Controls on carbonate platform architecture and reef recovery across the Palaeozoic to Mesozoic transition: A high‐resolution analysis of the Great Bank of Guizhou-Reference-Cited by-同舟云学术

Controls on carbonate platform architecture and reef recovery across the Palaeozoic to Mesozoic transition: A high‐resolution analysis of the Great Bank of Guizhou

Published:2020-07-09 Issue: Volume: Page:
ISSN:0037-0746
Container-title:Sedimentology
language:en
Short-container-title:Sedimentology

Author:

Kelley Brian M.¹²^ORCID,Lehrmann Daniel J.³^ORCID,Yu Meiyi⁴,Jost Adam B.⁵,Meyer Katja M.⁶,Lau Kimberly V.²,Altiner Demir⁷,Li Xiaowei¹,Minzoni Marcello⁸,Schaal Ellen K.⁹,Payne Jonathan L.¹

Affiliation:

1. Department of Geological Sciences Stanford University Stanford CA 94305 USA

2. Department of Geology & Geophysics University of Wyoming 1000 E. University Ave. Laramie WY 82071 USA

3. Geosciences Department Trinity University San Antonio TX 78212 USA

4. Department of Resources and Environmental Engineering Guizhou University Caijiaguan Guiyang 550003 Guizhou Province China

5. Department of Earth, Atmospheric, and Planetary Sciences Massachusetts Institute of Technology 77 Massachusetts Avenue, 54‐1025 Cambridge MA 02139 USA

6. Department of Environmental & Earth Sciences Willamette University Collins 215, 900 State Street Salem OR 97301 USA

7. Department of Geological Engineering Middle East Technical University Dumlupinar Blv. No: 1 Ankara 06531 Turkey

8. Department of Geological Sciences University of Alabama Tuscaloosa AL 35487 USA

9. Department of Environmental Science and Studies DePaul University 1110 W Belden Ave. Chicago IL 60614 USA

Funder

National Geographic Society

Publisher

Wiley

Subject

Stratigraphy,Geology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/sed.12741

Reference130 articles.

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2. Onset, development, and cessation of basal Early Triassic microbialites (BETM) in the Nanpanjiang pull-apart Basin, South China Block

3. Lithofacies and depositional processes on a high, steep-margined Carboniferous (Bashkirian–Moscovian) carbonate platform slope, Sierra del Cuera, NW Spain

4. Anatomical and ecological constraints on Phanerozoic animal diversity in the marine realm

5. The lower Triassic anachronistic carbonate facies in space and time

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