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岩浆作用的英文

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"岩浆作用"怎么读用"岩浆作用"造句

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  • magmatism

例句与用法

  • Characteristics of dulongjiang granite and magmatism in northwest yunnan
    滇西北独龙江花岗岩及岩浆作用特征
  • Magmatism and its tectonic significance in the manzhouli - e ergona region
    额尔古纳地区岩浆作用及其大地构造意义
  • Magmatic activities and its constraints on gold - silver mineralization in xiong ' ershan area , western henan province
    豫西熊耳山地区燕山期岩浆作用对金银成矿的制约因素
  • Given the fact that mesozoic magmatism was closely related to the lithospheric thinning , it is proposed that the diachronous lithospheric thinning is the main mechanism by which the taihangshan gravity lineament was formed
    由于岩浆作用与岩石圈减薄作用密切相关,因此认为华北岩石圈减薄的时空不均一性是形成太行山重力梯度带的重要机制。
  • After making detailed research on ore - controlling factors , the author points out that gold deposits in fujian resulted from the various geologic processes such as sedimentation , metamorphism , tectonism and magmatism
    详细研究了福建省金矿的金矿的控矿因素,提出省内金矿的形成是沉积作用、变质作用、构造作用和岩浆作用(包括火山作用)的综合结果。
  • It is presented that the hydrous fluxing as well as adiaba tic decompression plays an important role in melting of morb - like mantle beneath marina trough . compared with basalts from other back arc basins , it concludes that the magma varies from morb - like to arc - like with the evolution ; during the earlier stage of evolution , there coexist the two morb - like and arc - like lavas , it may be the nature of the magma in back arc basins ( especially in the earlier stage )
    综合马里亚纳海槽和其他弧后盆地玄武岩的研究成果发现,弧后盆地特别是早期扩张的弧后盆地,其岩浆产物均具从似岛弧型到似洋中脊型玄武岩的时空演化特征;同时存在岛弧型和morb型两种熔岩,可能是弧后盆地(特别是早期扩张弧后盆地)岩浆作用的一个共同属性。
  • The zijinshan fluid system and the gonglang fluid system were driven by the stress of extrusion nappe onto the basin and the thermal driving force of magmatism . when the fluids cycling in the basin encountered the boundary of reduction - oxidation or underwent fluid mixing , phase separating and fluid boiling caused by fault - induced pressure reducing , the physical chemistry condition abruptly changed and mineralization then took place
    在盆地两侧挤压推覆构造应力及岩浆作用热力驱动下,紫金山背斜和公郎弧两大流体系统的流体在盆地中运动,当遇到氧化还原界面或遭受流体混合、相分离及断裂导致的减压沸腾时,因物理化学条件发生重大变化而导致成矿作用的发生。
  • The control of the deep - seated structural - magmatic process over the metallogenic system around the middle - lower yangtze river reaches is shown as : ( 1 ) the mantle uplift belt is closely related to the general geological background of the metallogenic system ; ( 2 ) the primitive magma originated from different parts of the mantle uplift belt ( mantle ridge or mantle slope ) shows differences in style of formation and composition and results in different magmatic series and metallogenic subzones , respectively ; ( 3 ) the varying depths of structural - magmatic chambers may form a " three - layered structure " ( central type , network - like and ring - like ) and this is the primary factor that controls the different magmatic series and the concerned cluster of ore deposits ; ( 4 ) the alkaline basaltic magma derived from the mantle ridge forms high - potassium and calcium alkaline magma and shoshonitic magma due to its altering intensity of afc process with the lower crustal material , which has something to do with the copper - gold and iron - sulphur metallogenic subsystems , respectively
    深部构造岩浆作用对长江中下游成矿带安徽沿江地区成矿系统的控制表现为: ( 1 )地幔隆起带与成矿系统的总体地质背景的演变密切相关; ( 2 )源于地幔隆起带不同部位(幔脊与幔坡)的原始岩浆,其生成方式和物质组成不尽相同,它们分别产生相应的不同岩浆岩系列和成矿亚带; ( 3 )不同深度的构造岩浆房组成中心式网格式环带式“三层结构” ,是控制区内不同岩浆岩系列及有关矿床集中分布的主要因素; ( 4 )源于地幔隆起带脊部的碱性玄武岩浆,由于与下地壳物质发生的afc作用强度不同,形成了高钾钙碱性岩浆和橄榄安粗岩浆,分别与铜、金成矿亚系统和铁、硫成矿亚系统有关。
  • According to the characteristics of strata , tectonization and magmatism within the research area in the southwest margin of north china paleocontinent , and under the ideological guidance of mobilism and systematology , the geotectonic framework of the area could be divided as follows : ( 1 ) the longshoushan mountains continental margin ; ( 2 ) the hexi corridor back - arc basin ; ( 3 ) the northern qilianshan mountains suture zone ; ( 4 ) the central qilianshan mountains dispersion type island arc terrane ; ( 5 ) the southern qilianshan mountains back - arc basin ; ( 6 ) the qaidam massif
    根据本区地层、构造、岩浆作用特点,在“系统论” 、 “活动论”思想指导下,厘定华北古大陆西南边缘的构造格局如下:龙首山陆缘带、河西走廊弧后盆地、北祁连缝合带、中祁连离散型岛弧地体、南祁连弧后盆地、柴达木地块。
  • The copper , iron , nickel and silver deposits might be assigned to four metallogenic series : i . the metallogenic subseries of copper , molybdenum , gold , silver deposit related to late devonian - early carboniferous basic - intermediate - acid hypabyssal intrusive - eruptive rocks ; ii . the metallogenic subseriesof iron , copper , zinc deposits related to early carboniferous basic - intermediate - acid volcanic - intrusive rocks ; iii . the metallogenic subseries of copper , silver , iron deposits related to middle - late carboniferous basic - intermediate - acid volcanic - intrusive rocks ; iv . the metallogenic subseries of copper , nickel and platinum group deposits related to late carboniferous - early permian basic - ultrabasic rocks ; 3 , division of regional major metallogenic belts on the basis of the previous work conducted and by following the principles , grounds and methods of the division of metallogenic belts , areas and fields , . in light of this , metallogenic belts of grade iv were divided
    1 、按照成矿系列理论的学术指导思想,将研究区华里西期铜矿床成矿系列划分为四个成矿系列亚系列: 、晚泥盆?早石炭世延东?土屋?三岔口与中酸性岩浆侵入活动有关的cu 、 mo 、 au矿床成矿亚系列、早石炭世与岩浆作用有关的铁、铜、金、银矿床成矿亚系列、中石炭世与岩浆作用有关的cu 、 fe 、 ag 、 au矿床成矿亚系列、晚石炭世-早二叠世与幔源基性?超基性岩有关的铜、镍、铂族矿床成矿亚系列并从地层、岩浆岩、控矿构造、地球化学、成矿特征等方面对各成矿亚系列进行了详细论述。
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