Water Diffusion in Calc-alkaline Silicate Melts

Water Diffusion in Calc-alkaline Silicate Melts

209 pages· 2009· ISBN 9781109109085
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In addition, the exchange of oxygen isotopes between coexisting minerals during cooling was examined. The mineral pair with the largest isotopic fractionation (PLIF) can bracket their apparent equilibrium temperature (T ae) within their Dodson closure temperatures. This special feature of PLIF may be used to constrain the thermal history of slowly cooled plutonic and metamorphic rocks.

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