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- W2377668906 abstract "Hydrothermal solution sediment differs from the common sediment and is mainly related to hydrothermal fluid type. This paper classifies the hydrothermal solutions into the middle high temperature type and the middle low temperature type. Sedimentary rocks of middle high temperature hydrothermal solution include potash feldspar rock, silicalite, hyalotourmalite, albite rock; and the fluorite rock; and the sedimentary rocks of middle low temperature hydrothermal solution consist of hydrochloric rock, sulphate rock etc. Potash feldspar rock is identified as a standard type of middle high hydrothermal solution sedimentary rock in this paper and mainly includes adularia and baryta feldspar. Hydrothermal solution sedimentary carbonate minerals generally include Fe carbonatite, Mg carbonatite, Mn carbonatite and Ca carbonatite, and their forming is related to immiscibility temperature of H 2 O and CO 2 . That is to say, the carbonate is formed below 266℃, or above the seawater compensation level. There are interbedded strata of hydrothermal solution metasomatic alteration rock in hydrothermal solution sedimentary rock. Especially, hydrothermal solution metasomatic sedimentary rocks are formed through metasomatosing argillaceous and Ca argillaceous sediment in the high temperature hydrothermal solution active regions. These sedimentary rocks include scapolite corneit, pitkarantite, scarn, chloritite rock etc. The study of the Huogeqi Cu polymetal deposit shows that the total REE content is relatively low in hydrothermal solution metasomatic pitkarantite rock, rich in light REE and deficient in heavy REE, and that the model of the REE distribution is of positive abnormality of Eu." @default.
- W2377668906 created "2016-06-24" @default.
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- W2377668906 date "2001-01-01" @default.
- W2377668906 modified "2023-09-25" @default.
- W2377668906 title "HYDROTHERMAL SEDIMENTARY ROCK AND INDICATORS OF MINERALS AND ROCKS" @default.
- W2377668906 hasPublicationYear "2001" @default.
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