查询词典 orogenic

The southern orogenic system is composed of the central and western Qinling-Qilian-Kunlun and Songpan-Ganzi orogens from north to south, with the middle Qilian and Qaidam massifs.

北造山系以天山-兴安岭华力西造山系的西段为主体，向北接有阿尔泰-额尔古纳加里东造山系，间有准噶尔、伊犁等微地块。

The Zhangbaling tectonic belt is a part of the Dabie orogenic belt and an outcrop area of the mid-upper crust of the belt.

提要： 张八岭构造带是大别造山带的一部分，是造山带中上地壳出露地区。

Results of the study demonstrate that arsenic in the surface soil of Chengdu basin has approximately six kinds of sources, among which sedimentary series of post-Triassic, Jurassic and Cretaceous systems along Longmen orogenic belt and acid magmatic and basic-ultrabasic rocks in the area are three main sources.

研究结果表明：成都盆地浅层土壤中砷的来源有6种，其中龙门山一带晚三叠纪、侏罗纪、白里纪沉积岩系和酸性岩浆岩及基性岩、超基性岩是成都盆地浅层土壤的主要来源。

Tectonic analysis of Pre-Carboniferous metamorphic stratum and structural foliation dating have shown that The Qinling and its vicinities had happened an important regional tectonic event -Caledonian event, this event represents early paleozoic closure of the Qinling ocean basin and continent-continent obliquely diachronous collision, so we also could reconstruct Caledonian Qinling orogenic belt's basic tectonic framework.

对北秦岭地区前石炭纪变沉积—火山岩地层系统进行构造解析，以及构造面理定年数据表明，秦岭及邻区志留纪至早泥盆世经历了区域性的重大构造事件，相当于加里东事件，该事件代表了秦岭早古生代洋盆闭合、陆—陆碰撞造山的造山事件，并可恢复加里东古造山带的基本构造格局。

Based on analysises of characteristics of regional deformation and metamorphism as well as Carboniferous and Permian relict basins, think Qinling-Dabie orogenic belt might have undergone following Basin-mountain transformational process : the ocean basin developed in Silurian-early Paleozoic; ocean basin subduction began in Ordovician; Silurian-early Devonian continent-continent collision happened and the ocean basin disappeared; Carboniferous- Permian, with the strike-slip and pull-apart along the Shangdan fault, a series of small faulted basins formed on the north Qinling mountainous region composing of Pre-Carboniferous metamorphic stratum.

在解析区域变形变质特征，岩浆侵位的构造演化和北秦岭区石炭—二叠纪残余盆地分析基础上，认为秦岭—大别造山带现今的残余的加里东造山带，可能经历了震旦纪—早古生代洋盆发育，奥陶纪洋盆俯冲，志留纪—早泥盆世碰撞造山，洋盆消失，石炭—二叠纪沿商丹带走滑拉分断陷形成上叠于北秦岭加里东造山带之上的石炭—二叠纪沉积盆地的盆山转换过程。

Therefore, the initial uplift of the Himalayas during Miocene is interpreted to have trigged by gravitational collapse of the Himalayas-Yarlung Zangbo orogenic belt.

作为这个造山带的前缘，喜马拉雅山中段发生向南的推覆，这就是喜马拉雅山中段的推覆时间要远远滞后于印度和欧亚大陆的碰撞时间的原因。

This occurs because movement di rections on shallowly dipping structures are related to graviational collapse of the thickened orogenic pile rather than push transmitted from the subducting pl ate to the overriding plate.

在斑状变晶边缘上形成的、近乎垂直的叶理在基质中的方位可能在较大范围内变动，因为它们会在稍早期间形成的叶理再活化作用影响下发生转动或遭到破坏。

Only did few plutons related to iron deposits form at about early Permian(287Ma), showing post-orogenic setting.

少数与铁矿有关的花岗岩形成于早二叠世(287Ma)，为后造山伸展环境下岩浆侵入产物。

The study on structural pattern of plutons can reveal more information of regional deformation, provide us detailed information of structural evolution of orogenic belts, define the emplacement mechanism of plutons, and help to investigate the feedback relationship among magmatic activities, tectonism and deep processes.

岩体构造样式研究可以揭示更多的区域变形信息，可以提供造山带演化详细的构造演化信息，可以确定出岩体侵位机制，并进一步探讨岩浆活动与构造作用及深部过程之间的互反馈关系。研究花岗岩构造变形是花岗岩研究与大陆动力学研究的一个结合点。

By comparison of the deformation degree of these plutons with different time, the paper suggests that during 959-889Ma a sudden peak regional deformation was tacking place in the core of the Qinling orogenic belt, giving the evidence for the subduction of the plate tectonics.

通过不同时间岩体区域变形改造程度的对比，提出959～889Ma秦岭造山带核部发生过突发性峰期变形事件。这从构造变形角度佐证了板块俯冲作用的存在。

On the other hand, the more important thing is because the urban housing is a kind of heterogeneity products.

另一方面，更重要的是由于城市住房是一种异质性产品。

Climate histogram is the fall that collects place measure calm value, cent serves as cross axle for a few equal interval, the area that the frequency that the value appears according to place is accumulated and becomes will be determined inside each interval, discharge the graph that rise with post, also be called histogram.

气候直方图是将所收集的降水量测定值，分为几个相等的区间作为横轴，并将各区间内所测定值依所出现的次数累积而成的面积，用柱子排起来的图形，也叫做柱状图。