Open thermal convection dolomitization: an example from East Yunnan (China)

Dolostones are widely developed in the middle Permian rocks of East Yunnan, China, mainly in the shoal-facies Maokou Formation. The previously reported dolostone formation mechanisms cannot explain the distribution and geochemical characteristics of these dolostones, in particular their strontium, m...

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Published inGeological magazine Vol. 158; no. 2; pp. 330 - 348
Main Authors Zhang, Jing-Qi, Jin, Zhen-Kui, Zhu, Xiao-Er, Li, Yang, Guo, Qi-Heng, Shi, Shu-Ting
Format Journal Article
LanguageEnglish
Published Cambridge, UK Cambridge University Press 01.02.2021
Subjects
Asia
carbonate rocks
carbonatization
Cellular convection
chemical composition
China
Computational fluid dynamics
Convection
Distribution
Dolomitization
Dolostone
Far East
Fault lines
Fluid flow
fluid inclusions
Fluids
Free convection
Geology
Geophysics
Global positioning systems
GPS
Heat flux
Heat transfer
Hydrocarbons
igneous and metamorphic rocks
inclusions
isotopes
Liangshan Formation
Limestone
Lower Permian
Magnesium
mantle
Mantle plumes
Maokou Formation
Mineral resources
Original Article
Oxygen isotopes
Paleozoic
Permian
petroleum
Petrology
Qixia Formation
Seawater
Sedimentary facies
sedimentary rocks
Shoals
solid Earth (tectonophysics)
stratigraphic units
Stratigraphy
Strontium
Strontium isotopes
Yunnan China
China
Yunnan China
dolostone
East Yunnan
dolomitization
middle Permian
thermal convection
Emei mantle plume
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Abstract Dolostones are widely developed in the middle Permian rocks of East Yunnan, China, mainly in the shoal-facies Maokou Formation. The previously reported dolostone formation mechanisms cannot explain the distribution and geochemical characteristics of these dolostones, in particular their strontium, magnesium and oxygen isotope signatures. To help predict the distribution of dolostone reservoirs and reduce the exploration risk and cost, this study proposes a new model of dolomitization: open thermal convection dolomitization. In this new dolomitization model, Mg2+ in dolomitizing fluids originates mostly from seawater, with a minor component coming from deep hydrothermal fluids. Elevated heat flux (in this case due to the nearby Emei mantle plume) causes spatial temperature variations in the fluid along the circulation flow pathways, resulting in fast and pervasive dolomitization of limestone. The proposed model not only explains the characteristics and distribution of dolostones in the study area but also serves as a reference for predicting the distribution of dolostones in other areas subjected to thermal convection.
AbstractList Abstract Dolostones are widely developed in the middle Permian rocks of East Yunnan, China, mainly in the shoal-facies Maokou Formation. The previously reported dolostone formation mechanisms cannot explain the distribution and geochemical characteristics of these dolostones, in particular their strontium, magnesium and oxygen isotope signatures. To help predict the distribution of dolostone reservoirs and reduce the exploration risk and cost, this study proposes a new model of dolomitization: open thermal convection dolomitization. In this new dolomitization model, Mg 2+ in dolomitizing fluids originates mostly from seawater, with a minor component coming from deep hydrothermal fluids. Elevated heat flux (in this case due to the nearby Emei mantle plume) causes spatial temperature variations in the fluid along the circulation flow pathways, resulting in fast and pervasive dolomitization of limestone. The proposed model not only explains the characteristics and distribution of dolostones in the study area but also serves as a reference for predicting the distribution of dolostones in other areas subjected to thermal convection.
Dolostones are widely developed in the middle Permian rocks of East Yunnan, China, mainly in the shoal-facies Maokou Formation. The previously reported dolostone formation mechanisms cannot explain the distribution and geochemical characteristics of these dolostones, in particular their strontium, magnesium and oxygen isotope signatures. To help predict the distribution of dolostone reservoirs and reduce the exploration risk and cost, this study proposes a new model of dolomitization: open thermal convection dolomitization. In this new dolomitization model, Mg2+ in dolomitizing fluids originates mostly from seawater, with a minor component coming from deep hydrothermal fluids. Elevated heat flux (in this case due to the nearby Emei mantle plume) causes spatial temperature variations in the fluid along the circulation flow pathways, resulting in fast and pervasive dolomitization of limestone. The proposed model not only explains the characteristics and distribution of dolostones in the study area but also serves as a reference for predicting the distribution of dolostones in other areas subjected to thermal convection.
Author Shi, Shu-Ting
Jin, Zhen-Kui
Zhu, Xiao-Er
Zhang, Jing-Qi
Li, Yang
Guo, Qi-Heng
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  organization: College of Geosciences, China University of Petroleum, Beijing 102249, China
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  organization: College of Geosciences, China University of Petroleum, Beijing 102249, China
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  fullname: Shi, Shu-Ting
  organization: College of Geosciences, China University of Petroleum, Beijing 102249, China
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Issue 2
Keywords dolostone
East Yunnan
dolomitization
middle Permian
thermal convection
Emei mantle plume
Language English
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SSID ssj0013088
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Snippet Dolostones are widely developed in the middle Permian rocks of East Yunnan, China, mainly in the shoal-facies Maokou Formation. The previously reported...
Abstract Dolostones are widely developed in the middle Permian rocks of East Yunnan, China, mainly in the shoal-facies Maokou Formation. The previously...
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geoscienceworld
cambridge
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Publisher
StartPage 330
SubjectTerms Asia
carbonate rocks
carbonatization
Cellular convection
chemical composition
China
Computational fluid dynamics
Convection
Distribution
Dolomitization
Dolostone
Far East
Fault lines
Fluid flow
fluid inclusions
Fluids
Free convection
Geology
Geophysics
Global positioning systems
GPS
Heat flux
Heat transfer
Hydrocarbons
igneous and metamorphic rocks
inclusions
isotopes
Liangshan Formation
Limestone
Lower Permian
Magnesium
mantle
Mantle plumes
Maokou Formation
Mineral resources
Original Article
Oxygen isotopes
Paleozoic
Permian
petroleum
Petrology
Qixia Formation
Seawater
Sedimentary facies
sedimentary rocks
Shoals
solid Earth (tectonophysics)
stratigraphic units
Stratigraphy
Strontium
Strontium isotopes
Yunnan China
Title Open thermal convection dolomitization: an example from East Yunnan (China)
URI https://www.cambridge.org/core/product/identifier/S0016756820000503/type/journal_article
https://pubs.geoscienceworld.org/geolmag/article/158/2/330/594383/Open-thermal-convection-dolomitization-an-example
https://www.proquest.com/docview/2479030189
Volume 158
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