Contrasting styles of oxygen isotope exchange
Exchange of oxygen isotopes encrypts a sensitive record of the thermal evolution and fluid-exchange history of igneous and metamorphic rocks. Deciphering this record requires measurement of isotope ratios at an appropriate scale together with understanding of the processes involved: diffusion, recrystallization, new mineral growth, and fluid flow.
© 1994 Mineralogical Society.
Published - Eiler_1994p924.pdf