地壳构造的

There is good correlation of the geophysical fields with strong earthquake distribution, especially the Bouguer gravity anomaly and the thickness of crust.

海域地球物理场，特别是布格重力异常、地壳厚度分布与强震构造带的空间分布关系的相关性较好。

The cause of formation is the new structure rising of the earth's crust and the erosion and denudation of the external force.

形成原因是地壳的新构造抬升与外力的侵蚀、剥蚀。

Geomorhopologic landscapes in Xinjiang provided important cules for the studies of tectonics and crustal evolution, glaciology and geocryology, mountain research and desert research, and so on, it is valuable for science research and popular science education.

新疆地质地貌景观为大地构造及地壳演化研究、冰川冻土和山地研究、沙漠研究等领域科学问题的探讨提供了重要线索，具有极高的科学研究价值和科普教育价值。

Its basement is composed of Mesoproterozoic greenstone and associated complex, with the tectonic characteristics of earlier crustal evolution.

研究表明，其基底由前中元古代绿岩及与之伴生的花岗质杂岩组成，它们具有地壳早期演化的地质构造特徵。

Northern Guangxi is an ideal region not only for research of Precambrian stratigraphy but also for ...

桂北是华南前寒武纪地层研究的理想地区之一，同时也是研究华南地壳演化和前寒武纪大地构造性质的最佳地区之一。

The structure of the crust and upper mantle is characterized by consistent variations with the sh...

盖层和结晶地壳的密度和磁性结构在垂直方向以及隆起和坳陷构造带间，都存在明显的不均一性。

Therefore, in Southwest China took place a flow of crustal materials toward the southeastern direction.

在地壳物质流动过程中，由于阻力的差异，可以表现出不同的构造活动性。

The epicontinental arc volcanics related to the Permo-Triassic activities suggest the subduction of the Jinshajiang oceanic crust,and the ocean-continent tectonic regime transformation and the northward accretion of continental crust.

与二叠纪和三叠纪活动陆缘有关的陆缘弧火山岩带反映金沙江洋壳发生消减、洋-陆构造体制转换和大陆地壳向北增生的过程。

Comprehensive study for rheology of continental crust and the upper mantle is the best approach to understand continental structure and beyond plate tectonics.

大陆地壳和上地幔流变学的综合研究是认识大陆构造最佳途径之一。

The result shows that the crustal deformation is changing a lot in NW China: the deepest Moho is beneath the conjuction of west Kunlun and Karakorum, about 90 km deep, the shallowest Moho is beneath Jayir mountain to the west of Karamay, about 35.5 km; the Moho depth in the western segments of Tien shan is deeper then the mindle and eastern segments; there are Moho offset beneath Altyn fault, central Tien Shan northern margin fault and so on.

结果表明：比起我国其他地区，西北地区莫霍面无论是埋深还是形态均变化最大，反映出受印度板块与欧亚板块碰撞影响，西北地区地壳整体变形强烈。莫霍面最深（约90 km）位于西昆仑与喀喇昆仑构造结合处，最浅处位于准噶尔盆地西缘的克拉玛依（约35.5 km），最深与最浅差约55km。在盆山结合部位及大型走滑断裂，如阿尔金断裂、中天山北缘断裂带等均存在莫霍面错断。

For a big chunk of credit-card losses; the number of filings (and thus charge-off rates) would be rising again, whether

年美国个人破产法的一个改动使得破产登记急速下降，而后引起了信用卡大规模的亏损。

Eph. 4:23 And that you be renewed in the spirit of your mind

弗四23 而在你们心思的灵里得以更新