Emergence of the Late Permian Changhsingian reefs at the end of the Permian

Acta Geologica Sinica (English Edition)

Volumn 77, Issue 3, 2003, Pages 296-306

  Wu, Yasheng ^a   Fan, Jiasong ^a   Jin, Yugan ^b  

^a BEIJING INSTITUTE OF GEOLOGY FOR MINERAL RESOURCES   (China)

^b INSTITUTE OF GEOLOGY AND GEOPHYSICS   (China)

Author keywords

Changhsingian; Emergence; Mass extinction; Reef; Sabkha; Terminal Permian

Indexed keywords

DEPOSITIONAL ENVIRONMENT; DIAGENESIS; DOLOSTONE; MASS EXTINCTION; PERMIAN; REEF; SEA LEVEL CHANGE;

CHINA; GUIZHOU PROVINCE; ZIYUN COUNTY;

EID: 0141794657     PISSN: 10009515     EISSN: 17556724     Source Type: Journal    
DOI: None     Document Type: Article

References (6)

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2. Moore C H. 1989. Carbonate diagenesis and porosity. Elsevier. Amsterdam -Oxford- New York-Tokyo.
3. Noe S U. 1987. Facies and paleogeography of the marine Upper Permian and of the Permian - Triassic boundary in the southern Alps (Bellerophon Formation, Tesero Horizon). Facies, 16: 89-142.
4. Wignall P B, Hallam A. 1992. Anoxia as a cause of the Permian/Triassic mass extinction: facies evidence from northern Italy and the western United States. Paleogeo. Paleoclim. Paleoeco. , 93: 21-46.
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