metamorphic water

The low velocity layer possibly is formed by metamorphic water .

壳内低速层可能是由变质水造成的。

The ooze water of these various types belongs to low metamorphic water .

这些不同类型的软泥水均属软泥阶段的浅变质水。

From the isotopic constitutions of hydrogen and oxygen a metamorphic water feature is shown .

氢、氧同位素组成显示变质水特征。

H-O isotopes constitute reflects the characteristics of magma flow and metamorphic water interfusion .

石英的氢氧同位素组成反映出岩浆流体与变质水混入溶液特征。

The D and O isotopic compositions show that they emerge from the compound results of the magma water , metamorphic water , hosted water and rain water ;

脉石矿物D、O同位素组成代表了岩浆水、变质水、建造水及大气降水混合作用的结果；

Metamorphic water constitutes most of ore-bearing metamorphic hydrothermal water , which tends to mineralize in metamorphic front region and before the front region .

变质水则是含矿变质热液的主体并趋向于在变质前锋区及前锋区前成矿；

Based on the mineral intergrowth analysis and the determination of H , O isotopes in quartz , it is considered that hydrothermal ore forming solution mainly comes from metamorphic water .

通过矿物共生分析和石英中氢氧同位素测试等手段，认为成矿热液主要来源于变质水；

It is of meteoric water and metamorphic water genetic ore with bigger ore-forming depth . The genetic type belongs to the sedimentation metamorphosis and mid-lowed hydrothermal reconstruction .

其成因类型为大气降水变质水热液型金矿。

Its geochemical feature indicates that ore forming elements mainly comes from stratum and rock of pre Devonian period and ore forming solution is complex fluid of syngenetic water , metamorphic water and meteoric water .

矿床的地质地球化学特征表明，成矿物质主要来自前泥盆纪基底的地层和岩石，成矿溶液主要为盆地同生水与变质水及大气降水的混合流体。

The ore-forming fluids derived from more complex resources that some were mainly derived from magmatic water with some contributions from meteoric water , some prominently resulted from meteoric water and some were partly influenced by metamorphic water .

成矿流体来源较为复杂，有的以岩浆水为主混有大气降水，也有大气降水占主导，部分受到变质流体的影响。

Mineralization depth was about 1500m . Forming materials are mainly from Taishan group , and ore-forming fluid has the characteristics of multiple sources . They are mainly composed of magmatic water and meteoric water , accompanied with a small amount of metamorphic water .

成矿深度处在1500m左右。成矿物质主要来源于泰山岩群地层：成矿流体具多来源性，以岩浆水和大气降水为主，并有少量变质水的参与。

The magmatic water of granitoid related with gold deposits in . North China Platform is characterized by low SD values ( - 120-85 ‰) . The metamorphic water of ancient crys-talline basement is also characterized by low SD values ( - 95 ‰) .

华北地台与金矿床有关的花岗岩，其岩浆水以δD值较低为特征（-120‰&85‰），古老结晶基底变质水同样亦以贫δD为特征（-95‰）。

The ore forming fluid is mainly composed of magmatic water and metamorphic water with minor atmospheric water , whose chemical type is of K ~ - Na ~ + Ca ~ ( + + ) Mg ~ ( + + ) F ~ - Cl ~ - .

金矿成矿作用经三个阶级的流体活动。成矿流体的组成，以岩浆水和变质水为主，其次是大气降水，化学类型为K~+～Na~+Ca~（++）Mg~（++）F~-Cl~-型。

The generation of the carbonate of Chang 8 reservoir was related to the organic acid decarboxylation , and during migration , the oil source fluids were associated with the interaction of the hydrothermal fluids which were derived from magma intrusion or precipitation of the metamorphic water .

油层中的碳酸盐矿物与碳酸盐胶结物形成与有机酸脱羧作用有关，油源流体的运移过程中伴随着热流体的共同作用，热流体来自于区域上的岩浆侵入及变质水的沉淀作用。

By the association of rock and mineral , composition and property of the inclusion and testing of isotope etc. , the authors indicated that the mineralizing matter came from the wallrock , the mineralizing fluid came from the metamorphic water and mixed water of magmatic water and rainwater .

通过岩石矿物组合及包裹体组成、性质、同位素等测试，确定成矿物质来源于围岩，成矿流体来源于变质水且有岩浆水与雨水的混入。

Development and verification of creep constitutive model of low-grade metamorphic slate considering water damage .

考虑含水损伤的碎裂浅变质板岩蠕变本构模型开发及验证。

The mineralizing solutions are considered as a mixed system of metamorphic and meteoric water .

成矿溶液是变质水和大气降水的混合体系。

The primary mineralizing fluid is a H2O-NaCl-CO2-dominated system with low salinity , principally derived from a mixed source of metamorphic and meteoric water .

初始的成矿流体是一个低盐度的以H2O－NaCl-CO2为主的上学体系，主要源于大气水与变质建造水的混合。