2004•Contributions to Geology and Mineral Resources ResearchRequires access

ORE FLUID CHARACTERISTICS OF XIAOLIUGOU TUNSTEN DEPOSIT

Zhou Hong

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Abstract

Study of Xiaoliugou tunsten deposit indicates a complex genesis. The ore fluid is a mixture of meteoric water, sea water and magmatic water but dominated by sea water. The ore is formed under weak acidic condition. It is presumed that the deposit is a volcanic eruption sedimentary-late magmatic hydrothermal superimposed and reworked deposit.

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Study of Xiaoliugou tunsten deposit indicates a complex genesis. The ore fluid is a mixture of meteoric water, sea water and magmatic water but dominated by sea water. The ore is formed under weak acidic condition. It is presumed that the deposit is a volcanic eruption sedimentary-late magmatic hydrothermal superimposed and reworked deposit.

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Available abstract

Study of Xiaoliugou tunsten deposit indicates a complex genesis. The ore fluid is a mixture of meteoric water, sea water and magmatic water but dominated by sea water. The ore is formed under weak acidic condition. It is presumed that the deposit is a volcanic eruption sedimentary-late magmatic hydrothermal superimposed and reworked deposit.

Key concepts: Geology, Hydrothermal circulation, Geochemistry, Sedimentary rock, Meteoric water, Magmatic water, Volcano, Petrology

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