Sedimentology [electronic resource] : Process and Product /

The origin, dispersal, deposition and burial of natural sediment grains is the central concern of sedimentology. The subject is truly inter­ disciplinary, commands the attention of Earth scientists, is of consider­ able interest to fluid dynamicists and civil engineers, and it finds widespread practical applications in industry. Sedimentology may be approached from two viewpoints: a descrip­ tive approach, as exemplified by traditional petrography and facies analysis, and a quantitative approach through the physical and chemical sciences. Both approaches are complementary and must be used in tandem if the recent remarkable progress in the field is to be sustained. This text aims to introduce such a combined approach to senior undergraduate students, graduate students and to interested professional Earth scientists. Thus the many descriptive diagrams in the text are counterbalanced by the use of basic physical and chemical reasoning through equations. I have tried to construct a text that follows logically on from the origin of sediment grains through fluid flow, transport, deposition and diagenesis (the change from sediment to rock). The text has been written assuming that some basic previous instruction has been given in the Earth sciences and in general physics and chemistry. Certain important derivations are given in appendices. I have avoided advanced mathematical treatment since it is my opinion that recogni­ tion of the basic physical or chemical basis to a problem is more important to the student than the formal mathematical reduction of poorly gathered data. As T. H.

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Bibliographic Details
Main Authors: Leeder, M. R. author., SpringerLink (Online service)
Format: Texto biblioteca
Language:eng
Published: Dordrecht : Springer Netherlands, 1982
Subjects:Earth sciences., Sedimentology., Earth Sciences.,
Online Access:http://dx.doi.org/10.1007/978-94-009-5986-6
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id KOHA-OAI-TEST:221464
record_format koha
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.
Sedimentology.
Earth Sciences.
Sedimentology.
Earth sciences.
Sedimentology.
Earth Sciences.
Sedimentology.
spellingShingle Earth sciences.
Sedimentology.
Earth Sciences.
Sedimentology.
Earth sciences.
Sedimentology.
Earth Sciences.
Sedimentology.
Leeder, M. R. author.
SpringerLink (Online service)
Sedimentology [electronic resource] : Process and Product /
description The origin, dispersal, deposition and burial of natural sediment grains is the central concern of sedimentology. The subject is truly inter­ disciplinary, commands the attention of Earth scientists, is of consider­ able interest to fluid dynamicists and civil engineers, and it finds widespread practical applications in industry. Sedimentology may be approached from two viewpoints: a descrip­ tive approach, as exemplified by traditional petrography and facies analysis, and a quantitative approach through the physical and chemical sciences. Both approaches are complementary and must be used in tandem if the recent remarkable progress in the field is to be sustained. This text aims to introduce such a combined approach to senior undergraduate students, graduate students and to interested professional Earth scientists. Thus the many descriptive diagrams in the text are counterbalanced by the use of basic physical and chemical reasoning through equations. I have tried to construct a text that follows logically on from the origin of sediment grains through fluid flow, transport, deposition and diagenesis (the change from sediment to rock). The text has been written assuming that some basic previous instruction has been given in the Earth sciences and in general physics and chemistry. Certain important derivations are given in appendices. I have avoided advanced mathematical treatment since it is my opinion that recogni­ tion of the basic physical or chemical basis to a problem is more important to the student than the formal mathematical reduction of poorly gathered data. As T. H.
format Texto
topic_facet Earth sciences.
Sedimentology.
Earth Sciences.
Sedimentology.
author Leeder, M. R. author.
SpringerLink (Online service)
author_facet Leeder, M. R. author.
SpringerLink (Online service)
author_sort Leeder, M. R. author.
title Sedimentology [electronic resource] : Process and Product /
title_short Sedimentology [electronic resource] : Process and Product /
title_full Sedimentology [electronic resource] : Process and Product /
title_fullStr Sedimentology [electronic resource] : Process and Product /
title_full_unstemmed Sedimentology [electronic resource] : Process and Product /
title_sort sedimentology [electronic resource] : process and product /
publisher Dordrecht : Springer Netherlands,
publishDate 1982
url http://dx.doi.org/10.1007/978-94-009-5986-6
work_keys_str_mv AT leedermrauthor sedimentologyelectronicresourceprocessandproduct
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spelling KOHA-OAI-TEST:2214642018-07-30T23:59:24ZSedimentology [electronic resource] : Process and Product / Leeder, M. R. author. SpringerLink (Online service) textDordrecht : Springer Netherlands,1982.engThe origin, dispersal, deposition and burial of natural sediment grains is the central concern of sedimentology. The subject is truly inter­ disciplinary, commands the attention of Earth scientists, is of consider­ able interest to fluid dynamicists and civil engineers, and it finds widespread practical applications in industry. Sedimentology may be approached from two viewpoints: a descrip­ tive approach, as exemplified by traditional petrography and facies analysis, and a quantitative approach through the physical and chemical sciences. Both approaches are complementary and must be used in tandem if the recent remarkable progress in the field is to be sustained. This text aims to introduce such a combined approach to senior undergraduate students, graduate students and to interested professional Earth scientists. Thus the many descriptive diagrams in the text are counterbalanced by the use of basic physical and chemical reasoning through equations. I have tried to construct a text that follows logically on from the origin of sediment grains through fluid flow, transport, deposition and diagenesis (the change from sediment to rock). The text has been written assuming that some basic previous instruction has been given in the Earth sciences and in general physics and chemistry. Certain important derivations are given in appendices. I have avoided advanced mathematical treatment since it is my opinion that recogni­ tion of the basic physical or chemical basis to a problem is more important to the student than the formal mathematical reduction of poorly gathered data. As T. H.One The Origin of Sediment Grains -- Theme -- 1 The origin of terriginous clastic grains -- 2 The origin of calcium carbonate grains -- 3 Evaporites, biogenic silica, and phosphates -- 4 Grain properties -- Two Fluid Flow and Sediment Transport -- Theme -- 5 Fluid properties and fluid motion -- 6 Transport of sediment grains -- 7 Sediment gravity flows -- Three Bedforms and Sedimentary Structures -- Theme -- 8 Bedforms and structures in granular sediments -- 9 Bedforms caused by erosion of cohesive sediment -- 10 Biogenic and organo-sedimentary structures -- 11 Soft sediment deformation structures -- Four Environmental and Facies Analysis -- Theme -- 12 Environmental and fades analysis -- Five Continental Environments and Facies Analysis -- Theme -- 13 Deserts -- 14 Alluvial fans -- 15 River plains -- 16 Lakes -- 17 Glacial environments -- Six Coastal and Shelf Environments and Facies Analysis -- Theme -- 18 Physical processes of coast and shelf -- 19 Deltas -- 20 Estuaries -- 21 ‘Linear’ clastic shorelines -- 22 Clastic shelves -- 23 Carbonate-evaporite shorelines, shelves and basins -- Seven Oceanic Environments and Facies Analysis -- Theme -- 24 Oceanic processes -- 25 Clastic oceanic environments -- 26 Pelagic oceanic sediments -- Eight Diagenesis: Sediment Into Rock -- Theme -- 27 Diagenesis: general considerations -- 28 Terrigenous clastic sediments -- 29 Carbonate sediments -- 30 Evaporites, silica, iron and manganese -- 31 Hydrocarbons -- References.The origin, dispersal, deposition and burial of natural sediment grains is the central concern of sedimentology. The subject is truly inter­ disciplinary, commands the attention of Earth scientists, is of consider­ able interest to fluid dynamicists and civil engineers, and it finds widespread practical applications in industry. Sedimentology may be approached from two viewpoints: a descrip­ tive approach, as exemplified by traditional petrography and facies analysis, and a quantitative approach through the physical and chemical sciences. Both approaches are complementary and must be used in tandem if the recent remarkable progress in the field is to be sustained. This text aims to introduce such a combined approach to senior undergraduate students, graduate students and to interested professional Earth scientists. Thus the many descriptive diagrams in the text are counterbalanced by the use of basic physical and chemical reasoning through equations. I have tried to construct a text that follows logically on from the origin of sediment grains through fluid flow, transport, deposition and diagenesis (the change from sediment to rock). The text has been written assuming that some basic previous instruction has been given in the Earth sciences and in general physics and chemistry. Certain important derivations are given in appendices. I have avoided advanced mathematical treatment since it is my opinion that recogni­ tion of the basic physical or chemical basis to a problem is more important to the student than the formal mathematical reduction of poorly gathered data. As T. H.Earth sciences.Sedimentology.Earth Sciences.Sedimentology.Springer eBookshttp://dx.doi.org/10.1007/978-94-009-5986-6URN:ISBN:9789400959866