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深部地质作用
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  deep geological process
     It is not only an important deep geological process of North China platform activation but also the concret embodiment of deep" de-rooting".
     它既是华北地台活化的重要深部地质作用,亦是深部“去根作用”的具体体现。
短句来源
     The second stage of cratonization (the stage of intraplate) is controlled by new tectonic process, and is mainly a deep geological process.
     第二阶段 (板内阶段 )则出现新的构造格局 ,深部地质作用的重要性也越来越增加了。
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  “深部地质作用”译为未确定词的双语例句
     The websterite plagioclase granulite xenoliths were found in Cenozoic basalt, which is the key to know the geological process in deep.
     新生代玄武岩中发现二辉斜长麻粒岩等深源包体,为研究区域深部地质作用过程提供了证据。
短句来源
     It is considered that there are different patterns of Mesozoic and Cenozoic Basins superimposing on underlying Palaeozoic Basins in Yangzi Region and thus there are different superimposition effects to the underlying Palaeozoic marine source rocks due to different extent of reconstruction of Palaeozoic Basins.
     从地壳的深部地质作用,讨论了扬子地区主要中、新生代原型盆地生成与发展的深部过程。 认为扬子地区中、新生代盆地对古生代盆地的叠加方式各有所不同,对盆地下伏古生界海相烃源岩所产生的叠加效果也因古生代盆地改造程度的不同而有所不同。
短句来源
     (2)The deep geological processes such as the tilting and subsiding of Moho discontinuity, large-scaled deepmagmatism and deep faulting are main controlling factors for uranium metallogenesis;
     (2)深部地质作用如莫霍面的起伏、深部大规模的岩浆活动和深断裂作用是铀成矿的重要控制因素;
短句来源
     New multi-disciplinary study indicates that the tectono-thermal evolution and deep processes in the Jiao-Liao-Ji orogenic belt are summarized as following. The early mantle-plume-related underplating at a range from 2. 53 to 2. 36 Ga led to the 2. 47-2. 33 Ga intrusion of alkaline granite and mafic dyke swarm, the rifting of the Jiao-Liao-Ji rift and the bi-modal volcanism.
     根据新近多学科研究成果,综合揭示出胶辽吉造山带古元古代的构造-热演化和深部地质作用过程如下:早期底侵可能与深部地幔柱相关,发生于2.53~2.36 Ga之间,导致2.47~2.33 Ga岩墙事件、胶辽吉裂谷带的形成和双峰式火山活动。
短句来源
     As an open system the crust-mantle transition layer is an important layer where materialand energy exchange between crust and mantle takes place.
     壳幔过渡层作为地壳深部地质作用的一个开放体系,是物质交换和能量转换的重要场所。
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     and tectonic movement.
     (3)与深部地质作用有关;
短句来源
     Geologic process of cosmic ray
     宇宙射线的地质作用
短句来源
     GEOLOGICAL PROCESSES OF GROUND WATER
     关于地下水地质作用
短句来源
     SOME MAKING HEADWAY OF THE RELATIONSHIP BETWEEN GRANITICAL PROTOLYTE AND DEPTH GEOLOGISM
     花岗岩类源岩与深部地质作用关系研究的若干进展
短句来源
     This shows that tectonic development is closely related to deep geologic processes
     表明大地构造演化与深部地质作用过程密切相关。
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This paper synthetically analyses the gravity field, magnetic field and seismie data in northern Xinjiang and geological-geophysical data in adjoining areas, and describes the features of deep geologic processes in the region. According to the thickness of the lithosphere, P-wave velocity in the upper mantle and crustal structure, this region can be divided into Altay, Junggar and Tianshan lithospheric blocks separated by deep fault zones, which correspond to diwa regions at different development periods (Altay...

This paper synthetically analyses the gravity field, magnetic field and seismie data in northern Xinjiang and geological-geophysical data in adjoining areas, and describes the features of deep geologic processes in the region. According to the thickness of the lithosphere, P-wave velocity in the upper mantle and crustal structure, this region can be divided into Altay, Junggar and Tianshan lithospheric blocks separated by deep fault zones, which correspond to diwa regions at different development periods (Altay Diwa Region, Junggar Diwa Region and Tianshan Diwa Region). This shows that tectonic development is closely related to deep geologic processes

本文综合分析了新疆北部重力场、磁场及地震等资料和邻区地质-地球物理资料,研究了新疆北部地质作用特征。依据岩石圈厚度,上地幔纵波速度和地壳结构等特征,将研究区分为阿尔泰、准噶尔、天山3个岩石圈块体,其间为深断裂带所分割;它们分别与不同发展期的地洼区(阿尔泰地洼区、准噶尔地洼区和天山地洼区)相对应。表明大地构造演化与深部地质作用过程密切相关。

In this paper the author comprehensively analyses the features of the landsat imagery, the data of the geomorphology and hydrology,the gcophysic fields,the scismic activities and the Cenozoic volcaniactivity,and points out that there are several main NW trending structural zones in the east China.The NW trending linear structures,whose main active stages are in Cenozoic period, basically control the Cenozoic volcanic activities,the sedimetarty basins and the seismic acrivities,and can be classified into two...

In this paper the author comprehensively analyses the features of the landsat imagery, the data of the geomorphology and hydrology,the gcophysic fields,the scismic activities and the Cenozoic volcaniactivity,and points out that there are several main NW trending structural zones in the east China.The NW trending linear structures,whose main active stages are in Cenozoic period, basically control the Cenozoic volcanic activities,the sedimetarty basins and the seismic acrivities,and can be classified into two types according to their development and stress nature.One is the inherited shear-tension type and the other is the neogenic shear-compression type, whose original mechanism is related closely to the lithospheric stress state in the east China.The formation and development of the NW trending structures are controlled by the lithospheric deep geologic process.

本文综合分析了中国东部的卫星影象特征,并根据地貌、地球物理场、地震活动及火山活动等资料,确定了中国东部存在几条大型的北西向线性构造带。这些北西向线性构造带主要活动期在新生代,并对新生代的火山活动、沉积盆地及现代地震活动起主要控制作用。根据其演化史和力学性质可分为两种类型:继承性的张剪型和新生的压剪型。它们的成因机制与区域岩石圈的应力状态是一致的。因而,中国东部北西向线性构造的形成演化是岩石圈深部地质作用过程的必然产物。

During the recent years several series of phase equilibrium experiments on spinel, garnet therzolites have been done to calibrate the geothermobarometers, which are of critical importance for constructing T-p-fo2 regime of the upper mantle, and for understanding the mantle's magmatic processes. This paper gives a review to these thermodynamical methods, with particularly emphases on the T-p-composition limitations of the methods and the petro-genetical interpretations in practical applications.

上地幔的温压条件与氧化状态,对于了解上地幔的热结构、物态与相关系、深部地质作用、特别是岩浆起源及超镁铁岩的成因具有重要的意义。本文概述了近年来新提出的估算尖晶石、石榴石二辉橄榄岩相矿物平衡的温度、压力和氧逸度的热力学方法,对于从事金伯利岩、蛇绿岩和上地幔橄榄岩包体的研究具有重要的实用价值。

 
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