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3 edition of Carbonate diagenesis as a control on stratigraphic traps (with examples from the Williston Basin) found in the catalog.

Carbonate diagenesis as a control on stratigraphic traps (with examples from the Williston Basin)

Mark W. Longman

Carbonate diagenesis as a control on stratigraphic traps (with examples from the Williston Basin)

originally presented at the American Association of Petroleum Geologists Fall Education Conference, Calgary, Canada 1981

by Mark W. Longman

  • 30 Want to read
  • 6 Currently reading

Published by AAPG in Tulsa .
Written in English

    Subjects:
  • Geology, Stratigraphic.,
  • Rocks, Carbonate.,
  • Diagenesis.,
  • Porosity.

  • Edition Notes

    Bibliography: p. 149-158.

    StatementMark W. Longman.
    SeriesEducation course note series -- 21, AAPG continuing education course note series -- #21.
    ContributionsAmerican Association of Petroleum Geologists.
    Classifications
    LC ClassificationsQE40 .A4 no. 21
    The Physical Object
    Paginationvii, 159 p. :
    Number of Pages159
    ID Numbers
    Open LibraryOL22087611M
    ISBN 100891811702


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Carbonate diagenesis as a control on stratigraphic traps (with examples from the Williston Basin) by Mark W. Longman Download PDF EPUB FB2

Carbonate Diagenesis as a Control on Stratigraphic Traps, Mark W. Longman. Eucations Course Note Series No. 21 of the American Association of Petroleum Geologists, No. of pages: Price: U.S. $ (Soft cover) Carbonate Diagenesis as a Control on Stratigraphic Traps, Mark W.

Longman. Eucations Course Note. Carbonate diagenesis as a control on stratigraphic traps. Tulsa, Okla.: AAPG: AAPG Bookstore [distributor, ] (OCoLC) Material Type: Conference publication, Internet resource: Document Type: Book, Internet Resource: All Authors / Contributors: Mark W Longman.

Clyde H. Moore, William J. Wade, Summary of Early Diagenesis and Porosity Modification of Carbonate Reservoirs in a Sequence Stratigraphic and Climatic Framework, Carbonate Reservoirs - Porosity and Diagenesis in a Sequence Stratigraphic Framework, /B, Cited by: Book Title: CN Carbonate Diagenesis as a Control on Stratigraphic Traps (with Examples from the Williston Basin) Article/Chapter: Chapter 2.

Subject Group: Reservoirs--Carbonates. Spec. Pub. Type: Course Notes. Pub. Year: Author (s): Mark W. Longman. Text. Purchase Carbonate Reservoirs: Porosity, Evolution and Diagenesis in a Sequence Stratigraphic Framework, Volume 55 - 1st Edition.

Print Book & E-Book. ISBNPrice: $ It is thus impractical to contrast stratigraphic versus structural traps with the intention of searching for one type and not searching for the other. This is most clear in the case of carbonate traps where tectonism controls development of both erosional and depositional structure and affects depositional and diagenetic facies distribution.

About this book. Over the years, many papers on carbonate diagenesis have been published in Sedimentology, the journal of the International Association of Sedimentologists. This volume presents a collection of these papers with a commentary.

C.H. Moore. Elsevier, Apr 1, - Science - pages. 0 Reviews. Carbonate diagenesis is a subject of enormous complexity because of the basic chemical reactivity of carbonate minerals. These. Nonetheless, carbonate sediments proceed in a general way through the same diagenetic regimes as siliciclastic sediments.

That is, carbonate sediments go through early (shallow-burial), middle (deep-burial), and possibly late (uplift and unroofing) stages of diagenesis. The Finnmark carbonate platform underwent four distinct stages of depositional evolution.

Each of the four corresponding stratigraphic intervals (left margin of Fig. l) is characterized by a different style of diagenesis and porosity development, and is associated with a unique set of problems relevant to regional play potential and risk.

The initial chapters provide an overview of the carbonate sedimentologic system and the application of sequence stratigraphic concepts to carbonate rock sequences.

The nature of carbonate porosity and its control by diagenesis is explored. Porosity classification schemes are detailed, compared, and their utility s: 1.

Author: Andrew D. Horbury Publisher: Amer Assn of Petroleum Geologists ISBN: Size: MB Format: PDF, ePub, Mobi View: Get Books. Diagenesis And Basin Development eBook File: Book by Andrew D. Horbury, Diagenesis And Basin Development Books available in PDF, EPUB, Mobi Format. Download Diagenesis And Basin Development books.

Carbonate Reservoirs: Porosity, Evolution and Diagenesis in a Sequence Stratigraphic Framework: Porosity Evolution and Diagenesis in a Sequence Stratigraphic Framework (ISSN Book 55) - Kindle edition by Moore, Clyde H. Download it once and read it on your Kindle device, PC, phones or tablets.

Use features like bookmarks, note taking and highlighting while reading Carbonate Reservoirs: Porosity, Evolution and Diagenesis in a Sequence Stratigraphic Framework Reviews: 1. Collectively studies have shown that carbonate facies are commonly the product of processes that are active in their depositional setting.

Water depth, winds, waves, currents, temperature, water chemistry, and biologic action all affect the character of the carbonate formed.

Diagenesis, which also plays a major role in forming and modifying the facies that are found in the subsurface, are.

Sequence stratigraphic influence on regional diagenesis of a mixed carbonate-siliciclastic passive margin, Eocene, N.C., USA 81 BRIAN P. COFFEY Stratigraphic controls on the distribution of diagenetic processes, quality and heterogeneity of fluvial.

tion and diagenesis in a sequence stratigraphic frame- of the book include a detailed review of carbonate mineralogy, non-marine carbonate. Although carbonates make up only 20% of the sedimentary rock record, they account for more than 50% of the world's proven oil reserves.

Carbonates differ from siliclastics in generation, geomorphology, and diagenesis, all of which modify the mineralogy, porosity, and permeability so important to reservoir quality and 3-D seismic response. The first eight chapters establish the geologic. Diagenesis plays a considerable role in controlling the quality of a reservoir within a trap.

As discussed in Chapter 6, solution can enhance reservoir quality by generating secondary porosity, whereas cementation can destroy it. In some situations diagenesis can actually generate a hydrocarbon trap (Rittenhouse, ).

SUMMARY There are several simplistic models that can be used to summarize the observed variation in carbonate play types. The carbonate reservoirs that form stratigraphic traps may have lens-like, sheet-like or ribbon geometry.

carbonate bodies with lens-like geometries include biohermal or reef buildups that form during and after rapid relative sea level rises as well as down-slope debris fans. PSStratigraphic Traps: Quantitative Approach Based upon a Producing hydrodynamics, diagenesis, or other factors or a combination.

The prediction of stratigraphic traps relies on a good undestanding of complex geological High energy carbonate sand Organic buildup Carbonate foreslope P90= 43API.

The Rodessa Limestone (Aptian) produces from structural and combination traps in the East Texas basin. West Purt field, in northeastern Anderson County, is a Rodessa combination trap where porosity and permeability have been affected by hydrocarbon alteration, adding an additional complexity to.

The co-existence of K + - and NH 4 +-mica layers in mica–smectite was repeatedly evidenced in the context of burial diagenesis in the vicinity of source rocks. In addition to tobelite (NH 4 +-mica), paragonite, margarite, or aluminoceladonite may also occur in mica-containing mixed-layer contrasting layer-to-layer distance of these mica varieties (~~~and.

The mineralogy and textures of sedimentary carbonate rocks suggest two stages of diagenesis. The stabilization of skeletal fragments from aragonite, high magnesian calcite and calcite, to calcite is the first stage and generally pre-compactive grain fracture.

The formation of cements and consequent reduction in porosity is the second stage and is generally post compactive grain fracture. One of stratigraphic traps which formed associated with subsurface diagenesis is porous carbonate facies. This trap group could evolve locally and regionally.

The most common type is formed from the process dolomitisation where magnesium carbonate limestones deposited with less volume than the calcium carbonate replaced by a solution, resulting in porous and permeable rock.

Carbonate Microfabrics is the first attempt to bring together in one reference the application of microfabric analysis to the solution of problems in the fields of geology, geophysics and geotechnique.

This book, the result of a symposium and workshop on carbonate microfabrics, explores the relationship of microfabrics to fundamental properties and processes in carbonates. Stratigraphic trap A second major class of oil traps is the stratigraphic trap. It is related to sediment deposition or erosion and is bounded on one or more sides by zones of low permeability.

Because tectonics ultimately control deposition and erosion, however, few stratigraphic traps are completely without structural influence. The American Association of Petroleum Geologists is an international organization with o members in plus countries.

The purposes of this Association are to advance the science of geology. Sonic velocity in carbonate sediments and rocks Acoustic properties of carbonate rocks: use in quantitative interpretation of sonic and seismic measurements Carbonate seismic facies analysis Carbonate sequence stratigraphy and its application to hydrocarbon exploration and reservoir development @article{osti_, title = {Cycles and events in stratigraphy}, author = {Einsele, G and Ricken, W and Seilacher, A}, abstractNote = {This book reviews and discusses the most up-to-date knowledge in the fields of cyclostratigraphy and event stratigraphy.

The book contains 48 papers contributed by the most knowledgeable geologists and paleontologists in the fields of cycle and event. Stratigraphic problems are further aggravated by the prevalence of sedimentary gaps in the corresponding carbonate platform deposits simply due to their.

@article{osti_, title = {Trap and seal analysis in carbonate shelf margin stratigraphic trap exploration; example from the lower Miocene, Zhujiang Fm., Pearl River Mouth Basin, People's Republic of China}, author = {Chimney, P.J.

and Lomando, A.J. and Popek, J.P.}, abstractNote = {Carbonate shelf margin stratigraphic traps are a particularly risky play type because the same diagenetic. Cambridge Carbonates offer expertise in carbonate diagenesis, plus the description and interpretation of microfacies.

We produce diagenetic models which provide key results such as timing of fluid flow and evolution of reservoir properties throughout the entire diagenetic history. Resultant diagenetic models are useful to optimise the understanding of rock types. Oil and gas are stratigraphically trapped to the east against the Nemaha uplift, to the north by a regional wedge-out of Hunton strata, and by intraformational diagenetic traps.

Hunton Group reservoirs are the Bois d'Arc and Frisco Limestones, with lesser production from the Chimneyhill subgroup, Haragan Shale, and Henryhouse Formation. Most Influential Books In Carbonate Reservoirs.

C.H.,Carbonate Diagenesis and Porosity, Developments in Sedimentology Elsevier, New York, p. steep reverse, and low angle thrust faults. Stratigraphic traps include stratal terminations and diagenetic porosity pinch-outs.

Carbonate examples include the most abundant. Diagenesis may be critical for trap location; mineralogy and/or facies may control location of dissolution porosity Use sequence stratigraphy, hydrologic, or thermal maturity models. [1]. The initial chapters of this volume provide an overview of the carbonate sedimentologic system and the application of sequence stratigraphic concepts to carbonate rock sequences.

The nature of carbonate porosity and its control by diagenesis is explored. Porosity classification schemes are detailed, compared, and their utility examined. Sequence stratigraphy of carbonate ramps. Numerical forward modelling of carbonate systems.

Part 3 - Day 3 Early diagenesis of limestones; mineralogy, textures and porosity evolution. Dolomites and dolomitization. Late stage diagenesis of limestones and dolomites. Environments and trends in diagenesis. Carbonate Sequence Stratigraphy Although most of this website focuses on shallow-marine siliciclastic systems, sequence analysis can be just as readily applied to carbonate systems.

Carbonates have several aspects that make their response to relative sea-level changes and the character of their sequence stratigraphic elements somewhat different.

This comprehensive text and accompanying CD-ROM will provide the reader with an integrated overview of diagenesis and porosity evolution in carbonate petroleum reservoirs and ancient carbonate rock sequences.

The initial chapters of this volume provide an overview of the carbonate sedimentologic system and the application of sequence stratigraphic concepts to carbonate rock sequences. Diagenesis and reservoir quality of the Upper Mississippian Aux Vases Sandstone, Illinois Basin / Janet K.

Pitman, Mitchell Henry, and Hannes Leetaru. — U.S. Geological Survey professional paper ; ) Includes bibliographical references. Geology, Stratigraphic—Mississippian. Diagenesis—Illinois Basin. Seismic investigations provide a vital tool for the delineation of subtle hydrocarbon traps, and they are the basis for understanding the regional basin framework and the stratigraphic subdivision.

Seismic stratigraphy combines two very different scales of observation: the seismic and well control.Plays in this basin result from both structural and stratigraphic traps and occur in primarily Permian and then have superimposed structural control on these stratigraphic traps.

porosity limited by burial diagenesis. Heterogeneous carbonate reservoirs in the Phosphoria are productive (about 7 .Assess the role of mechanical stratigraphy and stress conditions on fracture and fault formation in carbonate and shale strata. Evaluate deformation mechanisms that operate in fault zones.

Evaluate complex structures like those that control hydrocarbon migration and trapping in carbonate petroleum provinces around the world.