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tectonics相关的网络例句

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与 tectonics 相关的网络例句 [注:此内容来源于网络,仅供参考]

With the rapid development of satellite observations, we can use the altimetry geoid to study submarine tectonics and geodynamics.

由于卫星观测技术的发展,现在已能利用测高大地水准面简捷可靠地研究海底构造与动力问题。

Photo Gallery: Plate Tectonics The Sheep Mountain anticline in Bighorn Basin, Wyoming, is part of the Rocky Mountains.

意译:板块构造的图片。羊山区背斜在洛矶山羊盆地,怀俄明州,是一部分的洛矶山脉。

Photo Gallery: Plate Tectonics Raplee Ridge, part of the Monument Upwarp in southeastern Utah, is a long, narrow, folded anticline that formed about 70 million to 50 million years ago.

意译:板块构造的图片。Raplee岭的一部分,纪念碑upwarp在犹他州东南部,是一项长期的,狭隘的,折叠背斜,形成约7000万至5000万年前。

HUANG Jiqing gave a brilliant exposition with E. Argand's mobilism thought as to the dynamical evolution process of the tectonics in On Major Tectonic Forms of China.

在《中国主要地质构造单位》中,他运用阿尔冈活动论的思想,阐述了中国大地构造的动力演化过程。

Palaeogeomorphology is a main factor to control the development and distributing of the sedimentary facies like the geomorphology today which is affected by the factors such as the location of the area tectonics, weather, the change of the datum plane and the tectonics movements.

古地形地貌是控制一个盆地后期沉积相发育与分布的一个主要因素,同现在地貌一样,古地貌形态受到了所处的区域构造位置、气候、基准面变化及构造运动等因素综合作用的影响。

In the evolution process, the relationship between the recently forming tectonics framework and the pre-exist tectonic framework is succession, development, modification, destruction and the superpose of new tectonics.

在发展演化过程中,既有对先存构造的继承、发展、改造和破坏,也有新构造的叠加。

Firstly, based on the distribution of global earthquakes and their kinematic and dynamic characteristics, the most active global-scale tectonics can be divided into three first-order tectonic system: the circum-Pacific deep subduction tectonic system, which is the region that oceanic lithosphere subduct under continental lithosphere; the mid-oceanic ridge tectonic system, where the joint tectonics of rift valleys and transform faults distribute widely; and the continent-continent shallow underthrusting tectonic system, where the different kinds of continental faults affect each other.

其中,环太平洋构造系以大洋岩石圈向大陆岩石圈俯冲为构造特征;大洋中脊构造系以大洋岩石圈内裂谷-转换断层的组合构造为特征;大陆构造系则以大陆岩石圈的边缘和内部各种断裂的相互作用为特征。

Which of the following can be inferred about the theory of plate tectonics? It is no longer of great interest to geologists. It was first proposed in the 1960's. It fails to explain why earthquakes occur. It refutes the theory of the existence of a supercontinent.

解析:根据原文末段末句,在1960's以前地质学家没有办法解释,而在之后tectonics理论给出了解释,于是可以推断这个理论在1960年推出,典型的"取非"细节推断题。

The influence on oil and gas,combination types, tectonic origin mechanism ,orogenic zone thrust-nappe tectonics and benching thrust-nappe tectonics are summaried in this paper.

本文概述了逆冲推覆构造对油气的影响,组合类型,构造成因机制,造山带逆冲推覆构造和台阶式逆冲推覆构造。

We have concluded five key tectonics geologic characteristics of Chinese foreland basins based on the study of the sedimentary infill, tectonics evolution, tectonic dynamics, spatial location distribution and structural deformation geometry.(1) The foreland basin is the superimposition of the compression sedimentary stratigraphic sequence with the extension basin, and the foreland basin includes underlying rift basin and upper dustpan flexure deposited basin.(2) The foreland thrustfold structural deformation has occurred four times since the Protozoic, in the Late Caledonian, Late Hercynian, Indosinan and Late Himalayan, respectively.(3) The foreland basin developed based on the control of two factors that are the basin basement collaged by many small plates or terrains and the rejuvenation of ancient orogenic belt, so the foreland basins or foreland thrusts are located in front of ancient orogenic belt.(4) The foreland basins and the rejuvenation of ancient orogenic belt make up a giant basinmountains system resulting from the distant effect of IndiaEurasia collision, which is located on the outer circle of Tibet Plateau, so the thrust deformation intensity, basin deposition range and coupling between orogenic belt and basin changed from strong to weak as from interior to outer circle of Tibet Plateau.(5) There are many structural styles of the thrust and fold belt in different basins, such as brittle behavior faultrelated fold, ductile behavior basementinvolved structure, basementinvolved faultrelated fold, and salt structure.

在综述前人认识的基础上,笔者通过对中国前陆盆地的构造演化历程、沉积充填特征、构造成因及其空间分布规律、构造变形特征等的研究,提出了中国前陆盆地构造地质发育的5个主要特征:(1)两种不同性质的原型盆地发生正反转的叠合性,即挤压构造下作为&本体&的前陆层序与拉张构造下作为&基础&的裂谷、断陷盆地之间的叠置;(2)显生宙以来中国大陆先后发生了4期前陆冲断构造演化的多期性,它们分别是加里东晚期、海西晚期、印支期和喜马拉雅晚期;(3)基于小克拉通基底拼贴后在造山带前缘复活再生的继承性,即统一拼合大陆内部的构造变形导致古造山带的复活,在古造山带边缘发育新生代前陆盆地或前陆冲断带;(4)在空间分布上受环青藏高原巨型盆山体系控制发生陆内变形的系统性,在环青藏高原巨型盆山体系内构造变形强度、盆地沉降幅度、盆山耦合程度等从内环向外环依次降低,从古造山带向克拉通方向构造变形强度依次降低,构造变形样式逐渐简单、构造变形时间依次变新;(5)前陆冲断带的构造样式由于受边界力学条件和沉积地层介质作用而具有多变性,存在沉积盖层内脆性变形的断层相关褶皱、造山带前缘韧性变形的基底卷入构造、与走滑构造相伴生的基底卷入的断层相关褶皱、盆地内部塑性变形的盐构造。

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