Paleocurrents and Basin Analysis [electronic resource] /

In the past, interest in sedimentary structures has arisen mainly from the expectation that these features might be a guide to the environment of depo­ sition. But many sedimentary structures have also proved useful in determining stratigraphic order in nonfossiliferous, steeply inclined beds especially in Pre­ cambrian terranes. As the sequence problem has been reviewed at length by Shrock, it seemed to us, therefore, that the time is now ripe for a new look at sedimentary structures, not with respect to "top and bottom," but with reference to "fore and aft. " Much of the present-day interest in these structures stems from their usefulness in mapping of paleocurrents. A stage has been reached where there is need for a work which assembles, digests, and organizes our collective knowledge of the usefulness of directional properties of sediments and their application to basin analysis. This we have attempted to write. The desirability and need for such a book occurred to both of us independently. Upon discovering our mutual interest, we decided that a better book could be written by collaboration. Fortunately this collaboration became a reality because of support by the Guggenheim Foundation of one of us and the cooperation and support of The Johns Hopkins University of both of us. We acknowledge with thanks this indispensable aid.

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Main Authors: Potter, Paul Edwin. author., Pettijohn, F. J. author., SpringerLink (Online service)
Format: Texto biblioteca
Language:eng
Published: Berlin, Heidelberg : Springer Berlin Heidelberg : Imprint: Springer, 1963
Subjects:Earth sciences., Geology., Earth Sciences.,
Online Access:http://dx.doi.org/10.1007/978-3-662-01020-4
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spelling KOHA-OAI-TEST:1767982018-07-30T22:55:25ZPaleocurrents and Basin Analysis [electronic resource] / Potter, Paul Edwin. author. Pettijohn, F. J. author. SpringerLink (Online service) textBerlin, Heidelberg : Springer Berlin Heidelberg : Imprint: Springer,1963.engIn the past, interest in sedimentary structures has arisen mainly from the expectation that these features might be a guide to the environment of depo­ sition. But many sedimentary structures have also proved useful in determining stratigraphic order in nonfossiliferous, steeply inclined beds especially in Pre­ cambrian terranes. As the sequence problem has been reviewed at length by Shrock, it seemed to us, therefore, that the time is now ripe for a new look at sedimentary structures, not with respect to "top and bottom," but with reference to "fore and aft. " Much of the present-day interest in these structures stems from their usefulness in mapping of paleocurrents. A stage has been reached where there is need for a work which assembles, digests, and organizes our collective knowledge of the usefulness of directional properties of sediments and their application to basin analysis. This we have attempted to write. The desirability and need for such a book occurred to both of us independently. Upon discovering our mutual interest, we decided that a better book could be written by collaboration. Fortunately this collaboration became a reality because of support by the Guggenheim Foundation of one of us and the cooperation and support of The Johns Hopkins University of both of us. We acknowledge with thanks this indispensable aid.1. Introduction -- 2. History of Paleocurrent Investigations -- 3. Fabrics and Geophysical Properties -- 4. Cross-Bedding and Ripple Marks -- 5. Linear Structures -- 6. Deformational Structures -- 7. Internal Directional Structures and Shape of Sedimentary Bodies -- 8. Dispersal and Current Systems -- 9. Basin Analysis and the Sedimentary Model -- 10. Methods of Study -- Author Index -- Formation Index -- Plate captions -- The Plates.In the past, interest in sedimentary structures has arisen mainly from the expectation that these features might be a guide to the environment of depo­ sition. But many sedimentary structures have also proved useful in determining stratigraphic order in nonfossiliferous, steeply inclined beds especially in Pre­ cambrian terranes. As the sequence problem has been reviewed at length by Shrock, it seemed to us, therefore, that the time is now ripe for a new look at sedimentary structures, not with respect to "top and bottom," but with reference to "fore and aft. " Much of the present-day interest in these structures stems from their usefulness in mapping of paleocurrents. A stage has been reached where there is need for a work which assembles, digests, and organizes our collective knowledge of the usefulness of directional properties of sediments and their application to basin analysis. This we have attempted to write. The desirability and need for such a book occurred to both of us independently. Upon discovering our mutual interest, we decided that a better book could be written by collaboration. Fortunately this collaboration became a reality because of support by the Guggenheim Foundation of one of us and the cooperation and support of The Johns Hopkins University of both of us. We acknowledge with thanks this indispensable aid.Earth sciences.Geology.Earth Sciences.Geology.Springer eBookshttp://dx.doi.org/10.1007/978-3-662-01020-4URN:ISBN:9783662010204
institution COLPOS
collection Koha
country México
countrycode MX
component Bibliográfico
access En linea
En linea
databasecode cat-colpos
tag biblioteca
region America del Norte
libraryname Departamento de documentación y biblioteca de COLPOS
language eng
topic Earth sciences.
Geology.
Earth Sciences.
Geology.
Earth sciences.
Geology.
Earth Sciences.
Geology.
spellingShingle Earth sciences.
Geology.
Earth Sciences.
Geology.
Earth sciences.
Geology.
Earth Sciences.
Geology.
Potter, Paul Edwin. author.
Pettijohn, F. J. author.
SpringerLink (Online service)
Paleocurrents and Basin Analysis [electronic resource] /
description In the past, interest in sedimentary structures has arisen mainly from the expectation that these features might be a guide to the environment of depo­ sition. But many sedimentary structures have also proved useful in determining stratigraphic order in nonfossiliferous, steeply inclined beds especially in Pre­ cambrian terranes. As the sequence problem has been reviewed at length by Shrock, it seemed to us, therefore, that the time is now ripe for a new look at sedimentary structures, not with respect to "top and bottom," but with reference to "fore and aft. " Much of the present-day interest in these structures stems from their usefulness in mapping of paleocurrents. A stage has been reached where there is need for a work which assembles, digests, and organizes our collective knowledge of the usefulness of directional properties of sediments and their application to basin analysis. This we have attempted to write. The desirability and need for such a book occurred to both of us independently. Upon discovering our mutual interest, we decided that a better book could be written by collaboration. Fortunately this collaboration became a reality because of support by the Guggenheim Foundation of one of us and the cooperation and support of The Johns Hopkins University of both of us. We acknowledge with thanks this indispensable aid.
format Texto
topic_facet Earth sciences.
Geology.
Earth Sciences.
Geology.
author Potter, Paul Edwin. author.
Pettijohn, F. J. author.
SpringerLink (Online service)
author_facet Potter, Paul Edwin. author.
Pettijohn, F. J. author.
SpringerLink (Online service)
author_sort Potter, Paul Edwin. author.
title Paleocurrents and Basin Analysis [electronic resource] /
title_short Paleocurrents and Basin Analysis [electronic resource] /
title_full Paleocurrents and Basin Analysis [electronic resource] /
title_fullStr Paleocurrents and Basin Analysis [electronic resource] /
title_full_unstemmed Paleocurrents and Basin Analysis [electronic resource] /
title_sort paleocurrents and basin analysis [electronic resource] /
publisher Berlin, Heidelberg : Springer Berlin Heidelberg : Imprint: Springer,
publishDate 1963
url http://dx.doi.org/10.1007/978-3-662-01020-4
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