Tectonic framework of north china block and its cratonization in the early precambrian 华北陆块基底构造格局及早期大陆克拉通化过程
Thus the tectonic systems have controlled basement tectonics of weihe basin and geothermal resources 这些断裂带控制着渭河盆地的基底构造以及地热资源的展布。
The strata of the region are divided into two structural layers : the basement rock consisting of metamorphic rock and cover layer of mesozoic and neozoic sedimentary rock . 将本区的地层划分为两个构造层:既变质岩系构成的基底构造层;中生代、新生代的沉积岩系构成的盖层构造层。
It obviously controls the distribution of the basement stucture and , in addition , evidently governs the subsequent stratigraphic sedimentation , magmatic activity and , especially , the formation and distribution of the xicheng lead - zinc orefield 它不仅对基底构造的展布具有明显的控制作用,而且对其后的地层沉积、岩浆活动,特别是对西成铅锌矿田的形成和分布也具有明显的控制作用。
This thesis studies each structural layer ' s feature : ( 1 ) structural layer of basement : it is a paleozoic folded basement , whose tectonic deformation and magma intrusion is fiercely , and it is affected by the early hercynian tectonic movement and related to the underthrust and closure ( c1 ) of zhungaer ocean basin and the areal pressing of continents ( c2 - 3 ) ; ( 2 ) structural layer of permian : due to the regional extending and fault depression role in mid - hercynian , it occurred to the combinations of structure and magma in santanghu basin and it ' s periphery area , such as a - granite ' s stock , batholiths and diabase ' s dike . there are many fault depressions possible 按照不同构造层,研究了各构造层的构造特征:基底构造层:受早海西期构造作用的影响,与准噶尔洋盆俯冲闭合、而后陆-陆碰撞的区域挤压构造作用有关,为一构造变形和岩浆侵入活动强烈的古生代褶皱基底。二叠系构造层:受中海西区域性伸展断陷作用的影响,盆地及其周缘地区发育与伸展构造有关的构造-岩浆组合,如呈岩株、岩基状侵位的a型花岗岩以及呈岩墙状侵位的辉绿岩等。