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深部地质过程
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  deep geological process
     The features and distributions of some gold deposits in the crust of Qinling don't coincide with the process of crustal evolution, but are in close relationship with deep geological process,particularly mantle activity.
     秦岭地壳中一些金矿床其特征及分布与地壳演化过程不协调,而与深部地质过程,特别是地幔活动密切相关。
短句来源
     The discovery of lamproites in this area is of farreaching significance in diamond prospecting and in research on deep geological process of the Tarim Platform.
     该钾镁煌斑岩的发现对研究区金刚石找矿和深部地质过程研究均具深远意义。
短句来源
     The studied result from Liaohe basin shows the concentration of Hg in natural gas is mainly affected by tectonic properties of basin and deep geological process.
     对此进行的研究表明:天然气(尤其是油型气)中汞含量明显受盆地构造背景和深部地质过程的影响,与源岩母质类型没有明显相关性;
短句来源
     The features of origin of magmatic rocks have revealed that the lithosphere structure in the ar ea experienced a process from double continental crust to normal continental cru st in the Yan-shanian stage. The deep geological process was the continuation of underplati ng and delamination.
     岩浆岩成因特点揭示出本区的岩石圈结构在燕山期存在一个从双倍陆壳到正常陆壳的过程,深部地质过程则是底侵作用和拆沉作用的继续。
短句来源
     Through systematical research of early to middle Permian basic igneous rocks the tocus on the trace element and REE geochemistry, the deposition characteristics, the source of basic igneous rocks and the deep geological process of early to middle Permian Magmatism are put forward.
     通过对塔里木盆地早-中二叠世基性岩类的微量元素、稀土元素和沉积特征的分析,提出了盆地早-中二叠世基性岩类的物质来源和岩浆作用的深部地质过程
短句来源
  geological process
     The features and distributions of some gold deposits in the crust of Qinling don't coincide with the process of crustal evolution, but are in close relationship with deep geological process,particularly mantle activity.
     秦岭地壳中一些金矿床其特征及分布与地壳演化过程不协调,而与深部地质过程,特别是地幔活动密切相关。
短句来源
     The discovery of lamproites in this area is of farreaching significance in diamond prospecting and in research on deep geological process of the Tarim Platform.
     该钾镁煌斑岩的发现对研究区金刚石找矿和深部地质过程研究均具深远意义。
短句来源
     The studied result from Liaohe basin shows the concentration of Hg in natural gas is mainly affected by tectonic properties of basin and deep geological process.
     对此进行的研究表明:天然气(尤其是油型气)中汞含量明显受盆地构造背景和深部地质过程的影响,与源岩母质类型没有明显相关性;
短句来源
     The features of origin of magmatic rocks have revealed that the lithosphere structure in the ar ea experienced a process from double continental crust to normal continental cru st in the Yan-shanian stage. The deep geological process was the continuation of underplati ng and delamination.
     岩浆岩成因特点揭示出本区的岩石圈结构在燕山期存在一个从双倍陆壳到正常陆壳的过程,深部地质过程则是底侵作用和拆沉作用的继续。
短句来源
     Through systematical research of early to middle Permian basic igneous rocks the tocus on the trace element and REE geochemistry, the deposition characteristics, the source of basic igneous rocks and the deep geological process of early to middle Permian Magmatism are put forward.
     通过对塔里木盆地早-中二叠世基性岩类的微量元素、稀土元素和沉积特征的分析,提出了盆地早-中二叠世基性岩类的物质来源和岩浆作用的深部地质过程
短句来源
  “深部地质过程”译为未确定词的双语例句
     N (ton) ~t figure shows that there seemed to have two-stage underplated in the Paleoproterozoic, and their peak ages are 2.5-2.4Ga and around 2.1Ga, respectively.
     N(t_(DM))—t图解分析表明,胶辽地块古元古代深部地质过程经历了两幕岩浆底板垫托作用,峰值分别为2.5~2.4Ga和2.2Ga左右。
短句来源
     The N(t_(DM))-t relation shows that there are perhaps twice Paleoproterozoic underplatings. The peak t_(DM) ages of these two underplatings are 2.5~2.4Ga and around 2.1Ga, respectively.
     统计的N(t_(DM))-t图解分析表明,胶辽地块古元古代深部地质过程经历了两幕岩浆底板垫托作用,底侵时代的峰值分别为2.5~2.4Ga和2.2Ga左右。
短句来源
     The Hg contents in natural gas bear positive correlation with the 3He/ 4He ratio,indicating that Hg may be partly originated from deep earth degassing or be affected by deep geological action.
     天然气中汞含量与稀有气体3 He/ 4He比值具有明显的正相关关系 ,表明天然气中一部分汞可能是来自地球深部的挥发分或与深部地质过程有关。
短句来源
     All these processes are wellrelated to subduction of adjacent oceanic plate in Mesozoic-Cenozoic and the causingresults of lithospheric stretching and thinning.
     这些深部地质过程与中新生代以来中国东部受相邻板块俯冲并导致岩石圈伸展、减薄等过程密切相关。
短句来源
     Petrology and geochemistry of the Cenozoic basalts from Yangyuan of Hebei Province and Datong of Shanxi Province:Implications for the deep process in the western North China Craton
     河北阳原和山西大同新生代玄武岩的岩石地球化学特征:华北克拉通西部深部地质过程初探
短句来源
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  geological process
The problem considered simulates the geological process of sedimentation in a basin.
      
The river discharge is a continuous, relatively stable (in time) geological process, whose action is dictated by climatic conditions of the region under consideration.
      
Thus, the petromagnetic thermometry of metamorphic events in oceanic peridotites may provide significant progress in the understanding of the geological process accompanying the formation of the oceanic lithosphere in slowly spreading ocean ridges.
      
The experimental data presented here are of great importance to elucidating the geological process in the earth's interior.
      
The main factor of evolution of lineament is a long geological process of extension of the earth's crust which is a result of the expanding earth.
      
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Based on diatectical materialism the paper discusses some aspects of the epistmology and methodology in the current igneous petrology. It is emphasized that the maxist principles on the ideas of the interaction and interdependeney. System science and dissipative structure have also been applied to the current igneous petrology. This paper philosophically discusses physical processess of magmatism, Mantle—magma—C—H—O system, open magma system, magmatism—plate tectonics—super—mantle plume—global mineralization....

Based on diatectical materialism the paper discusses some aspects of the epistmology and methodology in the current igneous petrology. It is emphasized that the maxist principles on the ideas of the interaction and interdependeney. System science and dissipative structure have also been applied to the current igneous petrology. This paper philosophically discusses physical processess of magmatism, Mantle—magma—C—H—O system, open magma system, magmatism—plate tectonics—super—mantle plume—global mineralization.

本文以现代火成岩岩石学的概念为出发点,从哲学的角度讨论了现代火成岩岩石学的某些前沿课题。对岩浆作用的全面认识,不仅要研究其化学过程,还必须从物理过程去探索;地幔—岩浆—C—H一O系统的研究是深部地质研究的一个侧面,深部地质过程是地表及浅部地质现象的动力来源;超地幔热柱是板块运动和大规模岩浆活动的起因,大规模的岩浆活动及板块运动是超地幔热柱在地表或地壳浅部的直接表现;开放的岩浆体系的提出,丰富了现代火成岩岩石学的内容。

Nonlinear Metallogeny is resulted by applying the nonlinear science to metallogeny.The features and distributions of some gold deposits in the crust of Qinling don't coincide with the process of crustal evolution, but are in close relationship with deep geological process,particularly mantle activity.The formation of gold deposit in Qinling district is of nonlinearity. Two types of gold deposits in Qinling district can be distinguished by studying this nonlinear feature:(1)linear, which is derived from the...

Nonlinear Metallogeny is resulted by applying the nonlinear science to metallogeny.The features and distributions of some gold deposits in the crust of Qinling don't coincide with the process of crustal evolution, but are in close relationship with deep geological process,particularly mantle activity.The formation of gold deposit in Qinling district is of nonlinearity. Two types of gold deposits in Qinling district can be distinguished by studying this nonlinear feature:(1)linear, which is derived from the earth crust and controlled by the crustal evolution and (2)nonlinear,which is derived from the mantle and controlled by the mantle heterogeneity.

非线性科学应用于成矿学研究,导致了“非线性成矿学”的产生。秦岭地壳中一些金矿床其特征及分布与地壳演化过程不协调,而与深部地质过程,特别是地幔活动密切相关。详细研究秦岭区金矿床形成的非线性特点,区别出秦岭区两种类型的金矿,即源于地壳并受地壳演化控制的线性金矿和源于地幔并受地幔非均一性控制的非线性金矿。

The paper discusses factors constrainting the chemical and isotopicheterogeneity and complicated evolutionary history of Cenozoic upper mantle beneathEastern China. Several major factors are summarized which include partial melting ofmantle, mantle metasomatism and asthenopheric dirpiring. All these processes are wellrelated to subduction of adjacent oceanic plate in Mesozoic-Cenozoic and the causingresults of lithospheric stretching and thinning.

探讨了制约中国东部新生代上地幔物质组成不均一性和复杂多阶段演化史的主要因素。中国东部新生代上地幔物质组成特征主要为地幔部分熔融、地幔交代和软流圈底辟等作用所决定。这些深部地质过程与中新生代以来中国东部受相邻板块俯冲并导致岩石圈伸展、减薄等过程密切相关。

 
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