斷層地壘 的英文怎麼說
中文拼音 [duàncéngdelěi]
斷層地壘
英文
fault horst-
It is the regional structure stress field formed in the processes of formation of the major faults of buried hills action on the graben that controlled the development of the fractures of sandstone of mesozoic of baigezhuang region
正是壘塊上古潛山內幕主要斷層形成過程中的局部構造應力場，控制形成了柏各莊地區潛山中生界砂泥巖中裂縫的發育。The regional structure interpretation with 3d seismic data shows that the graben and shied mode faults of the baigezhuang, which developed a series of normal faults which stroked in ne ( nee ) and dipped nw or nw, came into being in the rift development stage of ii act of the bohai bay rift basin in mesozoic and cenozoic and resulted from the protrudent boundary of the basin, i. e. the strike - slip and stretch processes of baigezhuang fault
同時，用三維地震資料進行區域構造解釋分析，論述了柏各莊地區的構造樣式，是中新生代渤海灣裂谷盆地的幕斷陷發育階段，同時由於盆地內凸起邊界?柏各莊斷層的走滑兼伸展作用，使柏各莊凸起的中生界形成壘、塹斷塊群構造樣式，發育一系列ne （ nee ）向，傾向nw或sw的正斷層。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造劃分為三層結構：即潛山內幕逆沖斷塊、古地貌殘山與低地和翹傾地壘塊。
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