Illite: Origins, Evolution and Metamorphism
It is our pleasure to present this large body of information and thoughts of many mineral scientists which has accumulated over decades. Illite is a mineral that has been discovered relatively recently, even though it has great importance in the geological cycles of weathering, sedimentation and bur...
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Hauptverfasser: | , |
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Format: | Elektronisch E-Book |
Sprache: | English |
Veröffentlicht: |
Berlin, Heidelberg
Springer Berlin Heidelberg
2004
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Schlagworte: | |
Online-Zugang: | BTU01 URL des Erstveröffentlichers |
Zusammenfassung: | It is our pleasure to present this large body of information and thoughts of many mineral scientists which has accumulated over decades. Illite is a mineral that has been discovered relatively recently, even though it has great importance in the geological cycles of weathering, sedimentation and burial. Illite is the major potassium mineral among silicates in the surface environment. Potassium represents the only alkaline metal, to be bound in silicate structures during the great chemical reshuffling called weathering. The weathering environment is one of strong chemical segregation, where Si and AI become the resistant, of silicate rocks. Iron forms an oxide and potassium forms residual elements the stable clay illite. Then Si and Al form smectites and kaolinite. Sodium, calcium and to a large extent magnesium are extracted from the solids as dissolved ionic species of the altering fluids. Ca and Mg are reintroduced into solid minerals via carbonate precipitation, and Na remains to make the sea saline. This mineral has been difficult to study because it is of fine grain size, as are all clays: 2 pm in diameter. Illite, along with other clays, had to wait to be discovered until a useful method of X-ray detection became available. With such a tool clays, whose definition was initially based upon the resolving power of an optical microscope (2 ]. lm), could be efficiently investigated. In fact the study of illite parallels the use and development of X -ray diffraction techniques |
Beschreibung: | 1 Online-Ressource (XVI, 288 p) |
ISBN: | 9783662078501 |
DOI: | 10.1007/978-3-662-07850-1 |
Internformat
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520 | |a It is our pleasure to present this large body of information and thoughts of many mineral scientists which has accumulated over decades. Illite is a mineral that has been discovered relatively recently, even though it has great importance in the geological cycles of weathering, sedimentation and burial. Illite is the major potassium mineral among silicates in the surface environment. Potassium represents the only alkaline metal, to be bound in silicate structures during the great chemical reshuffling called weathering. The weathering environment is one of strong chemical segregation, where Si and AI become the resistant, of silicate rocks. Iron forms an oxide and potassium forms residual elements the stable clay illite. Then Si and Al form smectites and kaolinite. Sodium, calcium and to a large extent magnesium are extracted from the solids as dissolved ionic species of the altering fluids. Ca and Mg are reintroduced into solid minerals via carbonate precipitation, and Na remains to make the sea saline. This mineral has been difficult to study because it is of fine grain size, as are all clays: 2 pm in diameter. Illite, along with other clays, had to wait to be discovered until a useful method of X-ray detection became available. With such a tool clays, whose definition was initially based upon the resolving power of an optical microscope (2 ]. lm), could be efficiently investigated. In fact the study of illite parallels the use and development of X -ray diffraction techniques | ||
650 | 4 | |a Earth Sciences | |
650 | 4 | |a Mineralogy | |
650 | 4 | |a Soil Science & Conservation | |
650 | 4 | |a Crystallography | |
650 | 4 | |a Mineral Resources | |
650 | 4 | |a Sedimentology | |
650 | 4 | |a Earth sciences | |
650 | 4 | |a Mineral resources | |
650 | 4 | |a Mineralogy | |
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650 | 4 | |a Crystallography | |
650 | 4 | |a Soil science | |
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author | Meunier, Alain 1948- Velde, Bruce |
author_GND | (DE-588)1145752241 (DE-588)120623013 |
author_facet | Meunier, Alain 1948- Velde, Bruce |
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dewey-ones | 549 - Mineralogy |
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dewey-search | 549 |
dewey-sort | 3549 |
dewey-tens | 540 - Chemistry and allied sciences |
discipline | Chemie / Pharmazie Geographie |
doi_str_mv | 10.1007/978-3-662-07850-1 |
format | Electronic eBook |
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spelling | Meunier, Alain 1948- Verfasser (DE-588)1145752241 aut Illite Origins, Evolution and Metamorphism by Alain Meunier, Bruce Velde Berlin, Heidelberg Springer Berlin Heidelberg 2004 1 Online-Ressource (XVI, 288 p) txt rdacontent c rdamedia cr rdacarrier It is our pleasure to present this large body of information and thoughts of many mineral scientists which has accumulated over decades. Illite is a mineral that has been discovered relatively recently, even though it has great importance in the geological cycles of weathering, sedimentation and burial. Illite is the major potassium mineral among silicates in the surface environment. Potassium represents the only alkaline metal, to be bound in silicate structures during the great chemical reshuffling called weathering. The weathering environment is one of strong chemical segregation, where Si and AI become the resistant, of silicate rocks. Iron forms an oxide and potassium forms residual elements the stable clay illite. Then Si and Al form smectites and kaolinite. Sodium, calcium and to a large extent magnesium are extracted from the solids as dissolved ionic species of the altering fluids. Ca and Mg are reintroduced into solid minerals via carbonate precipitation, and Na remains to make the sea saline. This mineral has been difficult to study because it is of fine grain size, as are all clays: 2 pm in diameter. Illite, along with other clays, had to wait to be discovered until a useful method of X-ray detection became available. With such a tool clays, whose definition was initially based upon the resolving power of an optical microscope (2 ]. lm), could be efficiently investigated. In fact the study of illite parallels the use and development of X -ray diffraction techniques Earth Sciences Mineralogy Soil Science & Conservation Crystallography Mineral Resources Sedimentology Earth sciences Mineral resources Soil science Soil conservation Illit (DE-588)4161272-3 gnd rswk-swf Illit (DE-588)4161272-3 s DE-604 Velde, Bruce (DE-588)120623013 aut Erscheint auch als Druck-Ausgabe 9783642058066 https://doi.org/10.1007/978-3-662-07850-1 Verlag URL des Erstveröffentlichers Volltext |
spellingShingle | Meunier, Alain 1948- Velde, Bruce Illite Origins, Evolution and Metamorphism Earth Sciences Mineralogy Soil Science & Conservation Crystallography Mineral Resources Sedimentology Earth sciences Mineral resources Soil science Soil conservation Illit (DE-588)4161272-3 gnd |
subject_GND | (DE-588)4161272-3 |
title | Illite Origins, Evolution and Metamorphism |
title_auth | Illite Origins, Evolution and Metamorphism |
title_exact_search | Illite Origins, Evolution and Metamorphism |
title_full | Illite Origins, Evolution and Metamorphism by Alain Meunier, Bruce Velde |
title_fullStr | Illite Origins, Evolution and Metamorphism by Alain Meunier, Bruce Velde |
title_full_unstemmed | Illite Origins, Evolution and Metamorphism by Alain Meunier, Bruce Velde |
title_short | Illite |
title_sort | illite origins evolution and metamorphism |
title_sub | Origins, Evolution and Metamorphism |
topic | Earth Sciences Mineralogy Soil Science & Conservation Crystallography Mineral Resources Sedimentology Earth sciences Mineral resources Soil science Soil conservation Illit (DE-588)4161272-3 gnd |
topic_facet | Earth Sciences Mineralogy Soil Science & Conservation Crystallography Mineral Resources Sedimentology Earth sciences Mineral resources Soil science Soil conservation Illit |
url | https://doi.org/10.1007/978-3-662-07850-1 |
work_keys_str_mv | AT meunieralain illiteoriginsevolutionandmetamorphism AT veldebruce illiteoriginsevolutionandmetamorphism |