also proves that the caledonian basin migrated to northwest when the cathaysian plate was gradually subducted toward yangtze plate from southeast to northwest

    這些差別這一方面說明了兩地區具有不同的構造背景，另一方面也反映了華夏板塊由南東逐漸地向北西揚子板塊靠攏，沉積盆地相應地向西北遷移的動力學過程。
  9. Bozhong area has different oil - gas accumulation characteristics from the adjace nt onshore oil fields. because of the latter thermal event and tectonic action, bo zhong area became the subsidence center and depo - center of the bohai bay basin

    其具有不同於周邊陸地油田的油氣成藏特點，晚期的熱沉降和構造活動使其成為渤海灣盆地的沉降和沉積中心，上第三系具有優于周邊陸地油田的良好的儲蓋條件，晚期的構造活動與油氣主要排烴期相匹配，為油氣向上第三系圈閉中運聚提供了良好條件。
  10. 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

    第四紀受強烈擠壓快速沉降接受陸相磨拉石沉積。自新第三紀以來，受帕米爾西昆侖北移和隆升沖斷的影響，塔西南和塔吉克盆地發生了復雜的褶皺沖斷變形，其差異在於塔西南明顯地受走滑為主的剪壓構造作用，而塔吉克盆地是受擠壓為主的剪壓構造作用的影響。塔西南和塔吉克盆地下第三系巖相組合類似，後期構造變形也相似，塔吉克盆地下第三系是該盆地的主力油層，已有許多油氣田發現，因此可以推斷塔西南也應該有良好的油氣前景。
  11. The formation and evolution of sequence stratigraphy of middle - upper jurassic series is affected by change of global sea level, tectonic uplift and subsidence, sedimentary supply and climate conditions

    中?上侏羅統層序地層的形成演化受全球海平面變化、構造隆升與沉降、沉積物供給以及氣候條件的綜合影響。
  12. Depending on the data of the new oil and gas resources survey, the subsidence history and structural evolution of north yellow sea basin are emphatically analyzed in this paper based on the brief discussion on the characteristics of tectonic geology of north yellow sea basin

    摘要依據最新油氣資源調查資料，在簡述北黃海盆地區域構造特徵的基礎上，重點分析了盆地的沉降史與構造演化特徵。
  13. There is a close relation between the tectonic subsidence and the heat how in basins

    摘要盆地的構造沈降和熱流演化具有密切的聯系。
  14. The tectonic movement controls different types of sequences by controlling subsidence of basement and sediment supply rate

    構造運動通過控制基底的沉降幅度和物源供給速度控制層序類型。
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