Dissolution processes of elements from subducting sediments into fluids: Evidence from the chemical composition of the Sanbagawa pelitic schists
Author:
Publisher
Geochemical Society of Japan
Subject
Geochemistry and Petrology,Geophysics
Reference56 articles.
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2. Banno, S., Higashino, T., Otsuki, M., Itaya, T. and Nakajima, T. (1978) Thermal structure of the Sanbagawa metamorphic belt in central Shikoku. J. Phys. Earth 26 (Suppl.), 345-356.
3. Bebout, G. E. (1995) The impact of subduction-zone metamorphism on mantle-ocean chemical recycling. Chem. Geol. 126, 191-218.
4. Bebout, G. E. (1997) Nitrogen isotope tracers of high-temperature fluid-rock interactions: Case study of the Catalina Schist, California. Earth Planet. Sci. Lett. 151, 77-90.
5. Bebout, G. E. and Fogel, M. L. (1992) Nitrogen-isotope compositions of metasedimentary rocks in the Catalina Schist, California: Implications for metamorphic devolatilization history. Geochim. Cosmochim. Acta 56, 2839-2849.
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