A Lady Doctor in Bakhtiari Land by Elizabeth Ness MacBean Ross, James Ness MacBean, Ross PDF

By Elizabeth Ness MacBean Ross, James Ness MacBean, Ross

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In the direct method knowledge of the temperature and mineraI-H20 fractionation factors is not required. Because, usually, several grammes (often 3 0 - 4 0 g) of a mineral have to be crushed in a vacuum line to extract sufficient water for analysis, there are often major problems associated with the selection of suitable material. Samples with both primary and secondary inclusions and recording a multistage mineralization history are common. In the analysis of such samples co-genetic fluid inclusions cannot be selectively crushed.

Two different types of volcanogenic deposits have been studied isotopically: (1) the cupriferous massive sulphide deposits related to ophiolite igneous complexes s7 and (2) the F e - C u - P b Z n - A g - A u Kuroko deposits, which are closely associated with submarine felsic volcanism. 89,9~ The deposits are relatively underformed and have not been metamorphosed. The isotopic characteristics of the fluids involved with the metamorphism of the oceanic basaltic host rocks and the hydrothermal stockwock mineralization are discussed in detail elsewhere in this volume.

G. Goldfield, Tonopah, Nevada (Ag-Au), Pachuca, Mexico (Ag-Au), San Juan Mountains District, Colorado ( A g - A u - P b - Z n ) ; sea w a t e r - Troodos, Cyprus (Fe-Cu), Kuroko, Japan (Fe-Cu-Pb-Zn). Solutions of more than one origin are important in certain de posits (magmatic and meteoric - porphyry copper and molybdenum deposits) and are present in many. In the porphyry Cu-Mo deposits the initial major ore transportation and alteration processes (K-feldspar-biotite alteration) are magmatic-hydrothermal events that occur at 750-500 ~C.

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A Lady Doctor in Bakhtiari Land by Elizabeth Ness MacBean Ross, James Ness MacBean, Ross

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