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Name:AntonioHic | 13, Nov, 2023 01:03:33 | |
and the pervasive impregnation of the depleted harzburgite by basaltic melt. The cumulate rocks near this transition are dominated by dunite with subordinate troctolite and gabbro and minor wehrlite. Facies Smc forms elongate channels trending at high angles to the palaeoflow of fluvial channels. Th | ||
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