Feldspars and Feldspathoids: Structures, Properties and Occurrences
Gespeichert in:
Weitere Verfasser: | |
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Format: | Elektronisch E-Book |
Sprache: | English |
Veröffentlicht: |
Dordrecht
Springer Netherlands
1984
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Schriftenreihe: | NATO ASI Series, Series C: Mathematical and Physical Sciences
137 |
Schlagworte: | |
Online-Zugang: | Volltext |
Beschreibung: | The feldspars form the most abundant group of minerals in the crust of the Earth and Moon and also occur in many meteorites. They play a fundamental role in all rock-forming processes at shallow depths, but are rare or absent from the upper mantle. Their detailed study is thus essential for the understanding of such varied processes as magma genesis and differentiation, metamorphism, alteration, erosion and sedimentation. This interest is show by the fact that two previous NATO Advanced Study Institutes on feldspars were held in Oslo in 1962 and in Manchester in 1972. The feldspars are particularly suitable for detailed studies, as they have very simple chemistry and develop some of the most complex microstructures known. The microstructures are often slow to form but are easily preserved, so that they are potentially extremely informative about the geological history of the rocks in which they occur. Furthermore, their study involves physical and chemical methods of increasing sophistication so that the results obtained are not always immediately understandable to research workers outside the field of modern mineralogy. Progress in knowledge about feldspars is probably slower in penetrating the fields of petrology and geochemistry than that on other mineral groups. For these reasons among others, it was particularly appropriate to hold a third NATO ASI on feldspars approximately ten years after the last one |
Beschreibung: | 1 Online-Ressource (XVIII, 542 p) |
ISBN: | 9789401569293 9789401569316 |
ISSN: | 1389-2185 |
DOI: | 10.1007/978-94-015-6929-3 |
Internformat
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490 | 1 | |a NATO ASI Series, Series C: Mathematical and Physical Sciences |v 137 |x 1389-2185 | |
500 | |a The feldspars form the most abundant group of minerals in the crust of the Earth and Moon and also occur in many meteorites. They play a fundamental role in all rock-forming processes at shallow depths, but are rare or absent from the upper mantle. Their detailed study is thus essential for the understanding of such varied processes as magma genesis and differentiation, metamorphism, alteration, erosion and sedimentation. This interest is show by the fact that two previous NATO Advanced Study Institutes on feldspars were held in Oslo in 1962 and in Manchester in 1972. The feldspars are particularly suitable for detailed studies, as they have very simple chemistry and develop some of the most complex microstructures known. The microstructures are often slow to form but are easily preserved, so that they are potentially extremely informative about the geological history of the rocks in which they occur. Furthermore, their study involves physical and chemical methods of increasing sophistication so that the results obtained are not always immediately understandable to research workers outside the field of modern mineralogy. Progress in knowledge about feldspars is probably slower in penetrating the fields of petrology and geochemistry than that on other mineral groups. For these reasons among others, it was particularly appropriate to hold a third NATO ASI on feldspars approximately ten years after the last one | ||
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Datensatz im Suchindex
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any_adam_object | |
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dewey-ones | 549 - Mineralogy |
dewey-raw | 549 |
dewey-search | 549 |
dewey-sort | 3549 |
dewey-tens | 540 - Chemistry and allied sciences |
discipline | Chemie / Pharmazie Physik |
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spelling | Feldspars and Feldspathoids Structures, Properties and Occurrences edited by William L. Brown Proceedings of the NATO Advanced Study Institute, Renn, France, June 26-July 6, 1983 Dordrecht Springer Netherlands 1984 1 Online-Ressource (XVIII, 542 p) txt rdacontent c rdamedia cr rdacarrier NATO ASI Series, Series C: Mathematical and Physical Sciences 137 1389-2185 The feldspars form the most abundant group of minerals in the crust of the Earth and Moon and also occur in many meteorites. They play a fundamental role in all rock-forming processes at shallow depths, but are rare or absent from the upper mantle. Their detailed study is thus essential for the understanding of such varied processes as magma genesis and differentiation, metamorphism, alteration, erosion and sedimentation. This interest is show by the fact that two previous NATO Advanced Study Institutes on feldspars were held in Oslo in 1962 and in Manchester in 1972. The feldspars are particularly suitable for detailed studies, as they have very simple chemistry and develop some of the most complex microstructures known. The microstructures are often slow to form but are easily preserved, so that they are potentially extremely informative about the geological history of the rocks in which they occur. Furthermore, their study involves physical and chemical methods of increasing sophistication so that the results obtained are not always immediately understandable to research workers outside the field of modern mineralogy. Progress in knowledge about feldspars is probably slower in penetrating the fields of petrology and geochemistry than that on other mineral groups. For these reasons among others, it was particularly appropriate to hold a third NATO ASI on feldspars approximately ten years after the last one Geography Mineralogy Earth Sciences Geografie Geowissenschaften Feldspäte (DE-588)4153949-7 gnd rswk-swf Feldspatvertreter (DE-588)4327846-2 gnd rswk-swf 1\p (DE-588)1071861417 Konferenzschrift 1983 Rennes gnd-content Feldspatvertreter (DE-588)4327846-2 s 2\p DE-604 Feldspäte (DE-588)4153949-7 s 3\p DE-604 Brown, William L. edt NATO ASI Series, Series C Mathematical and Physical Sciences 137 (DE-604)BV000902768 137 https://doi.org/10.1007/978-94-015-6929-3 Verlag Volltext 1\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk 2\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk 3\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk |
spellingShingle | Feldspars and Feldspathoids Structures, Properties and Occurrences Geography Mineralogy Earth Sciences Geografie Geowissenschaften Feldspäte (DE-588)4153949-7 gnd Feldspatvertreter (DE-588)4327846-2 gnd |
subject_GND | (DE-588)4153949-7 (DE-588)4327846-2 (DE-588)1071861417 |
title | Feldspars and Feldspathoids Structures, Properties and Occurrences |
title_alt | Proceedings of the NATO Advanced Study Institute, Renn, France, June 26-July 6, 1983 |
title_auth | Feldspars and Feldspathoids Structures, Properties and Occurrences |
title_exact_search | Feldspars and Feldspathoids Structures, Properties and Occurrences |
title_full | Feldspars and Feldspathoids Structures, Properties and Occurrences edited by William L. Brown |
title_fullStr | Feldspars and Feldspathoids Structures, Properties and Occurrences edited by William L. Brown |
title_full_unstemmed | Feldspars and Feldspathoids Structures, Properties and Occurrences edited by William L. Brown |
title_short | Feldspars and Feldspathoids |
title_sort | feldspars and feldspathoids structures properties and occurrences |
title_sub | Structures, Properties and Occurrences |
topic | Geography Mineralogy Earth Sciences Geografie Geowissenschaften Feldspäte (DE-588)4153949-7 gnd Feldspatvertreter (DE-588)4327846-2 gnd |
topic_facet | Geography Mineralogy Earth Sciences Geografie Geowissenschaften Feldspäte Feldspatvertreter Konferenzschrift 1983 Rennes |
url | https://doi.org/10.1007/978-94-015-6929-3 |
volume_link | (DE-604)BV000902768 |
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