Origin, diagenesis, and petrophysics of clay minerals in sandstones
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SEPM , Tulsa, Okla
Sandstone -- Congresses., Clay minerals -- Congre
|Statement||edited by David W. Houseknecht and Edward D. Pittman.|
|Series||Special publication ;, no. 47, Special publication (SEPM (Society for Sedimentary Geology)) ;, no. 47.|
|Contributions||Houseknecht, David W., Pittman, Edward D., Clay Minerals Society.|
|LC Classifications||QE471.15.S25 O75 1992|
|The Physical Object|
|Pagination||282 p. :|
|LC Control Number||93135221|
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Origin, Diagenesis, and Petrophysics of Clay Minerals in Sandstone–This volume grew out of a symposium held at the 27th Annual Meeting of the Clay Minerals Society in Columbia.
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Origin, Diagenesis, and Petrophysics of Clay Minerals in Sandstones. Sepm Special Publication No. 47 by David W. Houseknecht and Edward D. Pitman, ; No. of pages: Author: J.
Marshall. The symposium was designed to present a current synthesis of research devoted to the origin, diagenesis and petrophysics of clay minerals in sandstones. International authors demonstrate a multidisciplinary approach to interpreting the origin and diagenesis of clay minerals in sandstones and to evaluating their influence on reservoir quality.
Origin, diagenesis, and petrophysics of clay minerals in sandstones / edited by David W. Houseknecht and Edward D.
Pittman SEPM Tulsa, Okla Australian/Harvard Citation Pittman, Edward D. & Houseknecht, David W. & Clay Minerals Society (U. S.). Clay minerals are one of the most important groups of minerals that destroy permeability in sandstones.
However, they also react with drilling and completion fluids and induce fines migration during hydrocarbon production.
They are a very complex family of minerals that are routinely intergrown with each other, contain a wide range of solid solutions and form by a variety of processes under a.
Depositional, Infiltrated and Authigenic Clays in Fluvial Sandstones of the Jurassic Sergi Formation, Rec??ncavo Basin, northeastern Brazil In book: Origin, Diagenesis, and Petrophysics of. Sandstone Diagenesis: The Evolution of Sand to Stone burial diagenetic cementation in sandstones.
The clay mineral assemblages in of clay-mineral diagenesis are used to reconstruct the. This paper addresses the origin, distribution pattern and burial diagenetic evolution of clay minerals in sandstone: kaolin, smectite, illite, chlorite, berthierine, glauconite and mixed-layer illite–smectite and chlorite–smectite.
Description. Special Publication 47 This volume grew out of a symposium held at the 27th Annual Meeting of the Clay Minerals Society in Columbia, Missouri, during October, The symposium was designed to present a current synthesis of research devoted to the origin, diagenesis, and petrophysics of clay minerals in sandstones.
Provenance interpretation, in particular, can be severely affected by diagenetic processes that selectively remove feldspars, heavy minerals, or rock fragments by intrastratal solution. Diagenesis may also play an extremely important role in postdepositional modification of porosity, causing either decrease in porosity as a result of compaction and cementation or increase in porosity owing to Cited by: 1.
The Mexico Gulf Coast drill sites illustrate clay diagenesis with depth of burial, involving mainly the illite-to-smectite transition and becoming active when overburden exceeds 2 km thickness. The Galapagos spreading center documents the case of glauconite-like minerals developed from illite-smectite in Cited by: 7.
The study reveals that the diagenesis of sandstones includes compaction, dissolution, and formation of carbonate minerals, siliceous minerals and clay dsc-sports.com: James J.
Howard. Origin, diagenesis, and petrophysics of clay minerals in sandstones. David W Houseknecht; Edward D Pittman; Clay Minerals Society. Based on a symposium held at the 27th Annual Meeting of the Clay Minerals Society in Columbia, Missouri, during October, Clay minerals in Atokan deep-water sandstone facies.
The controls on various clay minerals are addressed and a variety of geochemical issues, including the importance of mass flux, links to carbonate mineral diagenesis and linked clay mineral diagenesis in interbedded mudstone-sandstone are explored.
Feb 28, · Clay minerals in North Sea sandstones In Origin, Diagenesis and Petrophysics of Clay Minerals in Sandstones, SEPM, Special Publication, 37, 65– Google Scholar Boles, J.R., Summary This paper addresses the origin, distribution pattern and burial diagenetic evolution of clay minerals in Clay Minerals in Sandstones: Controls on Formation, Distribution and Evolution.
Worden Adding oil to a sandstone stops clay diagenesis if the sandstone is oil‐wet but probably only slows clay reactions if the Cited by: Pollastro, R.M., and Schenk, C.J. Origin and diagenesis of clay minerals in relation to sandstone paragenesis: An example in eolian dune reservoirs and associated rocks, Permian upper part of the Minnelusa Formation, Powder River basin, Wyoming.
A common characteristic of late burial is alteration of clay minerals into mica, and development of well-crystallized phyllosilicate minerals in general. DIAGENESIS OF SANDSTONES 99 For this reason this late episode of diagenesis is termed thephyllomorphic stage.l Certain other minerals, particularly feldspar, appear as authigenic growths Cited by: A systematic study of 71 samples of sandstones and conglomerates of the Itabapoana Formation (Aptian), selected from the cores of 13 wells in the offshore portion of Campos Basin, eastern Brazil, allowed the recognition of the main primary and diagenetic constituents and pore types, and their space and time dsc-sports.com by: 9.
Origin, Diagenesis, and Petrophysics of Clay Minerals in Sandstones (SPECIAL PUBLICATION (SOCIETY OF ECONOMIC PALEONTOLOGISTS AND MINERALOGISTS)) by David W. Houseknecht and Edward D. Pitman | Oct 1, May 28, · Moraes M A S and De Ros L F.
Depositional, infiltrated and authigenic clays in fluvial sandstones of the Jurassic Sergi Formation, Reconcavo Basin, Northeast Brazil. In: Origin, Diagenesis and Petrophysics of Clay Minerals in Sandstones, Society of Economic Paleontologists and Mineralogists Special Publication.
Clay Miner. 19, – Kisch, H.J. () Mineralogy and petrology of burial diagenesis (burial metamorphism) and incipient metamorphism in clastic rocks.
– in: Diagenesis in Cited by: Clay Mineral Cements in Sandstones. Additional Information. How to Cite. Marfil, R., Delgado, A., Rossi, C., Iglesia, A.
Details Origin, diagenesis, and petrophysics of clay minerals in sandstones EPUB
and Ramseyer, K. () Origin and Diagenetic Evolution of Kaolin in Reservoir Sandstones and Associated Shales of the Jurassic and Cretaceous, Salam Field, Western Desert (Egypt), in Clay Mineral Cements in Sandstones.
Clay mineral phases differ frequently between the pre-MSC Qawasim and MSC Abu Madi sandstones, and their spatio-temporal distribution is likely controlled by the depositional and burial conditions.
Kaolinite is the most common authigenic clay in the pre-MSC Qawasim facies; whereas chlorite is only abundant in the MSC Abu Madi dsc-sports.com: Mahmoud Leila.
binding energy of the clay minerals, and (2) subsequent rearrangement of ions in the clay mineral to produce illitc. It is finally proposed that diagenesis of clay minerals is character- ized by the addition to and incorporation into them of Me ions, such as Mg, K, Ca, Na.
Diagenesis affects all sediments after their deposition and includes a fundamental suite of physical, chemical and biological processes that control the texture, mineralogy and fluid-flow properties of sedimentary rocks.
Understanding the processes and products of diagenesis is thus a critical component in the analysis of the evolution of sedimentary basins, and has practical implications for. Composition and diagenesis. Composition affects sandstone diagenesis in two ways. The higher the quartz content, the greater the mechanical stability (less compaction occurs).; The higher the variety of minerals, the lower the chemical stability (more cementation or dissolution occurs).
Mar 17, · The readership of this volume will include sedimentologists and petrographers who deal with the occurrence, spatial and temporal distribution patterns and importance of clay mineral cements in sandstones, geochemists involved in unraveling the factors that control clay mineral cement formation in sandstones and petroleum geoscientists involved.
Jan 20, · The Chang7 and Chang6 sandstones in the southwestern Ordos basin are the typical tight oil sandstones in China. Pore textures and their genetic classes of secondary porosity were studied in detail using a combination of optical petrography, SEM and dsc-sports.com by:.
Online shopping for Clay - Mineralogy from a great selection at Books Store. Advanced Chemical Methods for Soil and Clay Minerals Research: Proceedings of the NATO Advanced Study Institute held at the University of Illinois, July 23 – August 4, Origin, Diagenesis, and Petrophysics of Clay Minerals in Sandstones Oct 1 by.Clay Mineralogy books held on reserve winter term at the UGA Science library.
This is by no means an exhaustive list of books on clays. Your best bet is to go to the library stacks and "cruise" the QE, QE and TN sections.Development of a tight gas reservoir by a multiple fracced horizontal well: Ameland, the Netherlands. Houseknecht, D.W. & E.D.
Description Origin, diagenesis, and petrophysics of clay minerals in sandstones EPUB
Pittman (eds) Origin, dia genesis and petrophysics of clay minerals in sandstones — Soc. Econ. Paleont. D.W. & E.D. Pittman (eds) Origin, diagenesis and petrophysics of clay minerals in sandstones — Soc Cited by: 5.
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