FLUID INCLUSION STUDY OF XIHUASHAN TUNGSTEN DEPOSIT IN THE SOUTHERN JIANGXI PROVINCE, CHINA

被引：4

作者：

GIULIANI, G

LI, YD

SHENG, TF

机构：

[1] JIANGYI BUR GEOL,NANCHANG,PEOPLES R CHINA

[2] GIS,BUR RES GEOL MINIERES,ORLEANS,FRANCE

[3] CHINESE ACAD GEOL SCI,INST MINERAL DEPOSITS,BEIJING,PEOPLES R CHINA

来源：

MINERALIUM DEPOSITA | 1988年 / 23卷 / 01期

关键词：

SPECTROSCOPIC ANALYSIS - SPECTROSCOPY; RAMAN - Applications - TUNGSTEN METALLOGRAPHY - Inclusions;

D O I：

暂无

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

The Xihuashan tungsten deposit is closely related to a small highly evolved granitic intrusion. The fluid phases associated with the wolframite-bearing quartz veins have been investigated using microthermometry and the Raman microprobe. They are highly variable in density and composition. The Xihuashan hydrothermal evolution resulted from a discontinuous sequence of specific events occurring between 420 degree and 150 degree C and during a continuous hydrothermal evolution of the system during cooling. The role played by the CO//2-rich fluids in the tranport and deposition of tungsten in the hydrothermal environment is discussed.

引用

页码：24 / 33

页数：10

共 47 条

[21]

ISHIHARA S, 1980, MINING GEOL

[22]

JACKSON NJ, 1977, J GEOL SOC LONDON, V134, P343, DOI DOI 10.1144/GSJGS.134.3.0343

[23]

KALYUZHNYI VA, 1975, FLUID INCLUSION RES, V8, P82

[24] N2-CH4-CO2 FLUIDS DURING FORMATION OF THE DOME DE LAGOUT, FRANCE [J].

KREULEN, R ;

SCHUILING, RD .

GEOCHIMICA ET COSMOCHIMICA ACTA, 1982, 46 (02) :193-203

[25]

LEBEL L, 1984, TSCHER MINER PETROG, V33, P149

[26]

LU H, 1982, GEOCHEMISTRY, V1, P200

[27]

MARUJEOL P, 1985, TERRA COGNITA, V5, P284

[28]

MASSARE D, 1980, 8 RAST, P244

[29]

NAUMOV VB, 1971, GEOCHEM INT, V8, P381

[30]

Potter R., 1977, GEOL SURV B C, V1421-C, P1

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