Origin of the Neoproterozoic Baijianshan banded iron formation at the southeastern margin of the Tarim Block in NW China: implication for an extremely reducing ocean-Reference-Cited by-同舟云学术

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Origin of the Neoproterozoic Baijianshan banded iron formation at the southeastern margin of the Tarim Block in NW China: implication for an extremely reducing ocean

Published:2021-08-22 Issue: Volume: Page:
ISSN:1000-9515
Container-title:Acta Geologica Sinica - English Edition
language:en
Short-container-title:Acta Geologica Sinica (Eng)

Author:

Hao Xiao-Shu¹,Zhang Chuan-Lin¹,Zhang Hui-Chao¹,Ding Teng¹,Ye Xian-Tao¹

Affiliation:

1. College of Oceanography Hohai University Nanjing 210098 P.R. China

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/1755-6724.14801

Reference91 articles.

1. 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

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

3. Iron(II) oxide determination in rocks and minerals

4. Iron isotope fractionation during microbially stimulated Fe(II) oxidation and Fe(III) precipitation

5. Petrology and geochemistry of the banded iron formation (BIF) of Wadi Karim and Um Anab, Eastern Desert, Egypt: Implications for the origin of Neoproterozoic BIF

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