The Evolutionary Characteristics of Lower Permian Keziliqiman Reefs in the Southwest Margin of Tarim Basin, Northwest China

The Permian strata in the southwest Tarim Basin contain organic reefs with good exploration prospects. Based on observations of outcrops and thin section examination of the Permian Keziliqiman Formation reef in the Sangzhu section of Pishan County, Xinjiang, northwest China, the basic characteristic...

Full description

Saved in:
Bibliographic Details
Main Authors: Yijun Wang, Hongming Tang, Guang Yang, Zhenyu Wang, Yunfeng Zhang, Lei Chen
Format: Article
Language:English
Published: Wiley 2022-01-01
Series:Geofluids
Online Access:http://dx.doi.org/10.1155/2022/3851806
Tags: Add Tag
No Tags, Be the first to tag this record!
_version_ 1832549738851860480
author Yijun Wang
Hongming Tang
Guang Yang
Zhenyu Wang
Yunfeng Zhang
Lei Chen
author_facet Yijun Wang
Hongming Tang
Guang Yang
Zhenyu Wang
Yunfeng Zhang
Lei Chen
author_sort Yijun Wang
collection DOAJ
description The Permian strata in the southwest Tarim Basin contain organic reefs with good exploration prospects. Based on observations of outcrops and thin section examination of the Permian Keziliqiman Formation reef in the Sangzhu section of Pishan County, Xinjiang, northwest China, the basic characteristics of the reef are studied. This organic reef, as a point reef which grew along the platform margin, has a complete subfacies system of base, core, front, back, and cap. The lithology of the lower zone of the core is mainly sponge bafflestone, while that of the upper zone is coral framestone. The development of reefs was controlled by the rise and fall of sea level. It was when the sea level rose in southwest Tarim Basin that the Keziliqiman reef gradually came into existence. Later, with rapid decline of sea level in that area, the Sangzhu section turned into a hot and dry supratidal zone, where algae began to flourish, dolomitization intensified, reef building organisms died en masse, and eventually the reef died. Paleontological and geochemical characteristics of the Sangzhu reef indicate that the sea-level decline in southwest Tarim Basin may be related to the Early Permian glaciers. Since then, the reef began to be transformed by diagenesis. But on the whole, its effect was not significant. Furthermore, its diagenetic process had more to do with marine fluids than with nonmarine fluids, for nonmarine fluids was powerful enough to affect bioclasts but powerless to affect micritic matrix.
format Article
id doaj-art-aa8196610c674ccc8725b7486cebc806
institution Kabale University
issn 1468-8123
language English
publishDate 2022-01-01
publisher Wiley
record_format Article
series Geofluids
spelling doaj-art-aa8196610c674ccc8725b7486cebc8062025-02-03T06:08:41ZengWileyGeofluids1468-81232022-01-01202210.1155/2022/3851806The Evolutionary Characteristics of Lower Permian Keziliqiman Reefs in the Southwest Margin of Tarim Basin, Northwest ChinaYijun Wang0Hongming Tang1Guang Yang2Zhenyu Wang3Yunfeng Zhang4Lei Chen5School of Geoscience and TechnologySchool of Geoscience and TechnologySchool of Geoscience and TechnologySchool of Geoscience and TechnologySchool of Geoscience and TechnologySchool of Geoscience and TechnologyThe Permian strata in the southwest Tarim Basin contain organic reefs with good exploration prospects. Based on observations of outcrops and thin section examination of the Permian Keziliqiman Formation reef in the Sangzhu section of Pishan County, Xinjiang, northwest China, the basic characteristics of the reef are studied. This organic reef, as a point reef which grew along the platform margin, has a complete subfacies system of base, core, front, back, and cap. The lithology of the lower zone of the core is mainly sponge bafflestone, while that of the upper zone is coral framestone. The development of reefs was controlled by the rise and fall of sea level. It was when the sea level rose in southwest Tarim Basin that the Keziliqiman reef gradually came into existence. Later, with rapid decline of sea level in that area, the Sangzhu section turned into a hot and dry supratidal zone, where algae began to flourish, dolomitization intensified, reef building organisms died en masse, and eventually the reef died. Paleontological and geochemical characteristics of the Sangzhu reef indicate that the sea-level decline in southwest Tarim Basin may be related to the Early Permian glaciers. Since then, the reef began to be transformed by diagenesis. But on the whole, its effect was not significant. Furthermore, its diagenetic process had more to do with marine fluids than with nonmarine fluids, for nonmarine fluids was powerful enough to affect bioclasts but powerless to affect micritic matrix.http://dx.doi.org/10.1155/2022/3851806
spellingShingle Yijun Wang
Hongming Tang
Guang Yang
Zhenyu Wang
Yunfeng Zhang
Lei Chen
The Evolutionary Characteristics of Lower Permian Keziliqiman Reefs in the Southwest Margin of Tarim Basin, Northwest China
Geofluids
title The Evolutionary Characteristics of Lower Permian Keziliqiman Reefs in the Southwest Margin of Tarim Basin, Northwest China
title_full The Evolutionary Characteristics of Lower Permian Keziliqiman Reefs in the Southwest Margin of Tarim Basin, Northwest China
title_fullStr The Evolutionary Characteristics of Lower Permian Keziliqiman Reefs in the Southwest Margin of Tarim Basin, Northwest China
title_full_unstemmed The Evolutionary Characteristics of Lower Permian Keziliqiman Reefs in the Southwest Margin of Tarim Basin, Northwest China
title_short The Evolutionary Characteristics of Lower Permian Keziliqiman Reefs in the Southwest Margin of Tarim Basin, Northwest China
title_sort evolutionary characteristics of lower permian keziliqiman reefs in the southwest margin of tarim basin northwest china
url http://dx.doi.org/10.1155/2022/3851806
work_keys_str_mv AT yijunwang theevolutionarycharacteristicsoflowerpermiankeziliqimanreefsinthesouthwestmarginoftarimbasinnorthwestchina
AT hongmingtang theevolutionarycharacteristicsoflowerpermiankeziliqimanreefsinthesouthwestmarginoftarimbasinnorthwestchina
AT guangyang theevolutionarycharacteristicsoflowerpermiankeziliqimanreefsinthesouthwestmarginoftarimbasinnorthwestchina
AT zhenyuwang theevolutionarycharacteristicsoflowerpermiankeziliqimanreefsinthesouthwestmarginoftarimbasinnorthwestchina
AT yunfengzhang theevolutionarycharacteristicsoflowerpermiankeziliqimanreefsinthesouthwestmarginoftarimbasinnorthwestchina
AT leichen theevolutionarycharacteristicsoflowerpermiankeziliqimanreefsinthesouthwestmarginoftarimbasinnorthwestchina
AT yijunwang evolutionarycharacteristicsoflowerpermiankeziliqimanreefsinthesouthwestmarginoftarimbasinnorthwestchina
AT hongmingtang evolutionarycharacteristicsoflowerpermiankeziliqimanreefsinthesouthwestmarginoftarimbasinnorthwestchina
AT guangyang evolutionarycharacteristicsoflowerpermiankeziliqimanreefsinthesouthwestmarginoftarimbasinnorthwestchina
AT zhenyuwang evolutionarycharacteristicsoflowerpermiankeziliqimanreefsinthesouthwestmarginoftarimbasinnorthwestchina
AT yunfengzhang evolutionarycharacteristicsoflowerpermiankeziliqimanreefsinthesouthwestmarginoftarimbasinnorthwestchina
AT leichen evolutionarycharacteristicsoflowerpermiankeziliqimanreefsinthesouthwestmarginoftarimbasinnorthwestchina