tectogenesis

Mineralization period experienced three major evolutionary stages : sedimentary stage , tectogenesis period and the relatively stable tectonic movement stage .

成矿期大体经历了沉积阶段、构造运动阶段和构造运动相对稳定阶段三个时期。

New recognition on the Mesozoic tectogenesis in South-Anhui

皖南中生代构造运动新认识

Present Tectogenesis and Characteristics of Crustal Stress Field in Datong Basin

大同盆地现今构造活动及地壳应力场特征

The main factors that control reservoirs include deposition , diagenesis and tectogenesis .

影响储层储渗性的主要因素包括沉积作用、成岩作用及构造作用。

The effect of tectogenesis on endogenetic mineralization process of gold

构造作用对内生金矿形成过程的影响

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。

The tectogenesis in the Quaternary period of the Dongting Basin

洞庭盆地的第四纪构造活动

Since Neogene period , oil-gas reservoirs was readjusted and destroyed due to tectogenesis .

新近纪以来主要是已形成的油气藏重新调整和破坏时期。

Polycyclic tectogenesis and plate movement of Xinjiang

新疆多旋回构造与板块运动

Effected factors are the volcanic lithofacies , weathering crust , secondary alteration , volcanic rock and tectogenesis .

影响储层物性的因素有火山岩相、风化壳、次生蚀变、火山岩岩性、构造运动等。

It is showed that the control factors are lithology and lithologic association , diagenesis , weathering , and tectogenesis .

研究发现：静北潜山基岩储集层的主要控制因素有岩性及岩性组合、成岩作用、风化作用及构造作用等；

Tectogenesis , especially tectonic metamorphism is more important to the formation of the migmatite & metamorphics zone .

构造活动，尤其是构造变质对变质&混合岩带的形成起了相当重要的作用。

It has shown that they can be used neither for appreciation of equilibrium state of the earth , nor for the explanation of tectogenesis .

业已证明，这些模型既不能用以正确评估地球的平衡状态，也不能用以解释构造成因。

The dominant agent of the slope break is tectogenesis , and the scale of slope breaks relates with the size of tectogenesis .

构造运动是坡折带发育的主控因素，而且其规模与构造运动大小息息相关。

The second order tectonic sequence is thought to be the cause of making the variations of stratum sequence resulted from the secondary tectogenesis during certain tectonic phase .

二级构造层序揭示了大的构造幕中次一级构造作用（如构造沉降）所引起的充填地层层序变化序列。

The tectogenesis in Liaohe Basin

辽河盆地的构造运动

Overall , the frequently fluctuated lacustrine conditions and the surrounding tectogenesis are mainly responsible for the greatly varied form , different genesis of stromatolites .

柴达木盆地频繁变化的湖相水体条件和周围的构造运动是叠层石形态多样，成因各异的主要外部和环境因素。

Because the tectogenesis was not harmonious , the vertical diamictic continental shelf deposit system in the center and west of Tarim Basin was different from the transverse one .

由于构造运动的不均衡，中西部的混积陆棚沉积体系无论在纵向和横向上都有很大变化。

By means of studying the controlling factor of carbonate reservoir of Lower Permian in this district , these reservoir are ultimate outcomes of interaction by deposition and diagenesis and tectogenesis .

通过对区内下二叠统储层控制因素的研究，认为该储层是在数亿年的地质历史中，由沉积、成岩和构造作用相互影响而形成的最终结果。

Tectogenesis and volcanism and the basin evolution of the Mesozoic era in the northeast of Jiyang depression geological features of Mesozoic sags in the eastern part of Pearl River Mouth Basin

济阳坳陷东北部中生代构造运动和火山活动及盆地演化珠江口盆地东部中生代凹陷地质特征

Therefore , by virtue of finite element method , the idea , which can take rock gravity , tectogenesis and landform denudation into account , to get initial earth stress field of rock mass was presented .

以有限元数值分析为基本手段，提出了可以考虑构造运动、岩体自重和地形剥蚀等多因素的岩体初始地应力场反演思路。

The stress field of Neozoic tectogenesis stands in the dextrorotatory slippery tensile situation in the east of Eurasia . The geodynamical factors include plate movement and the motion of matter in mantle ;

欧亚大陆东部新生代区域构造运动总体处于右旋走滑拉张环境，其动力因素包括板块运动和地幔物质运动；

At the both side of the gravitational gradient zone of Daxing'an Mountain-Taihang Mountain-Wuling Mountain , the basin has different geophysical characteristics , which is connected with the course of the tectogenesis and the isostatic adjustment .

以大兴安岭太行山武陵山重力梯级带为界，两侧盆地具有不同的地球物理特征，这些特征与构造运动、均衡调整过程有关。

Under the influence of regional tectogenesis , the salt body underwent three times of plastic fluxion in geological history . The first time was in the late stage of Early Permian , the salt flowed 2 ~ 2.8 km southwards ;

受区域性构造运动的影响，盐体在地史时期曾经历了三次较为明显的塑性流动：第一次发生在早二叠世末期，表现为盐体向南流动了2～2－8km；

The structure of basement is composed of one group of East-west trending or similarly East-west trending anticline , syncline and fracture zones , and the mine is controlled by tectogenesis and distributed as East-West belt-shaped .

基底构造由一组东西向或近东西向的背斜、向斜和断裂带构成，矿床受构造控制，呈东西带状分布。