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tectonic相关的网络例句

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与 tectonic 相关的网络例句 [注:此内容来源于网络,仅供参考]

That is to say, the research area has experienced two substages of tectonic movements, respectively, the later tectonic stress is supposed to be about 60Mpa, and that of the former is supposed to be higher than that of the later.

研究区经历了两次构造运动,其中晚海西期构造力应为60Mpa左右,而晚加里东~早海西期的构造应力应该大于晚海西期。

According to geometry and mechanical distortion principle, a computer simulation and visualization technique is developed, which uses 2D seismic interpretative profile, tectonic plan map, sedimentary facies map and well log sheet to generate 3D tectonic-stratigraphic framework of basin, and also to establish spatial information system of real 3D digital basin.

根据几何学和机械变形原理,在具有自主知识产权的GeoView三维可视化地学信息系统平台上,研发出了通过二维地震解释剖面图、构造平面图、沉积相平面图和钻井柱状图生成真三维盆地构造-地层格架的计算机模拟和可视化技术,以及建立三维数字盆地的空间信息系统技术。

As for the drive power, both of them have been driving by climatic and tectonic power under the dominant control of N-S tectonic compression.

二者抬升的驱动力则较为相似,都是南北向挤压作用下的气候驱动,即是构造控制下构造与气候的共同作用

The text analyse region characteristic and rule of gravity and magnetism annormity in Chaoshan depression,conclusion think that the Chaoshan depression is tectonic transition belt of join two tectonic element about the dongsha islands to the xisha islands, the fault of turning towards the basin control growth of the Mesozoic group.

本文分析了潮汕坳陷区域重力、磁异常特征及地震地质规律,提出潮汕坳陷是衔接东沙群岛和西沙群岛两个构造单元的构造过渡带的观点,同时盆倾断层控制了中生界发育与分布。

The area has undergone multi-phased tectonic events including deformation, magmatism, tectonic uplift and strike slip movement.

该区经历了多期造山运动和岩浆热事件,遭受了多期的抬升、走滑和变形作用。

The tectonic reconstruction of the continental masses in China during Cambrian time has been made on the basis of the palaeomagnetic data available and plate tectonic information.

笔者根据近年来所获的古地磁数据及板块构造的研究成果,对中国各大陆块在寒武纪全球构造中的位置进行了再造。

In this tectonic setting, the special sedimentary environment and regional magmatism as well as tectonic force are the main factors which control the regional metallogenesis .

活动陆缘区特殊的沉积环境、区域岩浆活动及构造变形动力等作用,构成了区域矿产形成的主要背景和控制因素,从而使不同类型和元素组成的矿床得以形成,并表现区域成矿的总体分带规律。

Then, a hypothesis of "double force source" for tectonism is put forward, its main points are: the tectonism is not only the result from the action of tectonic stress, but also the result from the action of "double force source", namely, the tectonic stress and subsurface fluid force including force produced by precipitation, etc.

提出了&双力源&构造变动假设,即构造变动不仅是构造应力作用的结果,而且是构造应力与地下流体力共同作用的结果;二者共同作用因方式不同而产生不同的构造变动;在构造变动孕育与产生过程中,构造应力的作用是第一位的,地下流体力则是调制性的,只有那些能与构造应力增强过程产生力学耦合的地下流体力,才能调制与诱发出构造变动异常并促进构造变动。

The result showed that tectonic movement history was a key factor in the deep weathering mantle formation. Tectonic movement influenced driving force and potential energy of Benggangs, and eroded history of each cracking block, which determined the depth of weathering mantle.

结果表明:构造活动历史是崩岗区形成深厚风化壳的主导因素;构造活动影响崩岗侵蚀动力势能以及各断块遭受侵蚀的历史;侵蚀动力势能和侵蚀历史确定了崩岗发育之前风化壳的厚度。

The results of the study indicate:(1) the stress, strain and velocity fields as well as the uplift rates of the model are consistent essentially with those of the prototype in nature;(2) the major driving force for intraplate tectonic deformation in central-eastern Asia results mainly from the compression of the Indian plate;(3) the existence of the RSBs, such as those of Tarim, Alxa, Ordos and Sichuan basin, is one of the basic origins for the development of large-scale compressional basins and the table-like uplift of the Qinghai-Tibet plateau;(4) The netlike plastic-flow in the lower lithosphere is faster than the displacement in the upper layer, controlling the tectonic stress and deformation fields in the upper crust;(5) the weakness layer distributed discontinuously in the middle crust influences the level of difference between the stress directions in the lower lithosphere and those in the seismogenic layer.

研究结果表明:(1)模型中的应力场、应变场、位移速度场和地表隆升速率,与自然条件下的实际状况基本相符;(2)中东亚板内构造变形的驱动力源主要来自印度板块的推挤作用;(3)塔里木、阿拉善、鄂尔多斯、四川盆地等相对稳定块体的存在是促成大型压性盆地形成和青藏高原平台式隆升的基本原因之一;(4)岩石圈下层的网状塑性流动超前于上层,控制上层的构造应力场和变形场;(5)中部地壳的非连续分布软弱层影响上、下层之间应力方向的差异程度。

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