Reactive transport modeling of early burial dolomitization of carbonate platforms by geothermal convection

FF Whitaker; Y. Xiao

doi:10.1306/12090909075

Reactive transport modeling of early burial dolomitization of carbonate platforms by geothermal convection

FF Whitaker, Y. Xiao

Research output: Contribution to journal › Article (Academic Journal) › peer-review

111 Citations (Scopus)

Abstract

Reaction transport models (RTMs) permit quantitative investigation of diagenesis and its effects on reservoir quality. The RTM TOUGHREACT is used to investigate diagenesis in an isolated platform driven by geothermal (‘Kohout’) convection of seawater, which has been invoked to explain dolomitisation during early burial. Previous short (0.1 Ma) RTM simulations suggested that convection can drive dolomitisation, mostly at >50°C, and anhydritisation, but complete dolomitisation requires >30-60 Ma. Our more extended RTM simulations (

Translated title of the contribution	Reaction transport modeling of geothermal convection: a viable mechanism for early burial dolomitisation of platform carbonates
Original language	English
Pages (from-to)	889 - 917
Journal	American Association of Petroleum Geologists Bulletin
Volume	94
Issue number	6
DOIs	https://doi.org/10.1306/12090909075
Publication status	Published - 2010

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title = "Reactive transport modeling of early burial dolomitization of carbonate platforms by geothermal convection",

abstract = "Reaction transport models (RTMs) permit quantitative investigation of diagenesis and its effects on reservoir quality. The RTM TOUGHREACT is used to investigate diagenesis in an isolated platform driven by geothermal ({\textquoteleft}Kohout{\textquoteright}) convection of seawater, which has been invoked to explain dolomitisation during early burial. Previous short (0.1 Ma) RTM simulations suggested that convection can drive dolomitisation, mostly at >50°C, and anhydritisation, but complete dolomitisation requires >30-60 Ma. Our more extended RTM simulations (",

author = "FF Whitaker and Y. Xiao",

year = "2010",

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AU - Whitaker, FF

AU - Xiao, Y.

PY - 2010

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AB - Reaction transport models (RTMs) permit quantitative investigation of diagenesis and its effects on reservoir quality. The RTM TOUGHREACT is used to investigate diagenesis in an isolated platform driven by geothermal (‘Kohout’) convection of seawater, which has been invoked to explain dolomitisation during early burial. Previous short (0.1 Ma) RTM simulations suggested that convection can drive dolomitisation, mostly at >50°C, and anhydritisation, but complete dolomitisation requires >30-60 Ma. Our more extended RTM simulations (

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DO - 10.1306/12090909075

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JO - American Association of Petroleum Geologists Bulletin

JF - American Association of Petroleum Geologists Bulletin

IS - 6

ER -

Reactive transport modeling of early burial dolomitization of carbonate platforms by geothermal convection

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