Archean to Proterozoic (3535–900 Ma) crustal evolution of the central Aravalli Banded Gneissic Complex, NW India: New constraints from zircon U-Pb-Hf isotopes and geochemistry-Reference-Cited by-同舟云学术

Archean to Proterozoic (3535–900 Ma) crustal evolution of the central Aravalli Banded Gneissic Complex, NW India: New constraints from zircon U-Pb-Hf isotopes and geochemistry

Published:2021-07 Issue: Volume:359 Page:106179
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

Kaur Parampreet,Zeh Armin,Chaudhri Naveen

Funder

Deutsche Forschungsgemeinschaft

DAAD

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference129 articles.

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4. Tectono-sedimentary setting of the Paleoproterozoic Zawar Pb-Zn deposits, Rajasthan, India;Bhattacharya;Precambrian Res.,2010

5. Tectonothermal evolution of the Banded Gneissic Complex in central Rajasthan, NW India: Present status and correlation;Bhowmik;J. Asian Earth Sci.,2012

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