查询词典 tectonic force

Methods According to compaction correction model and Airy isostasy hypothesis, backstripping methode can be used easily to calculate the total subsidence and tectonic subsidence of the two sags.

利用回剥技术，根据压实校正模型和艾利均衡模型对两凹陷的总沉降量及构造沉降量进行求取。

Except for Tibetan Plateau and its surrounding regions, the results derived from lithospheric isostasy model are closer to observed elevations and consistent with vertical velocities of crustal movement in most tectonic units.

通过对均衡状态分析，我们得到以下主要结论：(1)构造稳定地区均衡程度较高；(2)青藏高原及周边造山带现今地壳运动主要为区域构造过程及深部动力学过程所控制，均衡调整过程不是主要控制因素；(3)现今地壳垂直运动比较明显的块体处于均衡调整阶段，地表垂直运动的大小反映了该区所受的均衡力作用的程度；(4)构造稳定地区基于岩石层均衡的理论计算海拔与观测海拔之差值和现今地壳垂直运动速率有较好的相关性，据此我们可以通过均衡分析研究构造块体的运动趋势和动力学性质；(5)地慢热结构对现今地形、海拔及地壳垂直运动有显著影响，在处理均衡问题时，地慢岩石圈热结构是我们必须考虑的重要因素。

In central Himalaya, massif was mainly uplifted in the tectonic model of channel flow during 17~7 Ma at a velocity of ~2 mm/a, then was extruded to earth surface at a much lower velocity. In eastern Himalaya Syntaxis, massif was mainly uplifted in the structural style of titling at a background of isostasy since 4.0~2.2 Ma.

喜马拉雅中段主要在17~7 Ma前以通道流的方式快速隆升，之后的抬升过程相对缓慢；东喜马拉雅构造结则主要在3 Ma以来，以地壳均衡作用为背景的掀斜式抬升为主要隆升模式。

Geotherm ; gravity anomaly ; isostasy ; tectonic movement

地热；重力异常；地壳均衡；构造运动

Tectonic activities and volcanism in the basin have an influence on hydrocarbon generation of kerogen and its change.

盆地构造活动和火山作用可以促进干酪根的成烃转化。

Tectonic deformation exists subsection longitudinally, different belt latitudinally and incoordination vertically.

构造变形呈现横向上的分段性、纵向上的分带性和垂向上的不协调性。

The Changning-Menglian belt located in western Yunnan of the Sanjiang fold belt in the Himalayan tectonic region of the Tethys is one of the important areas of studing and resolving many significant geological problems, like the nature、scale、 geological evolution、and ore-forming process of the paleo-Tethys and the boundary between Gondwana and Laurasia、etc., It has been always drawn close attention of geologists.

昌宁-孟连带位于特提斯喜玛拉雅构造域三江褶皱带，是研究和解决古特提斯性质、规模及地质演化、成矿作用及冈瓦纳与劳亚古陆分界等重大地质问题的重要地区之一，历来为地质学家所关注和研究。故滇西古特提斯昌宁-孟连带沉积地质研究对解决上述问题有着十分重要的意义。

Molybdenum deposits generally occur in nearly E-W direction along the tectonic lineament and are mostly concentrated in a zone stretching from Jinduicheng area of Shaanxi Province in the west to Nannihu-Sandaozhuang-Shangganggou area of Luanchuan and Leimenggou of Songxian in western Hena...

研究结果表明：除黄龙铺钼矿床形成于(221.5±0.3)Ma外，东秦岭地区钼矿床的大规模成矿主要出现在(144.8±2.1)~(132.4±2.0)Ma时限之间，对应的地球动力学背景为华北克拉通与扬子克拉通的碰撞造山后陆内造山局部伸展过程、中国东部地球动力学体制大转换晚期岩石圈拆沉及伸展时期。

The magma ofⅠ-⑥Concealed orebody experienced three stages:first,the deep liquation and pulsatory injection of the Cu- and PGE-rich magma; second,the concentration of tectonic activation;third,the later magma hydrothermal superposition.

探讨了来源于地幔深部的高镁玄武岩浆，在深部岩浆房和阶段岩浆房熔离分异时，富矿岩浆和矿浆之间存在富矿岩浆。

Finally, the controlling role of structure to sedimentary was analyzed. It is showing that time-transgressive different structural zone developed different sedimentary system; the thickness of sedimentary formation and lithic facies were different on the simultaneous lateral layer of growth fault; the expansive orientation of sedimentary system was controlled by the strike of fault; the sedimentary system developed differently became of the tectonic activity was differently; step thrust slip fault can built-up multistage fault fans.

最后分析构造对沉积的控制作用，主要表现在：不同时期不同的构造带发育不同的沉积体系；生长断层造成断层两侧同期地层沉积厚度与岩相的明显差异；断层的走向控制沉积体系的展布方向；构造活动导致沉积体系的发育有显著的差异；阶梯式逆冲断层可形成多级断崖扇。

These are places without aristocratic baggage; egalitarian places open to talent, self-improving, engaged in learning and innovation through networks that were at once competitive and cooperative.

这些地方没有贵族遗风作祟，而且对于那些有天分的人是开放的平等之地，这些人善于通过那些曾经很具有竞争力与合作精神的关系网进行自我提高以及学习创新。

Christine: You don't want to see me?

你不想见我？