Pyrite Dissolution in the Cretaceous Yogou Formation of the Niger (Chad) Basin: Implications for Basin Evolution under a Rift Tectonic Setting-Reference-Cited by-同舟云学术

Pyrite Dissolution in the Cretaceous Yogou Formation of the Niger (Chad) Basin: Implications for Basin Evolution under a Rift Tectonic Setting

Published:2022-11-21 Issue:48 Volume:7 Page:43411-43420
ISSN:2470-1343
Container-title:ACS Omega
language:en
Short-container-title:ACS Omega

Author:

Ahmed Kabir Shola¹^ORCID,Liu Keyu¹^ORCID,Fan Yuchen¹,Kra Kouassi Louis¹,Harouna Moussa²,Liu Jianliang¹,Ntibahanana Munezero¹^ORCID,Salim Moussa Z.³,Pidho Justin Jordan⁴,Kouame Melaine Emmanuel⁵,Moussa Hamma Ada²,Ahmed Hafizullah Abba⁶

Affiliation:

1. School of Geosciences, China University of Petroleum (East China), Qingdao 266580, People’s Republic of China

2. Université Abdou Moumouni, Faculté des Sciences et Techniques, Département de Géologie, BP 10662 Niamey, Niger

3. Shandong Ginzre New Material Development Co. Ltd., Jinan, 271100, People’s Republic of China

4. School of Petroleum Engineering, China University of Petroleum (East China), Qingdao 266580, People’s Republic of China

5. State Key Laboratory of Biogeology and Environmental Geology, School of Environmental Studies, China University of Geosciences, Wuhan 430074, People’s Republic of China

6. Department of Geology, Modibbo Adama University of Technology, P. M. B., 2076 Yola, Nigeria

Funder

National Natural Science Foundation of China

Publisher

American Chemical Society (ACS)

Subject

General Chemical Engineering,General Chemistry

Link

https://pubs.acs.org/doi/pdf/10.1021/acsomega.2c03027

Reference54 articles.

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2. Siesser, W. G. Petrography and geochemistry of pyrite and marcasite in DSDP Leg 40 sediments. Initial Reports of the Deep-Sea Drilling Project 1978, pp. 767–775.

3. Evolution of Pyrite Trace Element Compositions from Porphyry-Style and Epithermal Conditions at the Lihir Gold Deposit: Implications for Ore Genesis and Mineral Processing

4. Evolution and origins of pyrite in sandstone-type uranium deposits, northern Ordos Basin, north-central China, based on micromorphological and compositional analysis