Equilibrium and Kinetics in Contact Metamorphism: The Ballachulish Igneous Complex and Its Aureole
With the new global tectonics approach in the Earth Sciences, the quan titative aspects of the dynamics of rock-forming processes came into focus: geologists are no longer satisfied knowing the pressure-tempera ture conditions of the formation of a metamorphic rock or of the emplace ment of a magmat...
Gespeichert in:
| Weitere Verfasser: | , , , |
|---|---|
| Format: | Elektronisch E-Book |
| Sprache: | English |
| Veröffentlicht: |
Berlin, Heidelberg
Springer Berlin Heidelberg
1991
|
| Schlagworte: | |
| Online-Zugang: | BTU01 URL des Erstveröffentlichers |
| Zusammenfassung: | With the new global tectonics approach in the Earth Sciences, the quan titative aspects of the dynamics of rock-forming processes came into focus: geologists are no longer satisfied knowing the pressure-tempera ture conditions of the formation of a metamorphic rock or of the emplace ment of a magmatic body, but instead would like to learn the time history of these rocks as well, i. e. , derive the temperature-pressure-time path and relate it to a tectonic process. To achieve this goal, a knowledge of both pressure-temperature-dependent equilibria and the time scales at which these equilibria may be attained are essential. However, the latter kinetic information is much more difficult to retrieve than that on equilibria: whereas equilibria are controlled by state variables, and proper laboratory experiments may be directly applied to equilibrium natural assemblages, kinetics also depends on factors other than state variables, such as grain size, dislocation density, and especially time (rate of heating, duration of annealing, rate of cooling). Extrapolation of kinetic data obtained at high temperatures on laboratory time scales to more realistic lower tempera tures and geological time scales are dangerous because, for example, of possible changes from an intrinsically controlled defect regime to an extrinsic one as temperature is lowered, or from an interface-controlled to a diffusion-controlled reaction mechanism |
| Beschreibung: | 1 Online-Ressource (XIII, 484 p. 172 illus. in color) |
| ISBN: | 9783642761454 |
| DOI: | 10.1007/978-3-642-76145-4 |
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| 245 | 1 | 0 | |a Equilibrium and Kinetics in Contact Metamorphism |b The Ballachulish Igneous Complex and Its Aureole |c edited by Gerhard Voll, Jutta Tpel, David R. M. Pattison, Friedrich Seifert |
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| 520 | |a With the new global tectonics approach in the Earth Sciences, the quan titative aspects of the dynamics of rock-forming processes came into focus: geologists are no longer satisfied knowing the pressure-tempera ture conditions of the formation of a metamorphic rock or of the emplace ment of a magmatic body, but instead would like to learn the time history of these rocks as well, i. e. , derive the temperature-pressure-time path and relate it to a tectonic process. To achieve this goal, a knowledge of both pressure-temperature-dependent equilibria and the time scales at which these equilibria may be attained are essential. However, the latter kinetic information is much more difficult to retrieve than that on equilibria: whereas equilibria are controlled by state variables, and proper laboratory experiments may be directly applied to equilibrium natural assemblages, kinetics also depends on factors other than state variables, such as grain size, dislocation density, and especially time (rate of heating, duration of annealing, rate of cooling). Extrapolation of kinetic data obtained at high temperatures on laboratory time scales to more realistic lower tempera tures and geological time scales are dangerous because, for example, of possible changes from an intrinsically controlled defect regime to an extrinsic one as temperature is lowered, or from an interface-controlled to a diffusion-controlled reaction mechanism | ||
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Datensatz im Suchindex
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| discipline | Geologie / Paläontologie |
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| geographic | Ballachuliśh-Komplex (DE-588)4270586-1 gnd |
| geographic_facet | Ballachuliśh-Komplex |
| id | DE-604.BV045177958 |
| illustrated | Not Illustrated |
| indexdate | 2024-07-10T08:10:48Z |
| institution | BVB |
| isbn | 9783642761454 |
| language | English |
| oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-030567188 |
| oclc_num | 1185255070 |
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| physical | 1 Online-Ressource (XIII, 484 p. 172 illus. in color) |
| psigel | ZDB-2-EES ZDB-2-EES_Archiv ZDB-2-EES ZDB-2-EES_Archiv |
| publishDate | 1991 |
| publishDateSearch | 1991 |
| publishDateSort | 1991 |
| publisher | Springer Berlin Heidelberg |
| record_format | marc |
| spelling | Equilibrium and Kinetics in Contact Metamorphism The Ballachulish Igneous Complex and Its Aureole edited by Gerhard Voll, Jutta Tpel, David R. M. Pattison, Friedrich Seifert Berlin, Heidelberg Springer Berlin Heidelberg 1991 1 Online-Ressource (XIII, 484 p. 172 illus. in color) txt rdacontent c rdamedia cr rdacarrier With the new global tectonics approach in the Earth Sciences, the quan titative aspects of the dynamics of rock-forming processes came into focus: geologists are no longer satisfied knowing the pressure-tempera ture conditions of the formation of a metamorphic rock or of the emplace ment of a magmatic body, but instead would like to learn the time history of these rocks as well, i. e. , derive the temperature-pressure-time path and relate it to a tectonic process. To achieve this goal, a knowledge of both pressure-temperature-dependent equilibria and the time scales at which these equilibria may be attained are essential. However, the latter kinetic information is much more difficult to retrieve than that on equilibria: whereas equilibria are controlled by state variables, and proper laboratory experiments may be directly applied to equilibrium natural assemblages, kinetics also depends on factors other than state variables, such as grain size, dislocation density, and especially time (rate of heating, duration of annealing, rate of cooling). Extrapolation of kinetic data obtained at high temperatures on laboratory time scales to more realistic lower tempera tures and geological time scales are dangerous because, for example, of possible changes from an intrinsically controlled defect regime to an extrinsic one as temperature is lowered, or from an interface-controlled to a diffusion-controlled reaction mechanism Earth Sciences Geology Mineralogy Earth sciences Kontakthof (DE-588)4270589-7 gnd rswk-swf Kontaktmetamorphose (DE-588)4270587-3 gnd rswk-swf Ballachuliśh-Komplex (DE-588)4270586-1 gnd rswk-swf Ballachuliśh-Komplex (DE-588)4270586-1 g Kontaktmetamorphose (DE-588)4270587-3 s Kontakthof (DE-588)4270589-7 s 1\p DE-604 Voll, Gerhard edt Tpel, Jutta edt Pattison, David R. M. edt Seifert, Friedrich edt Erscheint auch als Druck-Ausgabe 9783642761478 https://doi.org/10.1007/978-3-642-76145-4 Verlag URL des Erstveröffentlichers Volltext 1\p cgwrk 20201028 DE-101 https://d-nb.info/provenance/plan#cgwrk |
| spellingShingle | Equilibrium and Kinetics in Contact Metamorphism The Ballachulish Igneous Complex and Its Aureole Earth Sciences Geology Mineralogy Earth sciences Kontakthof (DE-588)4270589-7 gnd Kontaktmetamorphose (DE-588)4270587-3 gnd |
| subject_GND | (DE-588)4270589-7 (DE-588)4270587-3 (DE-588)4270586-1 |
| title | Equilibrium and Kinetics in Contact Metamorphism The Ballachulish Igneous Complex and Its Aureole |
| title_auth | Equilibrium and Kinetics in Contact Metamorphism The Ballachulish Igneous Complex and Its Aureole |
| title_exact_search | Equilibrium and Kinetics in Contact Metamorphism The Ballachulish Igneous Complex and Its Aureole |
| title_full | Equilibrium and Kinetics in Contact Metamorphism The Ballachulish Igneous Complex and Its Aureole edited by Gerhard Voll, Jutta Tpel, David R. M. Pattison, Friedrich Seifert |
| title_fullStr | Equilibrium and Kinetics in Contact Metamorphism The Ballachulish Igneous Complex and Its Aureole edited by Gerhard Voll, Jutta Tpel, David R. M. Pattison, Friedrich Seifert |
| title_full_unstemmed | Equilibrium and Kinetics in Contact Metamorphism The Ballachulish Igneous Complex and Its Aureole edited by Gerhard Voll, Jutta Tpel, David R. M. Pattison, Friedrich Seifert |
| title_short | Equilibrium and Kinetics in Contact Metamorphism |
| title_sort | equilibrium and kinetics in contact metamorphism the ballachulish igneous complex and its aureole |
| title_sub | The Ballachulish Igneous Complex and Its Aureole |
| topic | Earth Sciences Geology Mineralogy Earth sciences Kontakthof (DE-588)4270589-7 gnd Kontaktmetamorphose (DE-588)4270587-3 gnd |
| topic_facet | Earth Sciences Geology Mineralogy Earth sciences Kontakthof Kontaktmetamorphose Ballachuliśh-Komplex |
| url | https://doi.org/10.1007/978-3-642-76145-4 |
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