Siliceous dolomites in the Horsethief Creek aureole, S.E. British Columbia: fluid infiltration and mineral reactions
Potassic siliceous dolomites in the Horsethief Creek aureole, S.E. British Columbia, Canada record peak contact-metamorphic conditions of ≈2.2 kbars and 650 °C in the inner aureole. The protolithic dolostones have varying but small amounts of disseminated quartz (≤ 5 volume percent) and K-feldspa...
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| Language: | English |
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2009
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| Online Access: | http://hdl.handle.net/2429/9016 |