Abiotic Methane Formation at the Dun Mountain Ophiolite, New Zealand
The production of hydrogen (H2) and methane (CH4) related to olivine hydration (i.e. serpentinization) is considered a major contributor to abiotic hydrocarbon synthesis on Earth. Recent discoveries have highlighted the importance of low temperature (<100oC) serpentinization at continental perido...
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| Language: | en |
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University of Canterbury. Geological Sciences
2015
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| Online Access: | http://hdl.handle.net/10092/10280 |