Origin of big garnet amphibolites at Gore Mountain and other localities, Adirondack Mountains, New York State, USA: Whole-rock geochemical constraints
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DOI: 10.1130/ges02812.1
Abstract: The Barton Mine garnet amphibolite orebody on Gore Mountain hosts garnet porphyroblasts routinely 15−30 cm across. The orebody was developed in the southern margin of a metamorphosed olivine gabbro pluton. Cumulate layering within the gabbro… read more here.
Keywords: gabbro; whole rock; olivine gabbro; barton mine ... See more keywords