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RAMAN SPECTROSCOPIC CHARACTERIZATION OF CARBONACEUS MATERIAL FROM OUTER CARPATHIANS HYDROTHERMAL VEINS - IMPLICATION TO THE INTERPRETATION OF -MARMAROSH DIAMONDS- CRYSTALLIZATION ENVIRONMENT
Abstract
Carbonaceous material (CM) from Outer Carpathians hydrothermal veins was investigated by Raman spectroscopy in order to reveal thermal conditions of its alteration. The studied CM as being found in association with пїЅmarmarosh diamondsпїЅ confirms that the crystallization environment of this mysterious quartz variety is connected with thermally-influenced organic matter. Obtained temperatures in the range of 159 to 205пїЅC are indicative for low to medium hydrothermal conditions. Presented temperatures stay in quite correlation with previously presented in reference to the hydrothermal minerals from Outer Carpathians veins. Therefore, the application of Raman geothermometry has been found to be useful tool for analysis of hydrothermally altered carbonaceous material.
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