Early-Middle Permian Reef Frameworks and Reef-building Models in the Eastern Kunlun Mountains

Reef frameworks and building models of the Early‐Middle Permian in the eastern Kunlun Mountains have been verified through studies of reef‐building communities, palaeoecology and carbonate facies. The eastern Kunlun reefs are built mainly by 6 reef‐building communities, which include 11 major catego...

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Bibliographic Details
Published inActa geologica Sinica (Beijing) Vol. 75; no. 2; pp. 115 - 125
Main Authors Shugan, TIAN, Jiasong, FAN
Format Journal Article
LanguageEnglish
Published Oxford, UK Blackwell Publishing Ltd 01.06.2001
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Summary:Reef frameworks and building models of the Early‐Middle Permian in the eastern Kunlun Mountains have been verified through studies of reef‐building communities, palaeoecology and carbonate facies. The eastern Kunlun reefs are built mainly by 6 reef‐building communities, which include 11 major categories of frame‐building organisms and 6 categories of reef‐associated organisms. Eight types of reef‐frames have been distinguished and eleven kinds of rocks identified to belong to 6 reef facies. Three sorts of reefs classified by previous researchers, namely mudmounds, knoll reefs and walled reefs, are well developed in the study area. Such reef‐facies association and reef distribution show that there are 4 models of reef growth and development, i.e. the tidal‐bank knoll‐reef model, the plateau‐margin wall‐reef model, the composite wall‐reef model and the deep‐water mudmound model. The reefs are mainly constructed by calcareous sponge and calcareous algae, which are similar to all Permian reefs in other areas of South China and the world. Their great scales indicate a secular stable platform‐marginal environment.
Bibliography:istex:8815411C869E3609858EB6D21097169622AFEB5E
ark:/67375/WNG-WN8QNN0D-F
ArticleID:ACGS513
sgtian2001@sina.com
Tian Shugang Born in September, 1951; graduated from Beijing University in 1977 and received his MS. and Ph. D. degrees at China University of Geosciences (Beijing) in 1985 and 1988 respectively; working now in the Institute of Geology, Chinese Academy of Geological Sciences. He has long been engaged mainly in studies of biostratigraphy, palaeoecology, sequence‐stratigraphy and reefs. Tel: 010–68328223; E‐Mail
ISSN:1000-9515
1755-6724
DOI:10.1111/j.1755-6724.2001.tb00513.x