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Metasomatism and the Chemical Transformation of Rock (Record no. 24673)

000 -LEADER
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003 - CONTROL NUMBER IDENTIFIER
control field OSt
005 - DATE AND TIME OF LATEST TRANSACTION
control field 20140310152331.0
007 - PHYSICAL DESCRIPTION FIXED FIELD--GENERAL INFORMATION
fixed length control field cr nn 008mamaa
008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION
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020 ## - INTERNATIONAL STANDARD BOOK NUMBER
International Standard Book Number 9783642283949
978-3-642-28394-9
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 -
-- Berlin, Heidelberg :
-- Springer Berlin Heidelberg :
-- Imprint: Springer,
-- 2013.
912 ## -
-- ZDB-2-EES
100 1# - MAIN ENTRY--PERSONAL NAME
Personal name Harlov, Daniel E.
Relator term author.
245 10 - IMMEDIATE SOURCE OF ACQUISITION NOTE
Title Metasomatism and the Chemical Transformation of Rock
Medium [electronic resource] :
Remainder of title The Role of Fluids in Terrestrial and Extraterrestrial Processes /
Statement of responsibility, etc by Daniel E. Harlov, Håkon Austrheim.
300 ## - PHYSICAL DESCRIPTION
Extent VI, 806 p. 285 illus., 164 illus. in color.
Other physical details online resource.
440 1# - SERIES STATEMENT/ADDED ENTRY--TITLE
Title Lecture Notes in Earth System Sciences,
International Standard Serial Number 2193-8571
505 0# - FORMATTED CONTENTS NOTE
Formatted contents note 1.  Metasomatism and the chemical transformation of rock: Rock-mineral-fluid interaction in terrestrial and extraterrestrial environments. -2. The Chemical Composition of Metasomatic Fluids in the Crust -- 3. Thermodynamic modeling and thermobarometry of metasomatized rocks -- 4. Structural controls of metasomatism on a regional scale -- 5. Mechanisms of metasomatism and metamorphism on the local mineral scale: The role of dissolution-reprecipitation during mineral re-equilibration. - 6. Geochronology of metasomatic events.-7. Effects of metasomatism on mineral systems and their host rocks: alkali metasomatism, skarns, greisens, tourmalinites, rodingites, black-wall alteration and listevenites -- 8. Metasomatism within the ocean crust -- 9. Metasomatism in subduction zones of subducted oceanic slabs, mantle wedges, and the slab-mantle interface -- 10. Metasomatism during High-Pressure Metamorphism: Eclogites and Blueschist-Facies Rocks -- 11. Prograde, peak and retrograde metamorphic fluids and associated metasomatism in upper amphibolite to granulite facies transition zones -- 12.  Mantle Metasomatism -- 13.   Mapping the distribution of fluids in the crust and lithospheric mantle utilizing geophysical methods -- 14. A Hydromechanical Model for Lower Crustal Fluid Flow -- 15. Metasomatism in the early solar sysem: The record fron Chondritic meteorites.
520 ## - SUMMARY, ETC.
Summary, etc Fluid-aided mass transfer and subsequent mineral re-equilibration are the two defining features of metasomatism and must be present in order for metamorphism to occur. Coupled with igneous and tectonic processes, metasomatism has played a major role in the formation of the Earth’s continental and oceanic crust and lithospheric mantle as well as in their evolution and subsequent stabilization. Metasomatic processes can include ore mineralization, metasomatically induced alteration of oceanic lithosphere, mass transport in and alteration of subducted oceanic crust and overlying mantle wedge, which has subsequent implications regarding mass transport, fluid flow, and volatile storage in the lithospheric mantle overall, as well as both regional and localized crustal metamorphism. Metasomatic alteration of accessory minerals such as zircon or monazite can allow for the dating of metasomatic events as well as give additional information regarding the chemistry of the fluids responsible. Lastly present day movement of fluids in both the lithospheric mantle and deep to mid crust can be observed utilizing geophysical resources such as electrical resistivity and seismic data. Such observations help to further clarify the picture of actual metasomatic processes as inferred from basic petrographic, mineralogical, and geochemical data. The goal of this volume is to bring together a diverse group of geologists, each of whose specialities and long range experience regarding one or more aspects of metasomatism during geologic processes, should allow them to contribute to a series of review chapters, which outline the basis of our current understanding of how metasomatism influences and helps to control both the evolution and stability of the crust and lithospheric mantle.
650 #0 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name as entry element Geography.
Topical term or geographic name as entry element Geochemistry.
Topical term or geographic name as entry element Physical geography.
Topical term or geographic name as entry element Mineralogy.
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 Geochemistry.
Topical term or geographic name as entry element Geophysics/Geodesy.
700 1# - ADDED ENTRY--PERSONAL NAME
Personal name Austrheim, Håkon.
Relator term author.
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 9783642283932
856 40 - ELECTRONIC LOCATION AND ACCESS
Uniform Resource Identifier http://dx.doi.org/10.1007/978-3-642-28394-9
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
2014-04-08AUM Main Library2014-04-08 2014-04-08 E-Book   AUM Main Library549
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