Field Geology of High-Grade Gneiss Terrains [electronic resource] /

Field Geology of High-Grade Gneiss Terrains [electronic resource] /

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Although there are numerous publications on the geology of high-grade gneiss terrains, few descriptions exist of how to map and carry out structural analysis in these terrains. Textbooks on structural geology concentrate on technIques appli­ cable to low-grade terrains. Geologists who have no experience of mapping high-grade gneisses are often at a loss as to how to apply techniques to high­ grade rocks that were developed for low to medium grade metamorphic terrains. Any study of deep crustal processes and their development through time should begin with examination of the primary data source - outcrops of high­ grade metamorphic terrains. We feel that the urge to apply advanced techniques of fabric analysis, petrology, geochemistry, isotope geochemistry and age deter­ mination to these rocks often results in brief sampling trips in which there is little, if any analysis of the structural and metamorphic history revealed by outcrop patterns. Many studies of the metamorphic petrology and geochemistry of high-grade gneiss terrains make ineffective use of available field data, often because the authors are unaware of structural complexities and of the ways to recognise and use them. This is unfortunate, because much data can be collected in the field at minimal cost that cannot easily, if at all, be obtained from material in the laboratory. The primary igneous or sedimentary nature of a rock, the relative age of intrusive veins, and the sequence of deformation that they under­ went, can usually best be determined by straightforward observation in the field.

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Main Authors: Passchier, Cees W. author., Myers, John Stuart. author., Kröner, Alfred. author., SpringerLink (Online service)
Format: Texto biblioteca
Language:eng
Published: Berlin, Heidelberg : Springer Berlin Heidelberg, 1990
Subjects:Earth sciences., Geochemistry., Geology., Mineralogy., Earth Sciences.,
Online Access:http://dx.doi.org/10.1007/978-3-642-76013-6
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id KOHA-OAI-TEST:218336
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.
Geochemistry.
Geology.
Mineralogy.
Earth Sciences.
Geology.
Geochemistry.
Mineralogy.
Earth sciences.
Geochemistry.
Geology.
Mineralogy.
Earth Sciences.
Geology.
Geochemistry.
Mineralogy.
spellingShingle Earth sciences.
Geochemistry.
Geology.
Mineralogy.
Earth Sciences.
Geology.
Geochemistry.
Mineralogy.
Earth sciences.
Geochemistry.
Geology.
Mineralogy.
Earth Sciences.
Geology.
Geochemistry.
Mineralogy.
Passchier, Cees W. author.
Myers, John Stuart. author.
Kröner, Alfred. author.
SpringerLink (Online service)
Field Geology of High-Grade Gneiss Terrains [electronic resource] /
description Although there are numerous publications on the geology of high-grade gneiss terrains, few descriptions exist of how to map and carry out structural analysis in these terrains. Textbooks on structural geology concentrate on technIques appli­ cable to low-grade terrains. Geologists who have no experience of mapping high-grade gneisses are often at a loss as to how to apply techniques to high­ grade rocks that were developed for low to medium grade metamorphic terrains. Any study of deep crustal processes and their development through time should begin with examination of the primary data source - outcrops of high­ grade metamorphic terrains. We feel that the urge to apply advanced techniques of fabric analysis, petrology, geochemistry, isotope geochemistry and age deter­ mination to these rocks often results in brief sampling trips in which there is little, if any analysis of the structural and metamorphic history revealed by outcrop patterns. Many studies of the metamorphic petrology and geochemistry of high-grade gneiss terrains make ineffective use of available field data, often because the authors are unaware of structural complexities and of the ways to recognise and use them. This is unfortunate, because much data can be collected in the field at minimal cost that cannot easily, if at all, be obtained from material in the laboratory. The primary igneous or sedimentary nature of a rock, the relative age of intrusive veins, and the sequence of deformation that they under­ went, can usually best be determined by straightforward observation in the field.
format Texto
topic_facet Earth sciences.
Geochemistry.
Geology.
Mineralogy.
Earth Sciences.
Geology.
Geochemistry.
Mineralogy.
author Passchier, Cees W. author.
Myers, John Stuart. author.
Kröner, Alfred. author.
SpringerLink (Online service)
author_facet Passchier, Cees W. author.
Myers, John Stuart. author.
Kröner, Alfred. author.
SpringerLink (Online service)
author_sort Passchier, Cees W. author.
title Field Geology of High-Grade Gneiss Terrains [electronic resource] /
title_short Field Geology of High-Grade Gneiss Terrains [electronic resource] /
title_full Field Geology of High-Grade Gneiss Terrains [electronic resource] /
title_fullStr Field Geology of High-Grade Gneiss Terrains [electronic resource] /
title_full_unstemmed Field Geology of High-Grade Gneiss Terrains [electronic resource] /
title_sort field geology of high-grade gneiss terrains [electronic resource] /
publisher Berlin, Heidelberg : Springer Berlin Heidelberg,
publishDate 1990
url http://dx.doi.org/10.1007/978-3-642-76013-6
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spelling KOHA-OAI-TEST:2183362018-07-30T23:55:10ZField Geology of High-Grade Gneiss Terrains [electronic resource] / Passchier, Cees W. author. Myers, John Stuart. author. Kröner, Alfred. author. SpringerLink (Online service) textBerlin, Heidelberg : Springer Berlin Heidelberg,1990.engAlthough there are numerous publications on the geology of high-grade gneiss terrains, few descriptions exist of how to map and carry out structural analysis in these terrains. Textbooks on structural geology concentrate on technIques appli­ cable to low-grade terrains. Geologists who have no experience of mapping high-grade gneisses are often at a loss as to how to apply techniques to high­ grade rocks that were developed for low to medium grade metamorphic terrains. Any study of deep crustal processes and their development through time should begin with examination of the primary data source - outcrops of high­ grade metamorphic terrains. We feel that the urge to apply advanced techniques of fabric analysis, petrology, geochemistry, isotope geochemistry and age deter­ mination to these rocks often results in brief sampling trips in which there is little, if any analysis of the structural and metamorphic history revealed by outcrop patterns. Many studies of the metamorphic petrology and geochemistry of high-grade gneiss terrains make ineffective use of available field data, often because the authors are unaware of structural complexities and of the ways to recognise and use them. This is unfortunate, because much data can be collected in the field at minimal cost that cannot easily, if at all, be obtained from material in the laboratory. The primary igneous or sedimentary nature of a rock, the relative age of intrusive veins, and the sequence of deformation that they under­ went, can usually best be determined by straightforward observation in the field.1 Introduction -- 2 Mapping in Gneiss Terrains -- 2.1 Introduction -- 2.2 General Problems -- 2.3 Working Method -- 2.4 Outcrop Analysis -- 2.5 What to Map -- 2.6 Types of Maps 7. -- 2.7 Scheme of Events -- 2.8 Sampling -- 3 Fabric Development in Gneiss Terrains -- 3.1 Introduction -- 3.2 The Geometry of Ductile Flow in Rocks -- 3.3 Fabric Elements -- 3.4 Shear Zones in High-Grade Conditions -- 3.5 Fabric Distribution in Shear Zones -- 4 Interpretation of Structures and Fabrics -- 4.1 The Inadequate Memory of Rocks -- 4.2 Igneous or Sedimentary Origin of Gneisses -- 4.3 Assessment of Strain Intensity -- 4.4 Shear Zones -- 4.5 Folds and Boudins -- 4.6 Overprinting Relations Involving Folds and Boudins -- 4.7 Overprinting Relations Involving Intrusions -- 4.8 Outcrop Surface and Fabric Patterns -- 5 Metamorphic History of Gneiss Terrains -- 5.1 Introduction -- 5.2 Metamorphic History -- 5.3 Fabric Evidence for Metamorphic History -- 5.4 Metamorphic Conditions -- 5.5 Sites to Study Retrogression Fabrics -- 5.6 Relative Dating of Metamorphic Events -- 5.7 Isograd Patterns -- 5.8 Geothermobarometry -- 6 Geochemistry, Isotope Geochemistry and Geoehronology: Application to Field Studies -- 6.1 Introduction -- 6.2 Geochemistry -- 6.3 Isotope Geochemistry -- 6.4 Geochronology -- 7 Origin and Evolution of High-Grade Gneiss Terrains -- 7.1 Introduction -- 7.2 Two Kinds of Gneiss Terrain -- 7.3 Crustal Structure of Gneiss Terrains -- 7.4 Origin and Evolution of High-Grade Gneiss Terrains -- 8 Problem Section -- 8.1 Introduction -- 8.2 Informative Misinterpretations -- 8.3 Problems -- 9 References -- 10 Index.Although there are numerous publications on the geology of high-grade gneiss terrains, few descriptions exist of how to map and carry out structural analysis in these terrains. Textbooks on structural geology concentrate on technIques appli­ cable to low-grade terrains. Geologists who have no experience of mapping high-grade gneisses are often at a loss as to how to apply techniques to high­ grade rocks that were developed for low to medium grade metamorphic terrains. Any study of deep crustal processes and their development through time should begin with examination of the primary data source - outcrops of high­ grade metamorphic terrains. We feel that the urge to apply advanced techniques of fabric analysis, petrology, geochemistry, isotope geochemistry and age deter­ mination to these rocks often results in brief sampling trips in which there is little, if any analysis of the structural and metamorphic history revealed by outcrop patterns. Many studies of the metamorphic petrology and geochemistry of high-grade gneiss terrains make ineffective use of available field data, often because the authors are unaware of structural complexities and of the ways to recognise and use them. This is unfortunate, because much data can be collected in the field at minimal cost that cannot easily, if at all, be obtained from material in the laboratory. The primary igneous or sedimentary nature of a rock, the relative age of intrusive veins, and the sequence of deformation that they under­ went, can usually best be determined by straightforward observation in the field.Earth sciences.Geochemistry.Geology.Mineralogy.Earth Sciences.Geology.Geochemistry.Mineralogy.Springer eBookshttp://dx.doi.org/10.1007/978-3-642-76013-6URN:ISBN:9783642760136

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