Geochemistry of Late Archaean shaly BIF formed by oxic exogenic processes: an example from Ramagiri schist belt, Dharwar Craton, India-Reference-Cited by-同舟云学术

Geochemistry of Late Archaean shaly BIF formed by oxic exogenic processes: an example from Ramagiri schist belt, Dharwar Craton, India

Published:2015-06-18 Issue:3 Volume:34 Page:362-378
ISSN:1000-9426
Container-title:Chinese Journal of Geochemistry
language:en
Short-container-title:Chin. J. Geochem.

Author:

Mishra Meenal^ORCID

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology

Link

http://link.springer.com/content/pdf/10.1007/s11631-015-0058-2.pdf

Reference97 articles.

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2. Balakrishnan S, Hanson GN, Rajamani V (1999) U-Pb isotope study on zircons and sphenes from the Ramagiri area, southern India: evidence for accretionary origin of eastern Dharwar Craton during late Archean. J Geol 107:69–86

3. Bau M (1993) Effects of syn- and post-depositional processes on the rare earth element distribution in Precambrian iron formations. Eur J Mineral 5:257–267

4. Bau M, Dulski P (1996) Distribution of yttrium and rare-earth. Elements in the Penge and Kuruman iron-formations, Transvaal Supergroup, South Africa. Precamb Res 79:37–55

5. Bau M, Moller P (1993) Rare earth element systematics of the chemically precipitated iron formations and the evolution of the terrestrial atmosphere-hydrosphere lithosphere system. Geochim Cosmochim Acta 57:2239–2249

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