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  hydrothermal
     Studies on Hydrothermal Circulation and Smokers of Modern Seafloor Hydrothermal Activity
     现代海底热液活动的热液循环及烟囱体研究
短句来源
     The Study on Models for Formation of Megaplume Flow in Modern Seafloor Hydrothermal Activity
     现代海底热液活动中巨羽流形成机制的模型研究
短句来源
     LOW TEMPERATURE lgfo_2-PH DIAGRAMS OF SULFUR ISOTOPE EVOLUTION IN EQUILIBRIUM WITH HYDROTHERMAL SYSTEM
     低温平衡热液系统中硫同位素演化的Igf_(O_2)-pH图解
短句来源
     HYDROTHERMAL URANIUM DEPOSITS AND SULPHUR ISOTOPES
     热液铀矿床与硫同位素
短句来源
     AN EXPERIMENTAL STUDY ON PHYSICO-CHEMICAL CONDITIONS FOR THE FORMATION OF SCAPOLITE IN THE HYDROTHERMAL SYSTEM
     方柱石在热液中形成的物理化学条件的实验研究
短句来源
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  hydrothermal solution
     the pressure of hydrothermal solution of pre-ore stage is (1—2)×10~8Pa, ore-forming stage is (5—10)×10~7Pa, post-ore stage is(3—5)×10~7Pa;
     矿前期热液压力为(1—2)×10~8SPa,矿期为(5—10)×10~7pa,矿后期为(3—5)×10~7Pa。
短句来源
     The Eh-pH diagrams for Cu-Fe-S-O-H, Fe-S-O-H, Cu-S-O-H, Pb-S- O-H and Zn-S-O-H systems at 150℃ have been constructed, and by these diagrams we can explain certain questions for forming minerals in hydrothermal solution.
     本文绘制了150℃ Cu-Fe-S-O-H、Fe-S-O-H、Cu-S-O-H、Pb-S-O-H及Zn-S-O-H系Eh-pH图,并利用这些图阐明热液成矿的某些问题。
短句来源
     The hydrothermal solution concentrated W, Ca, Mg, Be, Sr and Mo at W mineralization, and path-indicator are Ca and Mo.
     钨矿化阶段热液富集W、Ca、Mg、Be、Sr、Mo,矿化指示元素为Ca、Mo;
短句来源
     Among the superimpositions of multi-stage hydrothermal fluids and multi-stagemineralizations,the ore-forming hydrothermal solution of the early stage was probably provided jointly by Baishanzhi granodiorite(370±25 Ma)and Hanshan diorite(347.1±6.4 Ma).
     在多期热液叠加,多期成矿作用中,早期成矿的热液很可能是白山子花岗闪长岩(370±25 Ma)、寒山辉长岩(347.1±6.4 Ma)共同提供的。
     Among the superimpositions of multi-stage hydrothermal fluids and multi-stage mineralizations, the ore-forming hydrothermal solution of the early stage was probably provided jointly by Baishanzhi granodiorite (370±25 Ma) and Hanshan diorite (347.1±6. 4 Ma).
     在多期热液叠加,多期成矿作用中,早期成矿的热液很可能是白山子花岗闪长岩(370±25 Ma)、寒山辉长岩(347.1±6.4 Ma)共同提供的。
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  hydrothermal fluid
     δ~(34)S_(FeS2)=-2.3‰—+20.5‰(40 samples), δ~(34)S_(av). =+10.44%. These data indicate a mixed feature of sulfur in the hydrothermal fluid coming from the upper mantle and the crust.
     矿石中40个黄铁矿δ~(34)S=-2.3‰-+20.5‰,其平均值δ~(34)S=+10.44‰,这表明成矿热液中的硫具有深部硫和地壳硫的混合特征。
短句来源
     The mean temperature of the fluids is 96℃-158℃, average salinity is 0.26%-1.28% and depth of activity is 0.26km -0.67km. This indicates the hydrothermal fluid had the basic characteristics of low temperature, low salinity and were from shallow depths in the crust.
     平均均一温度96~158℃,平均盐度0.26%~1.08%,热液活动深度0.26~0.67km,具有低温、低盐度、在地壳浅部活动的基本特征.
短句来源
     In addition,various δ 34S values in H2S from hydrothermal fluid in different layers were believed to be resulted from the mixing between end compositions of seawater and basalt in different proportions.
     热液流体中的δ34S值(H2S)随时间的变化是由于海水端元和玄武岩端元不同比例的混合所致。
短句来源
     Evidences from REE geochemistry show that: (1) during tourmalinization, REE (especially HREE)migrated from γ_5~(2(3)B) granite to hydrothermal fluid, (2) both inherited and evolutional REE exist in the uranium veins, (3) it seems mostly likely that uranium and REE in the hydrothermal fluid was transported together as soluble carbonate complexes or fluoride complexes, (4) REE and other ore-forming source material of No.
     经REE地球化学研究表明:(1)电气石化自变质作用可以促使REE,特别是HREE向热液流体中转移; (2)热液铀矿脉中的REE对γ_5~(2(3)B)花岗岩既有继承性,又有演化性:(3)含铀热液流体中的REE同U一起呈含CO_3~(2-),F~-络合物形式迁移、分异和沉淀;
短句来源
     IONIC DIFFUSION IN HYDROTHERMAL FLUID:Ⅰ.THEORETICAL CALCULATION OF TRACER DIFFUSION COEFFICIENTS
     热液流体中的离子扩散作用:Ⅰ.示踪扩散系数的理论计算
短句来源
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  hydrothermal fluids
     (3)Na~(+)-K~(+)(-Ca~(2+))+Mg~(2+)composition of fluid inclusions diagram shows intimate relationship between gold metallogenic fluids and magmatic hydrothermal fluids;
     (3)在流体包裹体的w(Na+)-w(K+)-w(Ca2++Mg2+)成分三角图上表明金成矿流体和岩浆热液具亲缘关系;
短句来源
     MINERALOGICAL IMPLICATIONS FOR AU (HS)_2 ̄- IN PORPHYRY TYPE HYDROTHERMAL FLUIDS
     斑岩型成矿热液中Au(HS)_2~-存在的矿物学证据
短句来源
     Among the superimpositions of multi-stage hydrothermal fluids and multi-stagemineralizations,the ore-forming hydrothermal solution of the early stage was probably provided jointly by Baishanzhi granodiorite(370±25 Ma)and Hanshan diorite(347.1±6.4 Ma).
     在多期热液叠加,多期成矿作用中,早期成矿的热液很可能是白山子花岗闪长岩(370±25 Ma)、寒山辉长岩(347.1±6.4 Ma)共同提供的。
     Among the superimpositions of multi-stage hydrothermal fluids and multi-stage mineralizations, the ore-forming hydrothermal solution of the early stage was probably provided jointly by Baishanzhi granodiorite (370±25 Ma) and Hanshan diorite (347.1±6. 4 Ma).
     在多期热液叠加,多期成矿作用中,早期成矿的热液很可能是白山子花岗闪长岩(370±25 Ma)、寒山辉长岩(347.1±6.4 Ma)共同提供的。
     (6)S,H,O and Pb isotopes show that the ore-forming fluid and(metallogenic) material come from magmatic hydrothermal fluids.
     (6)S、H、O、Pb同位素组成表明成矿物质和成矿流体来自岩浆热液
短句来源
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  hydrothermal
Mordenite composite membranes were prepared by means of coating a porous α-alumina support with nanosized mordenite seeds followed by hydrothermal crystallization.
      
The growth rate of the mordenite crystal increases more along c-axis than that along a-axis or b-axis with increasing temperature for hydrothermal crystallization.
      
The ion-exchanger LiAlTiO4 of spinel type was prepared by the common precipitation/hydrothermal crystallization method, and was acid-modified.
      
Preparation of lithium fast ionic conductor by sol-gel-hydrothermal method
      
The solid fast ionic conductor was synthesized by the sol-gel-hydrothermal method.
      
更多          
  hydrothermal solution
It is found that the nanotubes of magnesium hydrosilicate Mg3Si2O5(OH)4 are formed through different mechanisms depending on the initial state of reactants, the composition of the hydrothermal solution, and temperature.
      
Precipitation of Amorphous Silica from a High-Temperature Hydrothermal Solution
      
The polymerization of monomeric silica in a hydrothermal solution with the formation of colloidal silica particles is investigated experimentally.
      
Formation of Solid Deposits of Amorphous Silica in a Flow of Hydrothermal Solution
      
It is established that the deposits are formed through the mass transfer of colloidal particles from a flow of a hydrothermal solution.
      
更多          
  hydrothermal fluid
A thermodynamic model of the effect of Se on the transport properties of Ag-bearing hydrothermal fluid has been developed.
      
The abnormal enrichment of noble metal elements is closely related with hydrothermal fluid that flew out on the sea floor through deep cycling and reaction with Proterozoic ultramafic-mafic igneous rocks forming noble metal rich fluid.
      
It was formed by illitization of plagioclase and micas during hydrothermal fluid-rock interaction within the porphyry body and near the contact zone with wall rocks.
      
The pattern of hydrothermal circulation and flow velocity of hydrothermal fluid are strongly influenced by strata permeability structures, changes of permeability in high permeable basement layer, fracture zone and cooling intrusion.
      
The main homogenization temperatures of primary fluid inclusions in fluorite are from 260 to 310°C, indicating the temperature of hydrothermal fluid.
      
更多          
  hydrothermal fluids
Results obtained show that authigenic carbonate formation is a biogeochemical (microbial) process, which involves carbon from ancient sedimentary rocks, abiogenic methane, and bicarbonate-ion of hydrothermal fluids into the modern carbon cycle.
      
The cavitation and cavitation-ablation mechanisms of formation of mineral nano-and microspherules in hydrothermal fluids are considered.
      
It has also been shown that the effect of hydroselenide complexes on Ag behavior in natural hydrothermal fluids may be ignored.
      
The hydrothermal fluids are considered to be of magmatic origin; as the hydrothermal system evolved, they became diluted with seawater that was contained in fractured oceanic crust.
      
Specifics in the composition and crystallization of the hybrid melt causes the enrichment of the residual melt and hydrothermal fluids in Fe and other elements, in particular, Cu and Mo.
      
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