Isotopic Sm-Nd signatures of Precambrian Banded Iron Formation from the Fennoscandian shield, East-European Platform, and Bundelkhand craton, India

Author:

Alfimova N.,Raza Mohd Baqar,Felitsyn S.,Matrenichev V.,Bogomolov E.,Nasipuri P.,Saha L.,Pati J.K.,Kumar V.

Funder

Institute of Precambrian geology and geochronology

Russian Academy of Sciences

IISER Bhopal

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference47 articles.

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2. Conditions of subaerial weathering of basalts in the Neoarchean and Paleoproterozoic;Alfimova;Precambr. Res.,2014

3. Silicon isotopes in 3.8 Ga West Greenland rocks as clues to the Eoarchaeansupracrustal Si cycle;André;Earth Planet. Sci. Lett.,2006

4. Bayanova, T.B., Egorov, D.G. 1999. U-Pb age of banded iron formation from Kola peninsula. In: Geology and mineral deposits of the North-West and Central Russia. Apatity. In Russian. pp. 19–24.

5. Yttrium and lanthanides in eastern Mediterranean seawater and their fractionation during redox-cycling;Bau;Mar. Chem.,1997

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