block faulting 中文意思是什麼
block faulting
解釋
塊斷運動-
The author also suggested that the fuxin block developed on the base of the geosyncline in the huabei craton, and had experienced three period process of orogeny, including hercynian folding orogeny in continental margin, mainly indo - sinian to early yanshanian intracontinental fold - faulting orogeny, and late yanshanian to early himalayaian intracontinental range - basin post orogeny
認為阜新地塊是在克拉通裂陷槽基礎上發育起來的，經歷了海西期陸緣褶皺始造山、印支?早燕山陸內褶斷主造山、晚燕山?早喜馬拉雅陸內盆山後（重）造山等過程。 -
They are paleozoic ~ early mesozoic - fold deformation and the appearance of reversed fault ; mesozoic - the beginning of graben faulting - block period ; early cenozoic - the phase of broke - the forming of block hill ; late cenozoic - the phase of segging - the forming of buried hill. we mark off five kinds of buried hill belts. they include three different kinds of trap on the basis of the cause of trap formation
本次研究在重新認識濟陽坳陷區域構造背景的基礎上，將濟陽坳陷古生界潛山的形成過程分為四個階段，即古生代早中生代?穩定沉降?隆升?輕微褶皺變形及逆斷層發育階段、中生代?初步斷陷階段?塊斷期、新生代早期?斷拗階段?塊斷潛山形成期以及新生代晚期?坳陷階段?潛山定型期。 -
Block faulting tectonics
塊狀斷裂構造 -
Basement block faulting
基底塊斷作用 -
Relationship between the wrench structure in the north - margin block - faulting belt in the qaidam basin and altun tectonic system
柴達木盆地北緣塊斷帶的扭動構造與阿爾金構造體系的關系 -
Since late tertiary the neotectonic movement in the region has been being more intense, and the most obvious feature of the neotectonic movement was characterized by large - amplitude block - faulting and strong volcanic activity
晚第三紀以來，本區新構造運動比較強烈，最顯著的特徵是斷塊大幅度升降運動和強烈的火山活動。 -
Based on predecessors research by geological - geophysical synthesized studying and three - dimensional technique, draw up west, middle and east three composite profiles, explanation of the structure model in different level including surface, middle and deep of the basin, finally concluded in homogeneity of the basin is show by belting in south - north trend, block - faulting in east - west trend and vertical sphere - laying
在前人研究基礎上，採用地質-地球物理綜合研究和三維技術，編制了西、中、東部三條地學綜合剖面，研究解釋了盆地淺、中、深部不同層次的結構構造樣式，得出盆地地殼結構不均一性規律。
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