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成矿构造的英文

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"成矿构造"怎么读用"成矿构造"造句

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  • metallotectonics

例句与用法

  • On dynamics of metallogenic geochemistry for gold deposits in the xiaoqinling area
    小秦岭地区金矿床成矿构造地球化学动力学研究
  • It needs a reasonable explanation for the relation between such similarity and the tectonic pulsation
    这种相似性与成矿构造脉动性的统一需要给予合理的解释。
  • The basic thinking on research of metallotectonics is mainly how to distinguish metallotectonic types , to understand metallotectonic texture and to build metallotectonic series
    鉴别成矿构造类型、了解成矿构造结构、建立成矿构造系列是成矿构造研究的基本思路。
  • The paper defines a set of metallotectonicses , which are interrelated together under a certain space - time domain and the same tectonic regine or some particalar geologic events , as metallotectonic series
    成矿构造系列指一定时空域中、同一构造体制下或某一特殊地质作用过程中形成的相互联系的一套成矿构造的总和。
  • Abstract : the paper defines a set of metallotectonicses , which are interrelated together under a certain space - time domain and the same tectonic regine or some particalar geologic events , as metallotectonic series
    文摘:成矿构造系列指一定时空域中、同一构造体制下或某一特殊地质作用过程中形成的相互联系的一套成矿构造的总和。
  • After three - year hardwork both in field and laboratory , the main advancement achieved is as following : 1 . according to the study of regional ore - forming structures , the author renewedly expatiated on the evolution history of ore - forming structures
    经过三年的野外地质调查和室内的综合研究工作,取得了如下进展: 1 、通过区域成矿构造分析,重新拟定并阐述了成矿构造演化史。
  • According to tectono - metallogenic setting in combination with main mineral distribution and metallogenic types and ore - forming epochs in this orogenic belt , the authors used the theory of metallogenic series to divide the deposits of the north qilian early palaeozoic convergent epicontinental cu , pd , zn , w ( mo ) , au , ophiolite metallogenic belt and the south qilian early palaeozoic epicontinental rifting cu , ni ( pt ) , cr , au , rare elements and pyrite metallogenic belt into six series
    文章依据成矿构造环境,结合区域主要矿种分布及其成矿类型和成矿时代等特徵,应用矿床成矿系列理论,将祁连造山带北祁连早古生代汇聚陆缘铜、铅、锌、钨(钼) 、金、蛇蚊石成矿带和南祁连早古生代陆缘裂解带铜、镍(铂族) 、铬、金、稀土、黄铁矿成矿带中的矿床划归为6个成矿系列。
  • Using the structural analytical method of physicochemical field of metallotectonics , the authors studied the structural characteristics of the metallotectonic stress field and of the ore - forming physicochemical field , and made a preliminary discussion on the corresponding - coupling relationship between the physicochemical field structure of metallotectectonics and the spatial location of gold orebodies as well as its ore - prospecting significance
    摘要采用成矿构造物理化学场结构分析方法,研究了河东金矿床的成矿构造应力场结构特徵和成矿物理化学场结构特徵,并对成矿构造物理化学场结构与金矿体空间定位的对应耦合关系及其找矿方向进行了初步探讨。
  • During the process of studying tectonic origin of gold - bearing breccia bodies in the shuangwang gold deposit , shanxi province , the author apply several modern tectonics theories , such as hydrofracturing , fluid dynamic breccia , tectonic pumping , deformation partitioning , embryonic fracture etc . the paper presents an kind of new model for the formation of hydrofracturing breccia - type metallotectonic , which is one of fracture - vein - breccia series metallotectonics concerning fluid , by deformation partitioning , embryonic fracture , hydrofracturing and rupture - healing
    本文所探讨的陕西双王含金角砾岩体的构造成因研究运用了水力压裂作用、流体动力角砾岩、流体泵吸作用、变形分解作用和雏形断裂理论等几个现代构造地质理论,提出了变形分解作用?雏形断裂作用?水力压裂作用?裂开愈合作用四位一体的水压角砾岩型咸矿构造模型,是与流体动力作用有关的裂隙?脉?角砾岩系成矿构造的一种新的模式。
  • The comparison study of the three belts indicates although they are distinct from each other all the three belts show many common features in the aspect of the metallogeny of large - rich vein uranium deposits , i . e : the important metallogenic areas are located above the old crystalline basement ; the paleo - rifting ( taphrogeny ) controls the development of the volcanic belt and at the same time it is favourable metallogenic tectonic environment ; the occurrence of uranium deposit does not depend on the lithology of volcanic rocks ; uranium metallogeny is obviously constrained by deep geologic processes and the connected fault - structural net is the necessary condition for the formation of large - rich uranium deposits
    对比研究表明,虽然它们各具特色,就脉型富大铀矿床成矿作用而言,它们又具有较多的共性:重要成矿区的火山喷发皆奠基在古老的结晶基底上;古裂谷(或裂陷)既控制了火山岩带的发育,又是有利的成矿构造背景;铀矿赋存对火山岩的岩性没有明显的选择性;铀成矿的深部控制作用明显;联通的构造网络系统是形成富大铀矿的必要条件。
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