Multi-scale development of a stratiform chromite ore body at the base of the dunitic mantle-crust transition zone (Maqsad diapir, Oman ophiolite): The role of repeated melt and fluid influxes
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1994 ◽
Vol 86
(1-3)
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pp. 5-24
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2013 ◽
Vol 377-378
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pp. 299-310
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2018 ◽
Vol 371
(1)
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pp. 262-268
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2017 ◽
Vol 43
(3)
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pp. 213-232
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2020 ◽
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2011 ◽
pp. 619-641
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2020 ◽
Vol 51
(4)
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pp. 1732-1743
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