Shelf sands and sandstones. Edited by R. John Knight and J. Ross McLean

Cover of: Shelf sands and sandstones.  Edited by R. John Knight and J. Ross McLean |

Published by Canadian Society of Petroleum Geologists in Calgary .

Written in English

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Subjects:

  • Rocks, Sedimentary,
  • Sedimentology

Edition Notes

11

Book details

ContributionsKnight, R.J., McLean, J.R.
Classifications
LC ClassificationsQE 471.15 S25S5 1986
The Physical Object
Pagination347 p.
Number of Pages347
ID Numbers
Open LibraryOL22052847M

Download Shelf sands and sandstones. Edited by R. John Knight and J. Ross McLean

Shelf Sands and Sandstones (Canadian Society of Petroleum Geologists, Memoir 11) Hardcover – January 1, by R. John Knight (Editor), J.

Ross McLean (Editor) See all formats and editions Hide other formats and editions. Price New from Used from Hardcover "Please retry" $ — Format: Hardcover.

Generation of Late Holocene Sand Ridges on the Middle Continental Shelf of New Jersey, USA—Evidence for Formation in a Mid‐Shelf Setting Based on Comparisons with a Nearshore Ridge (Pages: ).

Shelf sands and sandstone reservoirs are among the more poorly understood types of sandstones. Continental, shoreline and deep water sandstones have all been studied in much more depth than have shelf sands and sandstones. However, during the last fifteen years significant progress has been made in understanding shelf sands and by: Shelf Sands and Sandstone Reservoirs Hardcover – January 1, by R.G.

Walker Organized, Compiled and Edited by R.W. Tillman, D.J.P. Swift (Author) See all formats and editions Hide other formats and editionsAuthor: R.G. Walker Organized, Compiled and Edited by R.W.

Tillman, D.J.P. Swift. Shelf sands and sandstone reservoirs are among the more poorly understood types of sandstones. Continental, shoreline and deep water sandstones have all been studied in much more depth than have shelf sands and sandstones. However, during the last fifteen years significant progress has been made in understanding shelf sands and sandstones.

Shelf sands and sandstone reservoirs. Tulsa, Okla.: Society of Economic Paleontologists and Mineralogists, © (OCoLC) Document Type: Book: All Authors / Contributors: Donald J P Swift; Roderick W Tillman; Roger G Walker; Society of Economic Paleontologists and Mineralogists.

Shareable Link. Use the link below to share a full-text version of this article with your friends and colleagues. Learn more. The main framework of the first edition has been retained so that the reader can begin with the mineralogy and textural properties of sands and sandstones, progress through their organization and classification and their study as a body of rock, to consideration of their origin-prove­ nance, transportation, deposition, and lithification-and finally to their place in the stratigraphic column and the.

Swift, Donald J. & SEPM (Society for Sedimentary Geology). Shelf sand and sandstone bodies: geometry, facies, and sequence stratigraphy / edited by D.J.P. Swift [et al.] Blackwell Scientific Publicatons Oxford ; Melbourne.

PDF | On Jan 1,J.W. Snedden and others published Isolated shallow marine sand bodies: Deposits for all interpretations. In: Isolated Shallow Marine Sand Bodies: Sequence Stratigraphic. Home > Browse Collections > CSPG Special Publications > Book/Publication Shelf Sands and Sandstones — Memoir CSPG Special Publications.

Abstract Shelf Sands and Sandstones — Mem Pages vii-viii. Acknowledgements. John Knight, J. Ross McLean. View the First Page. A text abstract of this article is not available. The first. The Radków and Szczeliniec sandstones: an example of giant foresets on a tectonically controlled shelf of the Bohemian Cretaceous Basin (Central Europe) / T.

Jerzykiewicz and J. Wojewoda --Association of sand with mud deposits accumulating on Continental Shelves / C. Nittrouer [and others] --The Holocene shelf sediment wedge off the south.

In this chapter we summarize the facies assemblages, vertical profiles and architecture, and the autocyclic mechanisms that control deposition in the various clastic and chemical sedimentary. Response of the shelf floor, in Knight, R.J. and McLean, J.R., eds., Shelf Sands and Sandstones: Canadian Society of Petroleum Geologists Mem p.

– The main framework of the first edition has been retained so that the reader can begin with the mineralogy and textural properties of sands and sandstones, progress through their organization and 5/5(2). mudstone-rich slope deposits and sandstone-rich shelf margin to outer-shelf deltaic de- posited by the first sand-rich shelf-margin del- Welsink, H.J., Dwyer, J.D., and Knight, R.J., For comparison, I have added R.L.

Folk’s classification of terrigenous sandstones (from Folk,Petrology of Sedimentary Rocks). In this scheme, sand-dominated rocks and sediments carrying less than 15% matrix are called arenites; those with 15. You can write a book review and share your experiences. Other readers will always be interested in your opinion of the books you've read.

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Laboratory test results are presented and show that the material may range from sand to moderately weak rock. Microfabric analysis suggests that depositional and diagenetic processes have as much an influence on this variability as does weathering. A means of estimating the material shear strength of the weakest.

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In the current circumstances, we have decided to formalise some of. The sandstone is meaning sedimentary rocks which have the size rate between 1/16 until 2 mm. The size that is called sand can be very rough until the smallest one is very fine. Sandstone have the moderate grain size, not too rough like pebble, granule, cobble or boulder but not too fine like silt or clay.

So, there is easier to form the sand. Sedimentary rock - Sedimentary rock - Classification of sandstones: There are many different systems of classifying sandstones, but the most commonly used schemes incorporate both texture (the presence and amount of either interstitial matrix—i.e., clasts with diameters finer than millimetre—or chemical cement) and mineralogy (the relative amount of quartz and the relative abundance.

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Unfettered II: Ne. Sandstones. Sandstones are siliciclastic sedimentary rocks that consist mainly of sand-size grains (clast diameters from 2 to 1 / 16 millimetre) either bonded together by interstitial chemical cement or lithified into a cohesive rock by the compaction of the sand-size framework component together with any interstitial primary (detrital) and secondary (authigenic) finer-grained matrix component.

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As you can see, it’s not. TIGHT GAS SANDSTONE RESERVOIRS, PART 2: PETROPHYSICAL ANALYSIS AND RESERVOIR MODELING 15 W.R. Moore1, Y. Zee Ma1, I. Pirie1, Y. Zhang2 Schlumberger, Denver, CO, USA1; University of Wyoming, Laramie, WY, USA2 INTRODUCTION We discuss petrophysical analysis of wireline logs, methods for formation evaluation and issues in.

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