tectonic flow 中文意思是什麼
tectonic flow
解釋
構造流動-
To calculate this boundary parameter, mohorovicic discontinuity palaeo - heat flow value during basin evolution process is identified through geotectonic background analogy method based on " peeling " method model, and the basin basement palaeo - heat flow is calculated through inversion from today to antiquity with current tectonic structure as constraint condition for palaeo - crustal architecture analogy
為了求取這個邊界參數，以「剝層」法模型為基礎，通過大地構造背景類比法確定盆地演化過程中莫霍面古熱流值，以現今地殼結構為約束條件類比古地殼結構，從今至古反演求取了盆地基底的古熱流。 -
Main content in simulation is the spatio - temporal evolution of the set of descriptive variables characterizing tectonic mineralization state under coupling of various processes as following : ( 1 ) variables related to forming and property of ore - forming fluid, such as dissolution rate of minerals ( include metal minerals ) in rock, concentration and saturation of aqueous species in fluid, temperature, pressure, and ionic strength etc. ; ( 2 ) variables related to structural deformation and fluid flow, such as stress, deformation rate, fracture network, porosity, fracture permeability ; ( 3 ) variables related to precipitation and mineralization, such as nucleation rate of gangue and metal minerals, accumulation precipitation of various minerals, etc. ; ( 4 ) spatio - temporal coupling relation of various variables above, such as the coupling relationship between spatio - temporal evolution of fracture permeability and flow and focus of fluid and ore - forming
模擬的主要內容是在各種過程耦合作用下，以下描述構造成礦體系的主要變量的時空演化：與成礦流體的形成和性質有關的變量，如地層中礦物（包括成礦物質）的溶解速率、流體中各組分的濃度與飽和度、流體溫度、壓力、離子強度等；與構造變形和流體運移有關的各變量，如應力與變形速率、巖石孔隙度、構造（斷裂）滲透率等；與沉澱成礦有關的變量，如礦物（金屬礦物和脈石礦物）的成核速率、各礦物的沉澱量等；上述各有關變量間的時空耦合關系，如斷裂滲透率時空演化與流體流動、匯聚和成礦的耦合關系等。 -
According to the distribution of the fracture zones and the surface layers, the dazhaigou - haizigou valley can be divided into two first - grade and three second - grade tectonic areas, which greatly affect the landform pattern and surface material movement, and thus influence profoundly the formation and growth of debris flow
根據區內斷層展布格局和地層出露情況將該區分為兩個一級構造區和三個二級構造區，這三個構造區制約著地貌格局和地表物質遷移，進而對泥石流的形成和發展產生深刻影響。 -
By using the computerized dynamic modeling, the authors show that some quickly subsiding stages were involved in the process of basin formation, and the heat flow value generally varied from low to high as a whole, despite the fact that it may show alternatively increasing and decreasing trends at different stages, which demonstrates that the tectonic movement affected the heat flow value significantly
通過計算機技術的動態模擬，表明該區盆地演化過程中存在多個快速沈降期；其古熱流總體上由低到高變化，但在不同的演化階段表現不同，有升高也有降低，同時也反映了構造運動對熱流變化的影響。 -
Based on the analysis of distribution of upper jurassic and lower cretaceous strata and basin - controlled faults, tanlu fault zone strike slip to develop the three nw - trending grabens from north to south western to tanlu fault zone in late jurassic and early cretaceous, which are bohai graben, jiyang graben and luxinan graben. based on the analysis of regional geology, the basic tectonic pattern of bohai basin is the cenozoic basin pattern since early paleogene. the outline, structure, deposit characteristics and heat flow distributions show that the basin is pull - apart basin in cenozoic time. the tectonic evolution pattern can be reconstructed based on the analysis of cenozoic strata, deposit thickness, location and activity of basin - controlled faults in the different depresses in bohai basin. the characteristics of structure and depositment in this mesozoic and cenozoic time show that bohai basin is a mesozoic and cenozoic composite basin
根據中生界上侏羅統和下白堊統地層和控盆斷裂分佈分析，中生代晚期晚侏羅早白堊世郯廬斷裂帶的左旋走滑平移導致郯廬斷裂帶以西自北向南發育了3個北西向斷塹系，即北部的渤海斷塹系中部的濟陽斷塹系和南部的魯西南斷塹系。從區域資料綜合分析，渤海灣盆地的基本格局是早第三紀以來的新生代盆地格局。渤海灣盆地的形態構造和沉積特徵及熱流值分佈表明該盆地在新生代為拉分盆地。 -
Kinematic models have predominance in predicting heat flow but weakness in simulating basin geometry ; kinematic - rheological models are adept in tectonic modeling, but identical with kinematic models in heat flow prediction ; dynamic models contain latent advantages and also some obstacles in tectono - thermal modeling
運動學模型在預測盆地熱流演化方面具有優勢，但在預測構造沉降等幾何形態方面存在一定的缺陷；運動學流變學模型的優勢在於構造演化模擬，在熱演化方面類似於運動學模型；動力學模型蘊含著潛在的巨大優勢，只是目前還存在一些阻礙因素。
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