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Depositional And Diagenetic Controls On Porosity Evolution In The C Zone Red River Formation Upper Ordovician Divide County North Dakota
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Book Synopsis Depositional and Diagenetic Controls on Porosity Evolution in the "C" Zone, Red River Formation (Upper Ordovician), Divide County, North Dakota by : Jon Steven Fox
Download or read book Depositional and Diagenetic Controls on Porosity Evolution in the "C" Zone, Red River Formation (Upper Ordovician), Divide County, North Dakota written by Jon Steven Fox and published by . This book was released on 1993 with total page 622 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis Miscellaneous Series - North Dakota Geological Survey by :
Download or read book Miscellaneous Series - North Dakota Geological Survey written by and published by . This book was released on 1996 with total page 710 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Download or read book Miscellaneous Series written by and published by . This book was released on 1957 with total page 388 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis Depositional and Paragenetic Controls on Porosity Development, Upper Red River Formation, North Dakota by : W. Kipp Carroll
Download or read book Depositional and Paragenetic Controls on Porosity Development, Upper Red River Formation, North Dakota written by W. Kipp Carroll and published by . This book was released on 1978 with total page 306 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis Williston Basin Horizontal Red River Play by : Scott L. Montgomery
Download or read book Williston Basin Horizontal Red River Play written by Scott L. Montgomery and published by . This book was released on 1996 with total page 82 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis Bibliography of the Geology of North Dakota, 1980-1993 by : Larry Greenwood
Download or read book Bibliography of the Geology of North Dakota, 1980-1993 written by Larry Greenwood and published by . This book was released on 1996 with total page 386 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis Summary of Investigations - the Saskatchewan Geological Survey by : Saskatchewan Geological Survey
Download or read book Summary of Investigations - the Saskatchewan Geological Survey written by Saskatchewan Geological Survey and published by . This book was released on 2001 with total page 150 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Download or read book Petroleum Abstracts written by and published by . This book was released on 1986 with total page 1674 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis Innovative Applications of Petroleum Technology in the Rocky Mountain Area by : Edward B. Coalson
Download or read book Innovative Applications of Petroleum Technology in the Rocky Mountain Area written by Edward B. Coalson and published by . This book was released on 1997 with total page 264 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis The Relationship of Diagenesis to Porosity Development and Pore Geometry in the Red River Formation (upper Ordovician), Cabin Creek Field, Montana by : Kenneth Ruzyla
Download or read book The Relationship of Diagenesis to Porosity Development and Pore Geometry in the Red River Formation (upper Ordovician), Cabin Creek Field, Montana written by Kenneth Ruzyla and published by . This book was released on 1980 with total page 200 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis Stratigraphic and Diagenetic Controls on the Occurrence of Porosity in the Mississippian Mission Canyon Formation in the Billings Nose Area, North Dakota by : Daniel Edward Beaber
Download or read book Stratigraphic and Diagenetic Controls on the Occurrence of Porosity in the Mississippian Mission Canyon Formation in the Billings Nose Area, North Dakota written by Daniel Edward Beaber and published by . This book was released on 1989 with total page 172 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis Deposition and Diagenesis of the Upper Red River Formation (Upper Fort Garry Member) and Stony Mountain Formation (Upper Ordovician), North and West of Winnipeg, Manitoba by : Garnet Cecil Grant Wallace
Download or read book Deposition and Diagenesis of the Upper Red River Formation (Upper Fort Garry Member) and Stony Mountain Formation (Upper Ordovician), North and West of Winnipeg, Manitoba written by Garnet Cecil Grant Wallace and published by . This book was released on 1979 with total page 0 pages. Available in PDF, EPUB and Kindle. Book excerpt: The upper Ordovician (Richmondian) upper Red River and Stony Mountain Formations were studied in detail from drill core and quarry exposures at Headingley, Stonewall and Stony Mountain, Manitoba. The stratigraphy, depositional history and diagenetic alterations were documented for the upper portion of the Fort Garry Member (Red River Formation) and the Gunn, Penitentiary, Gunton and Williams Member (Stony Mountain Formation). The upper Fort Garry was deposited in a low to high energy tidal flat setting characterized by clean carbonate sedimentation. Following a period of subaerial exposure at the end of Fort Garry time the Gunn Member was deposited. Sedimentation during Gunn time took place in a shallow marine environment characterized by low energy conditions, an influx of terrigenous material and the development of low-relief mud banks ... Diagenetic processes such as; borings, burrowing, the development of Phase I cements, some secondary porosity, eearly (primary) dolomite, authigenic feldspar, length slow chalcedony and some pyrite occurred relatively early in the diagenetic history of the sediments in the eogenetic to shallow mesogenetic environments. The development of chert, some pyrite and hematite, Phase II cement, neomorphic spar, secondary dolomite, and some secondary stylolites occurred later in the diagenetic history of the sediments in the mesogenetic environment. The development of Phase III cement, some secondary porosity and some hematite occurred in the telogenetic environment and represent the last diagenetic processes to occur.
Book Synopsis Depositional and Diagenetic Controls on Porosity Distribution and Development, Norphlet Formation, Offshore Alabama Region by : David Bentley Markham
Download or read book Depositional and Diagenetic Controls on Porosity Distribution and Development, Norphlet Formation, Offshore Alabama Region written by David Bentley Markham and published by . This book was released on 1991 with total page 580 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis Depositional and Diagenetic Controls on the Distribution of Porosity in the Lower Cretaceous Fall River Sandstone, Southern Powder River Basin, Wyoming by : Greg P. Anderson
Download or read book Depositional and Diagenetic Controls on the Distribution of Porosity in the Lower Cretaceous Fall River Sandstone, Southern Powder River Basin, Wyoming written by Greg P. Anderson and published by . This book was released on 1993 with total page 460 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis Depositional and Diagenetic Controls on Reservoir Quality and Their Petrophysical Predictors Within the Upper Cretaceous (Cenomanian) Doe Creek Member of the Kaskapau Formation at Valhalla Field, Northwest Alberta by : Nathaniel H. Ball
Download or read book Depositional and Diagenetic Controls on Reservoir Quality and Their Petrophysical Predictors Within the Upper Cretaceous (Cenomanian) Doe Creek Member of the Kaskapau Formation at Valhalla Field, Northwest Alberta written by Nathaniel H. Ball and published by . This book was released on 2009 with total page 0 pages. Available in PDF, EPUB and Kindle. Book excerpt: Valhalla Field, discovered in 1979 and located in northwest Alberta, produces from the Upper Cretaceous Doe Creek Member of the Kaskapau Formation. Original reserves in place are 44 x 106m3 of oil, of which 10.3 x 106m3 of oil (82% of recoverable reserves) have been produced (ERCB, 2008). This study evaluates the depositional and diagenetic controls on reservoir quality within the Doe Creek at Valhalla Field in order to identify reservoir-prone facies and predict their distribution in wells lacking core. Analysis of core and well log data indicates that intervals of highest reservoir quality are preferentially associated with thin (meter-scale) sandstone bodies deposited in proximal lower and upper shoreface environments. Based upon the relationships of facies to deep resistivity, mud content as gamma-ray derived shale volume, and density-neutron porosity separation within cemented zones, a well log transform was created that successfully predicts the distribution of reservoir-prone facies and calcite cement.
Book Synopsis The Deposition and Diagenesis of the Bluell Zone, Upper Mission Canyon Formation (Mississippian), Flaxton Field, Burke County, North Dakota by : Dirk Anson Schwartz
Download or read book The Deposition and Diagenesis of the Bluell Zone, Upper Mission Canyon Formation (Mississippian), Flaxton Field, Burke County, North Dakota written by Dirk Anson Schwartz and published by . This book was released on 1987 with total page 492 pages. Available in PDF, EPUB and Kindle. Book excerpt:
Book Synopsis Depositional Environment, Diagenesis and Reservoir Quality of the Middle Bakken Member in the Williston Basin, North Dakota by : Oguzhan Ayhan
Download or read book Depositional Environment, Diagenesis and Reservoir Quality of the Middle Bakken Member in the Williston Basin, North Dakota written by Oguzhan Ayhan and published by . This book was released on 2016 with total page 638 pages. Available in PDF, EPUB and Kindle. Book excerpt: The Upper Devonian-Lower Mississippian Bakken Formation in the Williston Basin is an important source rock for oil production in North America. The Bakken Formation is comprised of three units: Upper and Lower Bakken black shales and Middle Bakken Member. Upper and Lower Bakken shales are high quality source rocks which source reservoirs in the Middle Bakken, Upper Three Forks and lower Lodgepole Formations. The Middle Bakken Member, consisting of predominantly gray, silty and sandy dolostone, is under investigation in this study. The goals of this study are to determine the regional distribution of lithofacies and depositional environments of the Middle Bakken Member and explain diagenetic sequence and reservoir quality parameters in the Williston Basin. The reservoir quality of the Middle Bakken Member is mainly influenced by mineralogical composition and cementation resulting in low porosity and permeability and linked to lithofacies distribution in the basin. Dolomitization is pervasive throughout the unit, and also occurs as dolomite cement. Moreover, cementation occurred including quartz overgrowths, K-felspar, clay cement and pyrite as both cement and nodules. Not only dolomitization but also pyrite cementation plays an important role in reducing pore space in the reservoir. The pore types that were identified are intergranular, intragranular, fracture and moldic pores. Secondary intragranular porosity generally resulted from dissolution of biogenic fragments and dissolution of other unstable minerals including feldspar and dolomite. In this study, five lithofacies and one sandy interval within lithofacies C were described throughout the North Dakota portion of the Williston basin. The sandy interval in Lithofacies C was interpreted as bars or channel fills, which differentiates this study from previous studies in terms of core description. N-S, W-E, NE-SW, NW-SE oriented cross-sections drawn via cores suggest that the lithofacies of the Middle Bakken Member pinch out towards the edges. However, the anticlines in the basin affect their thickness distributions. Sandy interval in Lithofacies C reaches its thickest succession in the center of the basin. Lithofacies C and D consist of up to 80% of dolomite although the other lithofacies consist of relatively lower dolomite (up to 65%). While well logs indicate 4-8% of porosity, point-counting results show up to 5% of porosity. The sequence of diagenetic events in the North Dakota portion of the Williston Basin is from youngest to oldest: micritization, mechanical and chemical compaction, calcite cementation, dolomitization, pyrite cementation, microcrystalline quartz cementation, syntaxial calcite overgrowth, quartz overgrowth, K-Feldspar overgrowth, dolomite dissolution, feldspar dissolution, dedolomitization, fracturing, anhydrite cementation and hydrocarbon migration.
