fault-controlled basin 中文意思是什麼
fault-controlled basin
解釋
斷層控制的盆地-
Based on first - hand materials, five regional faults ( nandan - du ' an fault zone, nanpanjiang fault zone, youjiang fault zone, bama fault zone and xialei - lingma fault zone ) were analyzed systematically which controlled the structural framework of the whole area. through discussing their activity and controlling basin behavior in different stage, fault zones " expression forms, and the activity mechanism of different section in different stage
論文在豐富的野外第一手資料的基礎上，對控制全區構造格架的五條區域性斷裂（南丹?都安斷裂帶、南盤江斷裂帶、右江斷裂帶、巴馬斷裂帶和下雷?靈馬斷裂帶）進行了系統的分析，討論了它們的構造表現形式、不同時期斷裂的控盆作用，並探討了它們不同時期不同段落的運動學機制。 -
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。 -
The basin was controlled by both dabie orognic belt and tan - lu fault zone. the model of the basin is a complex type that was composed of foreland and strike - slipping flexure in this period
這一系列現象表明，郯廬斷裂帶起源於華北與華南板塊印支期的陸?陸碰撞中，以轉換斷層的型式出現。
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