Depositional model of Early Permian reef-island ocean in Eastern Kunlun |
| |
Authors: | Wang Yongbiao Xu Guirong LIN Qixiang Gong Shuyun |
| |
Institution: | Faculty of Earth Sciences, China University of Geosciences, |
| |
Abstract: | Many fusulinid fossils have been found in thin- to middle-bedded limestones which are distributed between the Early Permian
limestone hills and formerly considered as Early Triassic. The fusulinid fossils, identified asNeoshwagerina sp.,Verbeekina sp. andSchwagerina sp., can also be found in massive limestone hills. At the same time, Early Permian radiolarian chert of deep basin facies
was discovered in Animaqing. All the above show that the massive limestone hills, thin- to middle-bedded limestones and radiolarian
chert belong to syndeposits in Early Permian ocean. The sediments in the study area can roughly be divided into three types:
shallow facies, basin facies and transitional facies. The carbonate buildup can be subdivided into massive bioclastic limestone
and reef framestone. Basin facies contains thin- or middle-bedded limestone, abyssal red mudstone or ooze, blue-green mudstone
and radiolarian chert. Transitional facies includes reef talus and platformal skirt facies. The Early Permian ocean in Eastern
Kunlun is recognized as a kind of reef-island ocean environment according to distribution and composition of different facies.
The reef-island ocean in Eastern Kunlun is characterized by reef islands (or carbonate buildups) alternating with basins,
complicated sea-floor topography, sharp facial change and well-developed reefs. |
| |
Keywords: | reef-island ocean Early Permian Eastern Kunlun |
本文献已被 万方数据 SpringerLink 等数据库收录! |
|