Carbon and oxygen isotopes of the Lianglitage Formation in the Tazhong area, Tarim Basin: Implications for sea‐level changes and palaeomarine conditions-Reference-Cited by-同舟云学术

Carbon and oxygen isotopes of the Lianglitage Formation in the Tazhong area, Tarim Basin: Implications for sea‐level changes and palaeomarine conditions

Published:2022-11-11 Issue:3 Volume:58 Page:967-980
ISSN:0072-1050
Container-title:Geological Journal
language:en
Short-container-title:Geological Journal

Author:

Tao Ye¹,Gao Da²^ORCID,He Youbin¹²,Ngia Ngong Roger³,Wang Mingmin⁴,Sun Chunyan⁵,Huang Xinmiao¹,Wu Jianwei¹

Affiliation:

1. School of Geosciences Yangtze University Wuhan China

2. Key Laboratory of Exploration Technologies for Oil and Gas Resources (Yangtze University) Ministry of Education Wuhan China

3. Department of Geology University of Buea Buea, Southwest Cameroon

4. South China Sea Institute of Oceanology Chinese Academy of Sciences Guangzhou China

5. Research Institute of Petroleum Exploration and Production Tarim Oilfield Company, PetroChina Korla China

Funder

National Natural Science Foundation of China

Yangtze University

Publisher

Wiley

Subject

Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/gj.4637

Reference50 articles.

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2. Negative δ13Ccarb values at the Jurassic-Cretaceous boundary – Vaca Muerta Formation, Neuquén Basin, Argentina

3. Bathymetric and isotopic evidence for a short-lived Late Ordovician glaciation in a greenhouse period

4. Delicata sedimentary model to Lianglitage formation of upper Ordovician in the northern margin of isolated platform in the center of Tarim basin;Chen X.;Acta Sedimentologica Sinica,2009

5. Facies, cycles, and controls on the evolution of a keep-up carbonate platform (Kimmeridgian, Swiss Jura)

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