Petrology and geochemistry of the <scp>Palaeo‐Mesoarchean</scp> Banded Iron formations ( <scp>BIFs</scp> ) from the central Bundelkhand greenstone belts, Bundelkhand Craton, India: Source characteristics and depositional environment-Reference-Cited by-同舟云学术

Petrology and geochemistry of the Palaeo‐Mesoarchean Banded Iron formations ( BIFs ) from the central Bundelkhand greenstone belts, Bundelkhand Craton, India: Source characteristics and depositional environment

Published:2022-05-09 Issue:8 Volume:57 Page:3292-3312
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Malviya Vivek P.¹²^ORCID,Arima Makoto²,Verma Sanjeet K.³^ORCID,K. Pati Jayanta⁴,Shareef Mohamed⁵^ORCID,L. Dora Muduru⁶^ORCID,K. Singh Vinod⁷^ORCID,Prakash Satya¹,Shukla Mayank³

Affiliation:

1. Mineral Physics Division Geological Survey of India, Northern Region Lucknow India

2. Graduate School of Environmental and Information Sciences Yokohama National University Yokohama Japan

3. División de Geociencias Aplicadas Instituto Potosino de Investigación Científica y Tecnológica (IPICYT) San Luis Potosí Mexico

4. Department of Earth and Planetary Sciences Nehru Science Centre, University of Allahabad Prayagraj India

5. Field Training Center Geological Survey of India, SU: Karnataka and Goa, Southern Region Bangalore India

6. Geological Survey of India, Southern Region Hyderabad India

7. Department of Geology, Institute of Earth Sciences Bundelkhand University Jhansi India

Funder

Japan Society for the Promotion of Science

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.4471

Reference106 articles.

1. Composition and weathering conditions of Paleoproterozoic upper crust of Bundelkhand craton, Central India: Records from geochemistry of clastic sediments of 1.9Ga Gwalior Group

2. Hydrothermal chert and associated siliceous rocks from the northern Pacific their geological significance as indication od ocean ridge activity

3. Continentally-derived solutes in shallow Archean seawater: Rare earth element and Nd isotope evidence in iron formation from the 2.9Ga Pongola Supergroup, South Africa

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

5. Rare earth elements in seawater: particle association, shale-normalization, and Ce oxidation

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