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magmatic hydrothermal solution
相关语句
  岩浆热液
     Metallogenic solution was magmatic hydrothermal solution of high temperature and rich in K ̄+,Na ̄+,HCO_3 ̄-,Cl ̄-,thedeposit was formed under the circumstance of low pressure,weak alkalinity and reduction.
     成矿流体为富K ̄+、Na ̄+、HCO ̄-_3、Cl ̄-的高温岩浆热液,矿床形成于低压、弱碱性,还原环境。
短句来源
     Concentrations of As, Co, Cu, F, Fe, Mo, Ni, U, and Zn are higher in anthracite which is obviously influenced by the magmatic hydrothermal solution than those in the fat or coke coals.
     该矿区不同变质程度煤中微量有害元素的含量不同,在明显受岩浆热液影响的无烟煤中As,Co,Cu,F,Fe,Mo,Ni,U,Zn含量较高;
短句来源
     The magmatic hydrothermal solution is the main factor of the enrichment of Zn, As, Mo, Cu, Ni, and Co in coals.
     岩浆热液形成的方解石和黄铁矿脉是峰峰矿区无烟煤中Zn,As,Mo,Cu,Ni,Co等微量有害元素富集的主要载体。
短句来源
     the ore-forming solution not only comes from the magmatic hydrothermal solution rich in REE, but also from the deep circulation warm groundwater rich in F-and Cl- but poor in REE.
     成矿溶液则具有多种来源,既有富含稀土元素的岩浆热液,也有富含F、Cl的贫稀土的深循环地下水热液参与。
短句来源
     hydrogen and oxygen isotope geochemistry indicates that the sources of ore-forming solution for hydrothermal vein-type uranium deposits in China may be divided into three cases, namely mix of magmatic hydrothermal solution and atmospheric water, main origin from atmospheric water, and mix of metamorphic water and atmospheric water.
     氢、氧同位素地球化学表明中国热液脉型铀矿的成矿溶液来源有三种情况,即岩浆热液和大气降水相混合,主要来源于大气降水及变质水和大气水相混合。
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  “magmatic hydrothermal solution”译为未确定词的双语例句
     Acidic magmatic hydrothermal solution in 400 my not only causes metamorphism of the ultrabasic rock but also dissolves part of gold which is scattered in the ultrabasic rock.
     400Ma时活动的中酸性岩浆热液不仅使超基性岩变质,而且使呈分散状态存在于超基性岩中的金一部分破活化而进入热液形成含矿热液。
短句来源
     The hydrothermal solution mightbe the mixture of primary volcanic magmatic hydrothermal solution and meteoric water.
     流体包裹体氢氧同位素测定,成矿热液以岩浆水为主.有大气降水加入形成混合流体,并以低盐度为特征。
短句来源
     The hydrothermal ore-forming solution is meterological water and magmatic hydrothermal solution respectively.
     成矿物质既来自岩体又来自地层.成矿热液以大气降水为主,含部分岩浆水(早期).金管冲铀矿床为一中-低温混合型热液铀矿床
短句来源
     As a deposit of structure--altered rock type, Gaoba gold deposit is located indynamic metamorphic cataclasites, i. e, cataclastic basalt and diorite with strong alteration,and formed in an active tectonic environment by magmatic hydrothermal solution
     高坝金铜矿床定位于动力变质的碎裂岩中,赋矿岩石为碎裂玄武岩和闪长岩,矿体在活动的构造环境中形成,围岩蚀变强烈,是一个在岩浆热液作用下形成的构造蚀变岩型矿床。
短句来源
     , the one led by volcanic hydrothermal solution of early-medium Tamulangou formation, and that by intruded magmatic hydrothermal solution of Late Cretaceous period.
     本区矿化亦可分为两期 ,一是由塔木兰沟中早期火山热液引起的塔木兰沟组地层矿化 ; 二是由于晚上库力期的侵入岩浆热液引起的矿化 .
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  相似匹配句对
     The deposit belongs to the mesothermal magmatic-hydrothermal type.
     它属于中温岩浆热液型矿床.
短句来源
     It is genetically of metamorphic - magmatic hydrothermal superimposed one.
     矿床成因类型为变质—岩浆热液叠加改造型。
短句来源
     Hydrothermal Eruption
     水热爆炸
短句来源
     ON HYDROTHERMAL ROCK
     关于热液岩
短句来源
     The hydrothermal ore-forming solution is dominated by magmatic water mixed with meteoric water.
     成矿热液主要是岩浆水中混入大量天水的混合水.
短句来源
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  magmatic hydrothermal solution
On the basis of the results of fluid inclusion research, the authors suggest that the ore-forming fluid must have a close genetic relation to magmatic hydrothermal solution.
      


On the basis of field study and test data obtained, the source of substancesand the metallogenetic condition of the Zhenzhupo polymetallic deposit are dis-cussed. Sulfur isotope study shows that the δ~(34)S value changes in a narrowrange with an average value close to that of the crust (δ~(34)S=+3.6%), anda normal character of distribution. The concentration of ore-forming elements Pb, Zn, Sb, Ag in wall rocksis about ten times more than Clark values. It is suggested that the sourcematerial was mainly derived...

On the basis of field study and test data obtained, the source of substancesand the metallogenetic condition of the Zhenzhupo polymetallic deposit are dis-cussed. Sulfur isotope study shows that the δ~(34)S value changes in a narrowrange with an average value close to that of the crust (δ~(34)S=+3.6%), anda normal character of distribution. The concentration of ore-forming elements Pb, Zn, Sb, Ag in wall rocksis about ten times more than Clark values. It is suggested that the sourcematerial was mainly derived from magmatic hydrothermal solution and second-ly from the wall rocks. The formation of the deposit was controlled not only by structure but alsoby wall rocks. Hydrothermal solution had played an important role in min-eralization.

根据矿床地质特征和试验资料,讨论矿床的物质来源及成矿条件。矿床的形成不仅受构造控制而且受围岩控制,在成矿作用中岩浆热液起很重要的作用。成矿物质主要来自岩浆热液,其次来自围岩。矿体以充填形式存在,成矿温度从290℃到62℃。属岩浆热液矿床。

The whole-rock lead isotope of the Mesozoic calc-alkaline magmatic rock and Carboniferous-Permian limestone in this region has been studied. The lead isotope of galena from Pb-Zn deposits and occurrences of various genetic types has also been studied, and further the evolution and metallogeny of lead in different geotectonic stages disussed. On this basis, the paper points out that the calc-alkaline magmatic rock is the product formed by contamination of mantle derived magma with continental crust consolidated...

The whole-rock lead isotope of the Mesozoic calc-alkaline magmatic rock and Carboniferous-Permian limestone in this region has been studied. The lead isotope of galena from Pb-Zn deposits and occurrences of various genetic types has also been studied, and further the evolution and metallogeny of lead in different geotectonic stages disussed. On this basis, the paper points out that the calc-alkaline magmatic rock is the product formed by contamination of mantle derived magma with continental crust consolidated 1600m.y, ago. Ore-forming material of the Pb—Zn deposits and occurrences located in the magmatic rock and along the contact zone was derived directly from post-magmatic hydrothermal solution, while ore-forming material of strata-bound Pb—Zn deposits and occurrences located far away from the contact zone was derived by remobilization in the diwa(geodepre-ssion) stage from the ancient platform sedimentary cover formed 340—900m.y.ago. The Carboniferous-Permian limestone is only an important ore-forming country rock, but not a source bed.

研究了本区中生代钙磷性岩浆岩和石炭—二叠系石灰岩的全岩铅同位素,以及不同成固类型铅锌矿床和矿化方铅矿的同位素,进而研究了铅同位素在不同大地构造发展阶段的演化历史及其成矿学。在此基础上提出;本区钙碱性岩浆岩系由地慢岩浆与1600百万年前固结的大陆地壳混熔作用形成的岩浆产物。产于岩浆及其接触带上的铅锌矿床或矿化,其成矿物质直接来自岩浆期后热液;而离接触带较远或很远的层控铅锌矿床或矿化,其成矿物质系由340—900百万年期间形成的古地台盖层中于地洼阶段活化转移而来。石炭—二叠系灰岩只是本区重要的成矿围岩,但不是矿源层。

The general pattern of geological structures in Shanhu district is abroom-shaped rotational structure, with the Hululing structure-magmaticarch as the central axis, and strongly right-rotating in the periphery. Itis converged to the south and spreaded out to the north. Accordingto the differences of structural environments on the two sides of theBijiashan fault, this district can be divided into two orefields. It is pre-dicted that there exists a hidden granite intrusion to the south of Chang-yingling and underneath...

The general pattern of geological structures in Shanhu district is abroom-shaped rotational structure, with the Hululing structure-magmaticarch as the central axis, and strongly right-rotating in the periphery. Itis converged to the south and spreaded out to the north. Accordingto the differences of structural environments on the two sides of theBijiashan fault, this district can be divided into two orefields. It is pre-dicted that there exists a hidden granite intrusion to the south of Chang-yingling and underneath the region from Damudu to LiandLowan. The ore-controlling structures in this district are the Changyingling grid faultsystem, and the ore-holding structures are the secondary shear crackswithin this system. The metallogenic model of this district is proposed inthis paper, i. e. post-magmatic hydrothermal solution was segregated inmany stages from the Changyinglins hidden grante, and coordinating withthe crack structures developed, the ores were deposited by polystage filling,

珊瑚地区地质结构的总格局是以葫芦岭构造岩浆穹隆为中心砥柱,外围强烈右旋并向南收敛、向北撤开的帚状旋扭构造。根据笔架山断层两侧地质构造环境差异,可将珊瑚区划分为东、西两个矿田。预测长营岭以南,大木肚、镰刀湾一带地下存在着隐伏岩体。该区控矿构造为长营岭格状断裂系统;而容矿构造则为格状断裂系统中的次级剪切裂隙。文章最后初步提出该区成矿模式的设想,即长营岭隐伏花岗岩岩浆期后热液多阶段分异,配合构造的发育,多次充填成矿。

 
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