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Constraints from the mantle sections of ophiolites...

Constraints from the mantle sections of ophiolites...
Constraints from the mantle sections of ophiolites...
Constraints from the mantle sections of ophiolites...
Constraints from the mantle sections of ophiolites...
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Constraints from the mantle sections of ophiolites...
Illustration
01/01/1998
fig i keleman.jpg
Date is approximate.
Caption from Oceanus magazine, Vol. 41, No. 1, Pg. 28:
Constraints from the mantle sections of ophiolites, and theoretical studies of reactive porous flow of melt through partially soluble rocks, can be used to infer that melt extraction beneath mid-ocean ridges occurs in a coalescing network of porous dunite channels.
Courtesy of Peter Kelemen
© Woods Hole Oceanographic Institution
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