Abstract
Plate G-1: Olivine gabbro between crossed polars showing a large grain of plagioclase surrounded by olivine and clinopyroxene in equilibrium. The plagioclase is saussuritised and the olivine is partly serpentinised. The plagioclase contains an olivine inclusion (158/80-2).
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Ghose, N.C., Chatterjee, N., Fareeduddin (2014). Gabbro . In: A Petrographic Atlas of Ophiolite. Springer, New Delhi. https://doi.org/10.1007/978-81-322-1569-1_14
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DOI: https://doi.org/10.1007/978-81-322-1569-1_14
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