Granite Genesis: In Situ Melting and Crustal Evolution (Record no. 61481)

MARC details
000 -LEADER
fixed length control field 06352nam a22004695i 4500
001 - CONTROL NUMBER
control field 978-1-4020-5891-2
003 - CONTROL NUMBER IDENTIFIER
control field DE-He213
005 - DATE AND TIME OF LATEST TRANSACTION
control field 20251006084527.0
007 - PHYSICAL DESCRIPTION FIXED FIELD--GENERAL INFORMATION
fixed length control field cr nn 008mamaa
008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION
fixed length control field 100301s2007 ne | s |||| 0|eng d
020 ## - INTERNATIONAL STANDARD BOOK NUMBER
International Standard Book Number 9781402058912
020 ## - INTERNATIONAL STANDARD BOOK NUMBER
International Standard Book Number 99781402058912
024 7# - OTHER STANDARD IDENTIFIER
Standard number or code 10.1007/978-1-4020-5891-2
Source of number or code doi
082 04 - DEWEY DECIMAL CLASSIFICATION NUMBER
Classification number 551
Edition information 23
100 1# - MAIN ENTRY--PERSONAL NAME
Personal name Chen, Guo-Neng.
Relator term author.
245 10 - TITLE STATEMENT
Title Granite Genesis: In Situ Melting and Crustal Evolution
Medium [electronic resource] /
Statement of responsibility, etc. by Guo-Neng Chen, Rodney Grapes.
264 #1 - PRODUCTION, PUBLICATION, DISTRIBUTION, MANUFACTURE, AND COPYRIGHT NOTICE
Place of production, publication, distribution, manufacture Dordrecht :
Name of producer, publisher, distributor, manufacturer Springer Netherlands,
Date of production, publication, distribution, manufacture, or copyright notice 2007.
300 ## - PHYSICAL DESCRIPTION
Other physical details online resource.
336 ## - CONTENT TYPE
Content type term text
Content type code txt
Source rdacontent
337 ## - MEDIA TYPE
Media type term computer
Media type code c
Source rdamedia
338 ## - CARRIER TYPE
Carrier type term online resource
Carrier type code cr
Source rdacarrier
347 ## - DIGITAL FILE CHARACTERISTICS
File type text file
Encoding format PDF
Source rda
505 0# - FORMATTED CONTENTS NOTE
Formatted contents note Preface -- Acknowledgements -- 1 Introduction -- 1.1 Rock genesis and its relationship to geosystems -- 1.2 Granites, migmatites and granite problems -- 2 Crustal melting: experiments and conditions -- 2.1 Introduction -- 2.2 Mineral melting -- 2.3 Rock melting - experimental evidence -- 2.4 Structure and composition of the crust -- 2.5 Water in the crust -- 2.6 Crustal heat and partial melting -- 3. In-situ melting and intracrustal convection: granite magma layers -- 3.1 Introduction -- 3.2 Crustal melting I: Initial melting and partial melt layer -- 3.3 Crustal melting II: Convection and formation of magma layer -- 3.4 Compositional variation within magma layer -- 3.5 Magma layer, granite layer and granite bodies -- 3.6 MI fluctuation (remelting) and granite sequence -- 3.7 Conclusion -- 4. Geological evidence for in-situ melting origin of granite layers -- 4.1 Migmatite to granite -- 4.2 Contact metamorphism -- 4.3 Xenoliths and mafic enclaves -- 4.4 Granite layer and granite exposures -- 4.5 Fluctuation of MI and downward younging granite sequence -- 5. Differentiation of magma layer: geochemical considerations -- 5.1 Introduction -- 5.2 Compositional variation -- 5.3 Strontium isotopes -- 5.4 Oxygen isotopes -- 5.5 Rare earth elements -- 5.6 Summary -- 6. Mineralisation related to in-situ granite formation -- 6.1 Introduction -- 6.2 Source of ore-forming elements -- 6.3 Formation and evolution of ore-bearing fluid -- 6.4 Types of mineral deposits -- 6.5 Age relationships -- 6.6 Temperature distribution -- 6.7 Formation and distribution of hydrothermal mineral deposits -- 6.8 Mineralised depth horizons -- 6.9 Mineralisation during elevated crustal temperatures -- 6.10 Mineralisation during granite remelting -- 6.11 Patterns of element redistribution and element fields -- 6.12 Summary -- 7. Heat source for crustal magma layers: tectonic models -- 7.1 Introduction -- 7.2 Crustal temperature disturbance related to plate convergence -- 7.3 Subduction and granite formation: western Pacific continental margin -- 7.4 Continental collision and granite formation: Tethys Belt -- 7.5 Concluding statement -- 8. Geological effects of crystallisation of a crustal granite magma layer: SE China -- 8.1 Fault-block basins -- 8.2. Volcanism -- 9. Material and element cycling of the continental crust and summary -- 9.1. Rock cycling of continental material -- 9.2. Element cycling of the continental crust -- 9.3. Overview -- References -- Appendix 1 map of SE China -- Appendix 2 Results of experimental rock melting -- Index .
520 ## - SUMMARY, ETC.
Summary, etc. Granitic rocks are a major component of the continental crust and the many and complex problems of their origin that have challenged geologists over some 200 years still are presenting challenges today. Current ideas of granite formation involve lower crustal melting, segregation, ascent (as dykes or diapirs) and emplacement in the upper crust. In this book we suggest an alternative model for the origin of granite in terms of in-situ meltingintracrustal convection that physically determines the process from partial melting of mid-upper crustal rocks to formation of a convecting magma layer. We illustrate the model using the geological, geochemical and geophysical studies from Australia, North and South America, Europe and China, and conclude that heat convection within a crustal partial melting layer is essential for formation of granite magma and that without convection, partial melting of rocks produces migmatites rather than granites. Granite is layer-like within the crust, and shape and size of granite bodies reflect the geometric relationship between an irregular upper surface of the crystallised magma layer and erosion surface. Repeated melting of the crust generates downward-younging granite sequences. Chemical and isotopic compositions of granites indicate differentiation within the magma rather than different deep sources. Of a number of proposed heat sources that can cause mid-upper crustal anatexis, large-scale crustal melting and formation of a granite magma layer is considered to be primarily related to plate convergence. A dynamic model with examples from the western Pacific continental margin in SE China and Tethys-Tibet is proposed to explain the relationship between plate convergence, granite and compressive deformation of the continental crust. Mineralisation related to granite formation, fault-block basins, formation of continental red beds and volcanism with examples from SE China, are also discussed in terms of the new model. In a final section, we suggest a new rock cycling model of the continental crust and the concept of Geochemical Fields of Elements, illustrating the unity between the microcosm and macrocosm of the natural world. Audience: This book will be of interest to scientists, researchers and students in geology, geophysics, geochemistry and economic geology.
650 #0 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element GEOCHEMISTRY.
650 #0 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element GEOLOGY.
650 #0 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element PHYSICAL GEOGRAPHY.
650 #0 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element MINERALOGY.
650 14 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element GEOSCIENCES.
650 24 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element GEOLOGY.
650 24 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element GEOPHYSICS/GEODESY.
650 24 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element GEOCHEMISTRY.
650 24 - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical term or geographic name entry element MINERALOGY.
700 1# - ADDED ENTRY--PERSONAL NAME
Personal name Grapes, Rodney.
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
Relationship information Printed edition:
International Standard Book Number 9781402058905
856 40 - ELECTRONIC LOCATION AND ACCESS
Uniform Resource Identifier <a href="http://dx.doi.org/10.1007/978-1-4020-5891-2">http://dx.doi.org/10.1007/978-1-4020-5891-2</a>
Public note Ver el texto completo en las instalaciones del CICY
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942 ## - ADDED ENTRY ELEMENTS (KOHA)
Source of classification or shelving scheme Dewey Decimal Classification
Koha item type Libros electrónicos
Holdings
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  Dewey Decimal Classification     Libro electrónico CICY CICY Libro electrónico 06.10.2025   551 06.10.2025 06.10.2025 Libros electrónicos