Low intra-crystalline closure temperatures of Cr-bearing spinels from the mantle xenoliths of the Middle Atlas Neogene-Quaternary Volcanic Field (Morocco): Mineralogical evidence of a cooler mantle beneath the West African Craton
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| Description | scholarly article in American Mineralogist, vol. 99 no. 2-3, February 2014 |
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| Publication date | February 1, 2014 |
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