Lowermost Triassic (Griesbachian) microbial bindstone-cementstone facies, southwest Japan
- 1 December 1997
- journal article
- Published by Springer Nature in Facies
- Vol. 36 (1) , 1-24
- https://doi.org/10.1007/bf02536874
Abstract
No abstract availableKeywords
This publication has 16 references indexed in Scilit:
- Anoxia as a cause of the Permian/Triassic mass extinction: facies evidence from northern Italy and the western United StatesPublished by Elsevier ,2003
- Oceanic Anoxia and the End Permian Mass ExtinctionScience, 1996
- Palaeoenvironmental changes across the Permian/Triassic boundary at Shangsi (N. Sichuan, China)Historical Biology, 1995
- Anisian (middle triassic) buildups of the Northern Dolomites (Italy): The recovery of reef communities after the permian/triassic crisisFacies, 1993
- Griesbachian (Earliest Triassic) palaeoenvironmental changes in the Salt Range, Pakistan and southeast China and their bearing on the Permo-Triassic mass extinctionPalaeogeography, Palaeoclimatology, Palaeoecology, 1993
- Microbial micritic carbonates in uppermost Permian reefs, Sichuan Basin, southern China: some similarities with Recent travertinesSedimentology, 1992
- Early Triassic stromatolites as post-mass extinction disaster formsGeology, 1992
- The anisian (middle triassic) carbonate bank of Camorelli (Lombardy, Southern Alps)Facies, 1989
- Chronology of Fluctuating Sea Levels Since the TriassicScience, 1987
- Significance of stromatolites for the environmental interpretation of the Buntsandstein (Lower Triassic) rocksInternational Journal of Earth Sciences, 1975