tectogenesis meaning in Chinese
大地构造成因
构造运动
构造作用
造山运动
Examples
- The main factors influenced fractures development are the tectogenesis , the physical weathering and the chemical dissolution
影响裂缝发育的主要因素是构造、物理风化和化学淋溶作用。 - Huge deep fractures in the east of china have a little influence on the pore of carbonatite reservoir of ? - o stratum in the regions of zhuangxi and chengdao . the karstification which probably happened at xishan tectogenesis period is also very limited
我国东部深大断裂对桩西、埋岛地区寒武一奥陶系碳酸盐岩的储层孔隙影响很小，可能发生在喜山期的岩溶作用(深部流体带来的岩溶作用)也是十分有限的。 - The mainly reservoirs in the middle of damintun depression of liaohe basin are the regional metamorphic rocks and the migmatites , which are more fractured and rigid by the cataclastics . the space of metamorphite is the mainly fractures , which are produced by the tectogenesis and the physical weathering
2 、辽河大民屯中部地区主要储集岩是太古界的区域变质岩和混合岩类，尤以裂缝发育和经过碎裂化的刚性变质岩类的储集性能最佳。 - This is the direct reason of bad reservoir property of sandstone , especially lower permeability . the influence and control factors of reservoirs include : deposition , diagenesis and tectogenesis . the deposition is the basic factor , it control the shape and distribution of sand body , and influence the type and the intensity of the diagenesis ; the diagenesis is the key factor , it control the process of pore evolvement , so the diagenesis control the sandstone ' s storage space and reservoir quality directly ; the fracture of the tectogenesis formation could improve the porosity and permeability of sandstone
其中沉积作用是基础，控制了储集砂体的形态特征和分布范围，同时由于不同沉积类型砂体在碎屑成分组成、泥质含量、颗粒粒度、砂体厚度、砂体内部的非均质性、孔隙介质的物理化学性质等方面不尽相同，从而也影响着砂岩所经历的成岩作用路径、类型和强度，因此沉积作用是控制储层发育的主导因素；成岩作用是关键，直接决定了砂岩的孔隙演化过程，从而决定了储层内部储集空间特征和储集性能；而构造作用形成的裂缝对改善砂岩的储渗性能具有一定作用。