SYNTHESIS OF PYROPE-GROSSULAR GARNETS: AN EXPERIMENTAL STUDY AT P = 2.5 GPA

dc.contributor.authorOrlando A.
dc.contributor.authorBorrini D.
dc.date.accessioned2021-12-30T03:20:45Z
dc.date.available2021-12-30T03:20:45Z
dc.date.issued2003
dc.description.abstractIn order to evaluate the stability of Mg-Ca garnets at P = 2.5 GPa/T = 800-1500 °C, some experiments were performed using both natural and synthetic starting materials. Particular attention was paid to the investigation of the Ca rich side of the pyrope-grossular join and the maximum pyrope content in grossular was found to be about 10 mol.%. The addition of Cr to the system only slightly increases the observed pyrope solubility in grossular whereas Na stabilises melilite and merwinite. Clinopyroxene with a composition lying on the diopside - Ca Tschermak join appears to be the only stable crystalline phase in the middle part of the pyrope-grossular join.
dc.identifierhttps://www.elibrary.ru/item.asp?id=5089451
dc.identifier.citationMineralogy and Petrology, 2003, 78, 1-2, 37-51
dc.identifier.issn0930-0708
dc.identifier.urihttps://repository.geologyscience.ru/handle/123456789/33946
dc.titleSYNTHESIS OF PYROPE-GROSSULAR GARNETS: AN EXPERIMENTAL STUDY AT P = 2.5 GPA
dc.typeСтатья

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