Persistence of pre-metamorphic C and O isotopic signatures in marbles subject to Pan-African granulite-facies metamorphism and U–Th mineralization (Tranomaro, Southeast Madagascar)-Reference-Cited by-同舟云学术

Persistence of pre-metamorphic C and O isotopic signatures in marbles subject to Pan-African granulite-facies metamorphism and U–Th mineralization (Tranomaro, Southeast Madagascar)

Published:1998-09 Issue:3-4 Volume:150 Page:247-262
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Boulvais P.,Fourcade S.,Gruau G.,Moine B.,Cuney M.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference53 articles.

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4. Banner, J.L., Hanson, G.N., Meyers, W.J., 1988. Water–rock interaction history of regionally extensive dolomites of the Burlington–Keokuk formation (Mississipian): isotopic evidence. In: Shukla, V., Baker, P.A. (Eds.), Sedimentology and Geochemistry of Dolostones. Spec. Pub. 43, Society of Econ. Paleontol. and Mineral., Tulsa, OK, USA, 97–113.

5. Transport mechanisms by fluid-flow in metamorphic rocks: oxygen and strontium decoupling in the Trois Seigneurs Massif—a consequence of kinetic dispersion?;Bickle;Am. J. Sci.,1992

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