Abstract
McSween and Nystrom (1979) have presented a detailed account of field, petrographic, and mineral chemical characteristics of the Dutchmans Creek gabbroic intrusion, which shows a strong resemblance to Permo–Triassic gabbroic intrusions in eastern Queensland, Australia. Recently, Ambler and Ashley (1977) described spectacular vermicular or-thopyroxene–magnetite intergrowths from the Wa-teranga layered mafic intrusion from southeast Queensland and presented petrographic and mineral chemical data for specimens containing the sym-plectites.
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