Lower Triassic peritidal cyclic limestone: an example of anachronistic carbonate facies from the Great Bank of Guizhou, Nanpanjiang Basin, Guizhou province, South China
- 1 September 2001
- journal article
- Published by Elsevier in Palaeogeography, Palaeoclimatology, Palaeoecology
- Vol. 173 (3-4) , 103-123
- https://doi.org/10.1016/s0031-0182(01)00302-9
Abstract
No abstract availableKeywords
This publication has 37 references indexed in Scilit:
- Palaeoenvironments and faunal recovery after the end-Permian mass extinctionPublished by Elsevier ,1999
- Early Triassic calcimicrobial mounds and biostromes of the Nanpanjiang basin, south ChinaGeology, 1999
- Lower Triassic large sea-floor carbonate cements: Their origin and a mechanism for the prolonged biotic recovery from the end-Permian mass extinctionGeology, 1999
- Controls on facies architecture of a large Triassic carbonate platform; the Great Bank of Guizhou, Nanpanjiang Basin, South ChinaJournal of Sedimentary Research, 1998
- Trace fossils and the aftermath of the Permo-Triassic mass extinction: evidence from northern ItalyPalaeogeography, Palaeoclimatology, Palaeoecology, 1996
- Palaeoenvironmental changes across the Permian/Triassic boundary at Shangsi (N. Sichuan, China)Historical Biology, 1995
- Early Triassic stromatolites as post-mass extinction disaster formsGeology, 1992
- Tectonics of the Tethysides: Orogenic Collage Development in a Collisional SettingAnnual Review of Earth and Planetary Sciences, 1987
- Speculations on the Mesozoic Plate tectonic evolution of eastern ChinaTectonics, 1983
- Tiering in Suspension-Feeding Communities on Soft Substrata Throughout the PhanerozoicScience, 1982