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Materials Science for Structural Geology (Record no. 25171)

000 -LEADER
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003 - CONTROL NUMBER IDENTIFIER
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005 - DATE AND TIME OF LATEST TRANSACTION
control field 20140310152340.0
007 - PHYSICAL DESCRIPTION FIXED FIELD--GENERAL INFORMATION
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008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION
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020 ## - INTERNATIONAL STANDARD BOOK NUMBER
International Standard Book Number 9789400755451
978-94-007-5545-1
050 #4 - LIBRARY OF CONGRESS CALL NUMBER
Classification number QE351-399.2
082 04 - DEWEY DECIMAL CLASSIFICATION NUMBER
Classification number 549
Edition number 23
264 #1 -
-- Dordrecht :
-- Springer Netherlands :
-- Imprint: Springer,
-- 2013.
912 ## -
-- ZDB-2-EES
100 1# - MAIN ENTRY--PERSONAL NAME
Personal name Paterson, Mervyn S.
Relator term author.
245 10 - IMMEDIATE SOURCE OF ACQUISITION NOTE
Title Materials Science for Structural Geology
Medium [electronic resource] /
Statement of responsibility, etc by Mervyn S. Paterson.
300 ## - PHYSICAL DESCRIPTION
Extent XIV, 247 p. 36 illus.
Other physical details online resource.
440 1# - SERIES STATEMENT/ADDED ENTRY--TITLE
Title Springer Geochemistry/Mineralogy,
International Standard Serial Number 2194-3176
505 0# - FORMATTED CONTENTS NOTE
Formatted contents note From the Contents: The Nature of Rocks and Minerals as Materials -- Thermodynamics -- Rate Processes -- Mechanical Fundamentals – Macroscopic -- Deformation Mechanisms - Atomic Transfer Flow -- Deformation Mechanisms - Crystal Plasticity -- Deformation Mechanisms - Granular Flow.
520 ## - SUMMARY, ETC.
Summary, etc This book sets out the basic materials science needed for understanding the plastic deformation of rocks and minerals.  Although at atmospheric pressure or at relatively low environmental pressures, these materials tend to be brittle, that is, to fracture with little prior plastic deformation when non-hydrostatically stressed, they can undergo substantial permanent strain when stressed under environmental conditions of high confining pressure and high temperature, such as occur geologically in the Earth’s crust and upper mantle.  Thus the plastic deformation of rocks and minerals is of fundamental interest in structural geology and geodynamics.  In mountain-building processes and during convective stirring in the Earth’s mantle, rocks can undergo very large amounts of plastic flow, accompanied by substantial changes in microstructure.  These changes in microstructure remain in the rocks as evidence of the past deformation history.  There are a number of types of physical processes whereby rock and minerals can undergo deformation under geological conditions.  The physics of these processes is set out in this book.
650 #0 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name as entry element Geography.
Topical term or geographic name as entry element Geology.
Topical term or geographic name as entry element Mineralogy.
Topical term or geographic name as entry element Thermodynamics.
Topical term or geographic name as entry element Earth Sciences.
Topical term or geographic name as entry element Mineralogy.
Topical term or geographic name as entry element Geology.
Topical term or geographic name as entry element Thermodynamics.
710 2# - ADDED ENTRY--CORPORATE NAME
Corporate name or jurisdiction name as entry element SpringerLink (Online service)
773 0# - HOST ITEM ENTRY
Title Springer eBooks
776 08 - ADDITIONAL PHYSICAL FORM ENTRY
Display text Printed edition:
International Standard Book Number 9789400755444
856 40 - ELECTRONIC LOCATION AND ACCESS
Uniform Resource Identifier http://dx.doi.org/10.1007/978-94-007-5545-1
942 ## - ADDED ENTRY ELEMENTS (KOHA)
Source of classification or shelving scheme
Item type E-Book
Copies
Price effective from Permanent location Date last seen Not for loan Date acquired Source of classification or shelving scheme Koha item type Damaged status Lost status Withdrawn status Current location Full call number
2014-04-09AUM Main Library2014-04-09 2014-04-09 E-Book   AUM Main Library549

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