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Archaean Noranda-type exhalative massive sulphide ores were formed by sub-seafloor geothermal activity which leached mafic constituents and ore metals from iron-rich bimodal (basalt–rhyolite) tholeiites and converted them to hydrothermally altered greenschist facies ‘intermediate’ rocks of apparent calc-alkaline affinity.
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本文概览： Archaean Noranda-type exhalative massive sulphide ores were formed by sub-seafloor geo...
文章不错《古细菌的地热系统，“ calc-alsalli”趋势和巨大的硫化物起源》内容很有帮助