![Diagenesis and reservoir quality of the Sherwood Sandstone (Triassic), Corrib Field, Slyne Basin, west of Ireland [An article from: Marine and Petroleum Geology]](https://www.ebooknetworking.net/books/B00/0RR/bigB000RR0DT4.jpg)
Diagenesis and reservoir quality of the Sherwood Sandstone (Triassic), Corrib Field, Slyne Basin, west of Ireland [An article from: Marine and Petroleum Geology]
Book Details
Author(s)S. Schmid, R. Worden, Q. Fisher
PublisherElsevier
ISBN / ASINB000RR0DT4
ISBN-13978B000RR0DT2
AvailabilityAvailable for download now
MarketplaceUnited States 🇺🇸
Description
This digital document is a journal article from Marine and Petroleum Geology, published by Elsevier in 2004. The article is delivered in HTML format and is available in your Amazon.com Media Library immediately after purchase. You can view it with any web browser.
Description:
The Triassic Sherwood Sandstone in the Corrib Field, Slyne Basin west of Ireland on the European continental margin, is a dry gas reservoir with a Mercia mudstone top-seal. Petrographic analysis combined with X-ray diffraction, stable isotope, fluid inclusion and core analysis have been used to assess: timing of growth and origin of mineral cements, whether sandstone diagenesis involved mass flux, the controls on reservoir quality and how reservoir quality is likely to vary in more deeply buried sections. Depositional and early diagenetic characteristics of the Sherwood in Corrib are typical of a semi-arid fluvial environment, containing groundwater of meteoric origin. Early diagenesis included the development of copious dolomite cement, in the form of dolocrete, as well as the formation of abundant clay while less volumetrically important, grain-coating haematite and K-feldspar cement also grew. Burial diagenesis witnessed the initial growth of minor chlorite and albite. Quartz overgrowths and ankerite followed and are the most important burial cements growing over a temperature interval between 100 and 1165 ^oC. Albite commenced growth at about 90 ^oC, quartz cement at 100 ^oC and ankerite at 110 ^oC. These cements reached the zenith of their development at 105-110 ^oC for albite, 125-130 ^oC for quartz and 135-145 ^oC for ankerite. Siderite and anhydrite are relatively minor, late-stage cements. The formation water has been consistently highly saline during burial and, in terms of mineral cement-derived oxygen stable isotope values, is likely to be a diagenetically evolved version of the initial depositional water suggesting long-term stagnation of the pore-fluids. The diagenetic reactions that formed burial cements all seem to be essentially isochemical including the ankerite that has carbon isotope characteristics of the cannibalisation of dolocrete. Reservoir quality is mainly controlled by early diagenetic dolomite and clay although grain size is also important because only sandstones with >200 @mm grain size have >50md permeability. Both shallower and deeper sections than Corrib may have similar porosity and permeability since temperature-dependent diagenetic controls on reservoir quality, e.g. quartz and illite cement, are peripheral.
Description:
The Triassic Sherwood Sandstone in the Corrib Field, Slyne Basin west of Ireland on the European continental margin, is a dry gas reservoir with a Mercia mudstone top-seal. Petrographic analysis combined with X-ray diffraction, stable isotope, fluid inclusion and core analysis have been used to assess: timing of growth and origin of mineral cements, whether sandstone diagenesis involved mass flux, the controls on reservoir quality and how reservoir quality is likely to vary in more deeply buried sections. Depositional and early diagenetic characteristics of the Sherwood in Corrib are typical of a semi-arid fluvial environment, containing groundwater of meteoric origin. Early diagenesis included the development of copious dolomite cement, in the form of dolocrete, as well as the formation of abundant clay while less volumetrically important, grain-coating haematite and K-feldspar cement also grew. Burial diagenesis witnessed the initial growth of minor chlorite and albite. Quartz overgrowths and ankerite followed and are the most important burial cements growing over a temperature interval between 100 and 1165 ^oC. Albite commenced growth at about 90 ^oC, quartz cement at 100 ^oC and ankerite at 110 ^oC. These cements reached the zenith of their development at 105-110 ^oC for albite, 125-130 ^oC for quartz and 135-145 ^oC for ankerite. Siderite and anhydrite are relatively minor, late-stage cements. The formation water has been consistently highly saline during burial and, in terms of mineral cement-derived oxygen stable isotope values, is likely to be a diagenetically evolved version of the initial depositional water suggesting long-term stagnation of the pore-fluids. The diagenetic reactions that formed burial cements all seem to be essentially isochemical including the ankerite that has carbon isotope characteristics of the cannibalisation of dolocrete. Reservoir quality is mainly controlled by early diagenetic dolomite and clay although grain size is also important because only sandstones with >200 @mm grain size have >50md permeability. Both shallower and deeper sections than Corrib may have similar porosity and permeability since temperature-dependent diagenetic controls on reservoir quality, e.g. quartz and illite cement, are peripheral.
