Diagenetic History of Eocene Wilcox Sandstones and Associated Formation Waters, South-Central Texas

Diagenetic History of Eocene Wilcox Sandstones and Associated Formation Waters, South-Central Texas PDF Author: Robert Stephen Fisher
Publisher:
ISBN:
Category : Diagenesis
Languages : en
Pages : 0

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Diagenetic History of Eocene Wilcox Sandstones and Associated Formation Waters, South-Central Texas

Diagenetic History of Eocene Wilcox Sandstones and Associated Formation Waters, South-Central Texas PDF Author: Robert Stephen Fisher
Publisher:
ISBN:
Category : Diagenesis
Languages : en
Pages : 0

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Diagenesis, II

Diagenesis, II PDF Author: G.V. Chilingarian
Publisher: Elsevier
ISBN: 0080869572
Category : Science
Languages : en
Pages : 279

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Book Description
Diagenesis is a highly developed, interdisciplinary field of study. It is reciprocal in that it borrows from numerous scientific or technological specialities and then, in turn, repays them with useful results. Too often, however, the information gained and concepts developed remain unintegrated instead of being utilized quickly by several related earth-science fraternities. This volume, the second of a multi-volume work, attempts to bring together such information, thereby assisting the individual and the research group in keeping up with the data explosion. There is no end in sight to diagenetic research because of its wide practical and intellectual appeals. Consequently, periodic reviews, such as presented in this volume, are greatly needed.

Provenance of Arenites

Provenance of Arenites PDF Author: G.G. Zuffa
Publisher: Springer Science & Business Media
ISBN: 9401728097
Category : Science
Languages : en
Pages : 404

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Proceedings of the NATO Advanced Study Institute on Reading Provenance from Arenites, Cetraro, Cosenza, Italy, June 3-11, 1984

Terrigenous Clastic Depositional Systems

Terrigenous Clastic Depositional Systems PDF Author: W. E. Galloway
Publisher: Springer Science & Business Media
ISBN: 146840170X
Category : Science
Languages : en
Pages : 423

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Book Description
The reserves, or extractable fraction, of the fuel-mineral endowment are sufficient to supply the bulk of the world's energy requirements for the immediately forseeable future-well into the next century according to even the most pessimistic predictions. But increasingly sophisticated exploration concepts and technology must be employed to maintain and, if possible, add to the reserve base. Most of the world's fuel-mineral resources are in sedimentary rocks. Any procedure or concept that helps describe, under stand, and predict the external geometry and internal attributes of major sedimentary units can therefore contribute to discovery and recovery of coal, uranium, and petroleum. While conceding the desirability of renewable and nonpolluting energy supply from gravitational, wind, or solar sources, the widespread deployment of these systems lies far in the future-thus the continued commercial emphasis on conventional nonrenewable fuel mineral resources, even though their relative significance will fluctuate with time. For example, a decade ago the progilostications for uranium were uniformly optimistic. But in the early 1980s the uranium picture is quite sombre, although unlikely to remain permanently depressed. Whether uranium soars to the heights of early expectations remains to be seen. Problems of waste disposal and public acceptance persist. Fusion reactors may ultimately eliminate the need for uranium in power generation, but for the next few decades there will be continued demand for uranium to fuel existing power plants and those that come on stream. This book is, to some extent, a hybrid.

Diagenesis and Burial History of the Lower Cretaceous Travis Peak Formation, East Texas

Diagenesis and Burial History of the Lower Cretaceous Travis Peak Formation, East Texas PDF Author: S. P. Dutton
Publisher:
ISBN:
Category : Diagenesis
Languages : en
Pages : 76

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Petrographic and geochemical studies were used to determine the diagenetic and burial history of Travis Peak sandstones in East Texas and to relate the diagenesis to permeability variations within the formation. Permeability in much of the formation has been reduced to less than 0.1 md by compaction, cementation and minor pressure solution. Travis peak sandstone is quartzarenite and subarkose, having an average composition Q95F4R1. The first authigenic cements to precipitate were illite, which coated detrital grains with tangentially oriented crystals, and dolomite. Next, extensive quartz cement, averaging 17% of the rock volume in well-sorted sandstone, occluded much of the primary porosity. Quartz is most abundant in the lower Travis Peak, in well-connected sandstone beds that were deposited in braided streams. Dissolution of orthoclase and albitization of plagioclase followed quartz cementation and occurred prior to mid-Cretaceous movement of the Sabine Uplift. Illite, chlorite, and ankerite precipitated after feldspar diagenesis. Oil migrated into Travis Peak reservoirs in the Late Cretaceous from Jurassic source rocks. Later deasphalting of the oil filled much of the remaining porosity in some zones near the top of the formation with reservoir bitumen.

Dissimilar Diagenetic Histories of Smackover Sandstones, Gulf of Mexico, U.S.A.

Dissimilar Diagenetic Histories of Smackover Sandstones, Gulf of Mexico, U.S.A. PDF Author: Stephen Irving Dworkin
Publisher:
ISBN:
Category : Diagenesis
Languages : en
Pages : 490

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Journal of Sedimentary Petrology

Journal of Sedimentary Petrology PDF Author:
Publisher:
ISBN:
Category : Petrology
Languages : en
Pages :

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Proceedings

Proceedings PDF Author: Brian Hitchon
Publisher:
ISBN:
Category : Hydrogeology
Languages : en
Pages : 298

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Petroleum Abstracts. Literature and Patents

Petroleum Abstracts. Literature and Patents PDF Author:
Publisher:
ISBN:
Category : Petroleum
Languages : en
Pages : 1528

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Depositional systems in the Sparta Formation (Eocene), Gulf Coast basin of Texas

Depositional systems in the Sparta Formation (Eocene), Gulf Coast basin of Texas PDF Author: José Ulises Ricoy
Publisher:
ISBN:
Category : Facies (Geology)
Languages : en
Pages : 196

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