Thermodynamics in Geology: Proceedings of the NATO Advanced Study Institute held in Oxford, England, September 17–27, 1976
Gespeichert in:
1. Verfasser: | |
---|---|
Format: | Elektronisch E-Book |
Sprache: | English |
Veröffentlicht: |
Dordrecht
Springer Netherlands
1977
|
Schriftenreihe: | NATO Advanced Study Institutes Series, Series C — Mathematical and Physical Sciences
30 |
Schlagworte: | |
Online-Zugang: | Volltext |
Beschreibung: | It has long been realized that the mineral assemblages of igneous and metamorphic rocks may reflect the approach of a rock to chemical eCluilibrium during its formation. However progress in the application of chemical thermodynamics to geological systems has been hindered since the time of Bowen and the other early physical-chemical petrologists by the recurring Cluandary of the experimental geologist. His systems are complex and are experimentally intractable, but if they were not so refractory they would not be there to study at all. It is only recently that accurate measurements of the thermodynamic properties of pure, or at least well-defined minerals, melts and volatile fluid phases, combined with experimental and theoretical studies of their mixing properties, have made it possible to calculate the eCluilibrium conditions for particular rock systems. Much work is now in progress to extend the ranges of com position and conditions for which sufficient data exist to enable such calculations to be made. Moreover the routine availability of the electron microprobe will ensure that the demand for such information will continue to increase. The thermodynamic techniClues reCluired to apply these data to geological problems are intrinsically simple and merely involve the combination of appropriate standard state data together with corrections for the effects of solution in natural minerals, melts or volatile fluids |
Beschreibung: | 1 Online-Ressource (XIII, 410 p) |
ISBN: | 9789401012522 9789027708342 |
ISSN: | 1389-2185 |
DOI: | 10.1007/978-94-010-1252-2 |
Internformat
MARC
LEADER | 00000nmm a2200000zcb4500 | ||
---|---|---|---|
001 | BV042415542 | ||
003 | DE-604 | ||
005 | 00000000000000.0 | ||
007 | cr|uuu---uuuuu | ||
008 | 150316s1977 |||| o||u| ||||||eng d | ||
020 | |a 9789401012522 |c Online |9 978-94-010-1252-2 | ||
020 | |a 9789027708342 |c Print |9 978-90-277-0834-2 | ||
024 | 7 | |a 10.1007/978-94-010-1252-2 |2 doi | |
035 | |a (OCoLC)863774643 | ||
035 | |a (DE-599)BVBBV042415542 | ||
040 | |a DE-604 |b ger |e aacr | ||
041 | 0 | |a eng | |
049 | |a DE-91 |a DE-83 | ||
082 | 0 | |a 551.9 |2 23 | |
084 | |a PHY 000 |2 stub | ||
100 | 1 | |a Fraser, Donald G. |e Verfasser |4 aut | |
245 | 1 | 0 | |a Thermodynamics in Geology |b Proceedings of the NATO Advanced Study Institute held in Oxford, England, September 17–27, 1976 |c edited by Donald G. Fraser |
246 | 1 | 3 | |a Proceedings of the NATO Advanced Study Institute, Oxford, England, September 17-27, 1976 |
264 | 1 | |a Dordrecht |b Springer Netherlands |c 1977 | |
300 | |a 1 Online-Ressource (XIII, 410 p) | ||
336 | |b txt |2 rdacontent | ||
337 | |b c |2 rdamedia | ||
338 | |b cr |2 rdacarrier | ||
490 | 0 | |a NATO Advanced Study Institutes Series, Series C — Mathematical and Physical Sciences |v 30 |x 1389-2185 | |
500 | |a It has long been realized that the mineral assemblages of igneous and metamorphic rocks may reflect the approach of a rock to chemical eCluilibrium during its formation. However progress in the application of chemical thermodynamics to geological systems has been hindered since the time of Bowen and the other early physical-chemical petrologists by the recurring Cluandary of the experimental geologist. His systems are complex and are experimentally intractable, but if they were not so refractory they would not be there to study at all. It is only recently that accurate measurements of the thermodynamic properties of pure, or at least well-defined minerals, melts and volatile fluid phases, combined with experimental and theoretical studies of their mixing properties, have made it possible to calculate the eCluilibrium conditions for particular rock systems. Much work is now in progress to extend the ranges of com position and conditions for which sufficient data exist to enable such calculations to be made. Moreover the routine availability of the electron microprobe will ensure that the demand for such information will continue to increase. The thermodynamic techniClues reCluired to apply these data to geological problems are intrinsically simple and merely involve the combination of appropriate standard state data together with corrections for the effects of solution in natural minerals, melts or volatile fluids | ||
650 | 4 | |a Geography | |
650 | 4 | |a Geochemistry | |
650 | 4 | |a Earth Sciences | |
650 | 4 | |a Geografie | |
650 | 4 | |a Geowissenschaften | |
650 | 0 | 7 | |a Geologie |0 (DE-588)4020227-6 |2 gnd |9 rswk-swf |
650 | 0 | 7 | |a Thermodynamik |0 (DE-588)4059827-5 |2 gnd |9 rswk-swf |
655 | 7 | |8 1\p |0 (DE-588)1071861417 |a Konferenzschrift |y 1976 |z Oxford |2 gnd-content | |
689 | 0 | 0 | |a Geologie |0 (DE-588)4020227-6 |D s |
689 | 0 | 1 | |a Thermodynamik |0 (DE-588)4059827-5 |D s |
689 | 0 | |8 2\p |5 DE-604 | |
856 | 4 | 0 | |u https://doi.org/10.1007/978-94-010-1252-2 |x Verlag |3 Volltext |
912 | |a ZDB-2-PHA |a ZDB-2-BAE | ||
940 | 1 | |q ZDB-2-PHA_Archive | |
999 | |a oai:aleph.bib-bvb.de:BVB01-027851035 | ||
883 | 1 | |8 1\p |a cgwrk |d 20201028 |q DE-101 |u https://d-nb.info/provenance/plan#cgwrk | |
883 | 1 | |8 2\p |a cgwrk |d 20201028 |q DE-101 |u https://d-nb.info/provenance/plan#cgwrk |
Datensatz im Suchindex
_version_ | 1804153082763804672 |
---|---|
any_adam_object | |
author | Fraser, Donald G. |
author_facet | Fraser, Donald G. |
author_role | aut |
author_sort | Fraser, Donald G. |
author_variant | d g f dg dgf |
building | Verbundindex |
bvnumber | BV042415542 |
classification_tum | PHY 000 |
collection | ZDB-2-PHA ZDB-2-BAE |
ctrlnum | (OCoLC)863774643 (DE-599)BVBBV042415542 |
dewey-full | 551.9 |
dewey-hundreds | 500 - Natural sciences and mathematics |
dewey-ones | 551 - Geology, hydrology, meteorology |
dewey-raw | 551.9 |
dewey-search | 551.9 |
dewey-sort | 3551.9 |
dewey-tens | 550 - Earth sciences |
discipline | Geologie / Paläontologie Physik |
doi_str_mv | 10.1007/978-94-010-1252-2 |
format | Electronic eBook |
fullrecord | <?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>03493nmm a2200529zcb4500</leader><controlfield tag="001">BV042415542</controlfield><controlfield tag="003">DE-604</controlfield><controlfield tag="005">00000000000000.0</controlfield><controlfield tag="007">cr|uuu---uuuuu</controlfield><controlfield tag="008">150316s1977 |||| o||u| ||||||eng d</controlfield><datafield tag="020" ind1=" " ind2=" "><subfield code="a">9789401012522</subfield><subfield code="c">Online</subfield><subfield code="9">978-94-010-1252-2</subfield></datafield><datafield tag="020" ind1=" " ind2=" "><subfield code="a">9789027708342</subfield><subfield code="c">Print</subfield><subfield code="9">978-90-277-0834-2</subfield></datafield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/978-94-010-1252-2</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(OCoLC)863774643</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-599)BVBBV042415542</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-604</subfield><subfield code="b">ger</subfield><subfield code="e">aacr</subfield></datafield><datafield tag="041" ind1="0" ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="049" ind1=" " ind2=" "><subfield code="a">DE-91</subfield><subfield code="a">DE-83</subfield></datafield><datafield tag="082" ind1="0" ind2=" "><subfield code="a">551.9</subfield><subfield code="2">23</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">PHY 000</subfield><subfield code="2">stub</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Fraser, Donald G.</subfield><subfield code="e">Verfasser</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Thermodynamics in Geology</subfield><subfield code="b">Proceedings of the NATO Advanced Study Institute held in Oxford, England, September 17–27, 1976</subfield><subfield code="c">edited by Donald G. Fraser</subfield></datafield><datafield tag="246" ind1="1" ind2="3"><subfield code="a">Proceedings of the NATO Advanced Study Institute, Oxford, England, September 17-27, 1976</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Dordrecht</subfield><subfield code="b">Springer Netherlands</subfield><subfield code="c">1977</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">1 Online-Ressource (XIII, 410 p)</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="490" ind1="0" ind2=" "><subfield code="a">NATO Advanced Study Institutes Series, Series C — Mathematical and Physical Sciences</subfield><subfield code="v">30</subfield><subfield code="x">1389-2185</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">It has long been realized that the mineral assemblages of igneous and metamorphic rocks may reflect the approach of a rock to chemical eCluilibrium during its formation. However progress in the application of chemical thermodynamics to geological systems has been hindered since the time of Bowen and the other early physical-chemical petrologists by the recurring Cluandary of the experimental geologist. His systems are complex and are experimentally intractable, but if they were not so refractory they would not be there to study at all. It is only recently that accurate measurements of the thermodynamic properties of pure, or at least well-defined minerals, melts and volatile fluid phases, combined with experimental and theoretical studies of their mixing properties, have made it possible to calculate the eCluilibrium conditions for particular rock systems. Much work is now in progress to extend the ranges of com position and conditions for which sufficient data exist to enable such calculations to be made. Moreover the routine availability of the electron microprobe will ensure that the demand for such information will continue to increase. The thermodynamic techniClues reCluired to apply these data to geological problems are intrinsically simple and merely involve the combination of appropriate standard state data together with corrections for the effects of solution in natural minerals, melts or volatile fluids</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geography</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geochemistry</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Earth Sciences</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geografie</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Geowissenschaften</subfield></datafield><datafield tag="650" ind1="0" ind2="7"><subfield code="a">Geologie</subfield><subfield code="0">(DE-588)4020227-6</subfield><subfield code="2">gnd</subfield><subfield code="9">rswk-swf</subfield></datafield><datafield tag="650" ind1="0" ind2="7"><subfield code="a">Thermodynamik</subfield><subfield code="0">(DE-588)4059827-5</subfield><subfield code="2">gnd</subfield><subfield code="9">rswk-swf</subfield></datafield><datafield tag="655" ind1=" " ind2="7"><subfield code="8">1\p</subfield><subfield code="0">(DE-588)1071861417</subfield><subfield code="a">Konferenzschrift</subfield><subfield code="y">1976</subfield><subfield code="z">Oxford</subfield><subfield code="2">gnd-content</subfield></datafield><datafield tag="689" ind1="0" ind2="0"><subfield code="a">Geologie</subfield><subfield code="0">(DE-588)4020227-6</subfield><subfield code="D">s</subfield></datafield><datafield tag="689" ind1="0" ind2="1"><subfield code="a">Thermodynamik</subfield><subfield code="0">(DE-588)4059827-5</subfield><subfield code="D">s</subfield></datafield><datafield tag="689" ind1="0" ind2=" "><subfield code="8">2\p</subfield><subfield code="5">DE-604</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.1007/978-94-010-1252-2</subfield><subfield code="x">Verlag</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">ZDB-2-PHA</subfield><subfield code="a">ZDB-2-BAE</subfield></datafield><datafield tag="940" ind1="1" ind2=" "><subfield code="q">ZDB-2-PHA_Archive</subfield></datafield><datafield tag="999" ind1=" " ind2=" "><subfield code="a">oai:aleph.bib-bvb.de:BVB01-027851035</subfield></datafield><datafield tag="883" ind1="1" ind2=" "><subfield code="8">1\p</subfield><subfield code="a">cgwrk</subfield><subfield code="d">20201028</subfield><subfield code="q">DE-101</subfield><subfield code="u">https://d-nb.info/provenance/plan#cgwrk</subfield></datafield><datafield tag="883" ind1="1" ind2=" "><subfield code="8">2\p</subfield><subfield code="a">cgwrk</subfield><subfield code="d">20201028</subfield><subfield code="q">DE-101</subfield><subfield code="u">https://d-nb.info/provenance/plan#cgwrk</subfield></datafield></record></collection> |
genre | 1\p (DE-588)1071861417 Konferenzschrift 1976 Oxford gnd-content |
genre_facet | Konferenzschrift 1976 Oxford |
id | DE-604.BV042415542 |
illustrated | Not Illustrated |
indexdate | 2024-07-10T01:20:57Z |
institution | BVB |
isbn | 9789401012522 9789027708342 |
issn | 1389-2185 |
language | English |
oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-027851035 |
oclc_num | 863774643 |
open_access_boolean | |
owner | DE-91 DE-BY-TUM DE-83 |
owner_facet | DE-91 DE-BY-TUM DE-83 |
physical | 1 Online-Ressource (XIII, 410 p) |
psigel | ZDB-2-PHA ZDB-2-BAE ZDB-2-PHA_Archive |
publishDate | 1977 |
publishDateSearch | 1977 |
publishDateSort | 1977 |
publisher | Springer Netherlands |
record_format | marc |
series2 | NATO Advanced Study Institutes Series, Series C — Mathematical and Physical Sciences |
spelling | Fraser, Donald G. Verfasser aut Thermodynamics in Geology Proceedings of the NATO Advanced Study Institute held in Oxford, England, September 17–27, 1976 edited by Donald G. Fraser Proceedings of the NATO Advanced Study Institute, Oxford, England, September 17-27, 1976 Dordrecht Springer Netherlands 1977 1 Online-Ressource (XIII, 410 p) txt rdacontent c rdamedia cr rdacarrier NATO Advanced Study Institutes Series, Series C — Mathematical and Physical Sciences 30 1389-2185 It has long been realized that the mineral assemblages of igneous and metamorphic rocks may reflect the approach of a rock to chemical eCluilibrium during its formation. However progress in the application of chemical thermodynamics to geological systems has been hindered since the time of Bowen and the other early physical-chemical petrologists by the recurring Cluandary of the experimental geologist. His systems are complex and are experimentally intractable, but if they were not so refractory they would not be there to study at all. It is only recently that accurate measurements of the thermodynamic properties of pure, or at least well-defined minerals, melts and volatile fluid phases, combined with experimental and theoretical studies of their mixing properties, have made it possible to calculate the eCluilibrium conditions for particular rock systems. Much work is now in progress to extend the ranges of com position and conditions for which sufficient data exist to enable such calculations to be made. Moreover the routine availability of the electron microprobe will ensure that the demand for such information will continue to increase. The thermodynamic techniClues reCluired to apply these data to geological problems are intrinsically simple and merely involve the combination of appropriate standard state data together with corrections for the effects of solution in natural minerals, melts or volatile fluids Geography Geochemistry Earth Sciences Geografie Geowissenschaften Geologie (DE-588)4020227-6 gnd rswk-swf Thermodynamik (DE-588)4059827-5 gnd rswk-swf 1\p (DE-588)1071861417 Konferenzschrift 1976 Oxford gnd-content Geologie (DE-588)4020227-6 s Thermodynamik (DE-588)4059827-5 s 2\p DE-604 https://doi.org/10.1007/978-94-010-1252-2 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 |
spellingShingle | Fraser, Donald G. Thermodynamics in Geology Proceedings of the NATO Advanced Study Institute held in Oxford, England, September 17–27, 1976 Geography Geochemistry Earth Sciences Geografie Geowissenschaften Geologie (DE-588)4020227-6 gnd Thermodynamik (DE-588)4059827-5 gnd |
subject_GND | (DE-588)4020227-6 (DE-588)4059827-5 (DE-588)1071861417 |
title | Thermodynamics in Geology Proceedings of the NATO Advanced Study Institute held in Oxford, England, September 17–27, 1976 |
title_alt | Proceedings of the NATO Advanced Study Institute, Oxford, England, September 17-27, 1976 |
title_auth | Thermodynamics in Geology Proceedings of the NATO Advanced Study Institute held in Oxford, England, September 17–27, 1976 |
title_exact_search | Thermodynamics in Geology Proceedings of the NATO Advanced Study Institute held in Oxford, England, September 17–27, 1976 |
title_full | Thermodynamics in Geology Proceedings of the NATO Advanced Study Institute held in Oxford, England, September 17–27, 1976 edited by Donald G. Fraser |
title_fullStr | Thermodynamics in Geology Proceedings of the NATO Advanced Study Institute held in Oxford, England, September 17–27, 1976 edited by Donald G. Fraser |
title_full_unstemmed | Thermodynamics in Geology Proceedings of the NATO Advanced Study Institute held in Oxford, England, September 17–27, 1976 edited by Donald G. Fraser |
title_short | Thermodynamics in Geology |
title_sort | thermodynamics in geology proceedings of the nato advanced study institute held in oxford england september 17 27 1976 |
title_sub | Proceedings of the NATO Advanced Study Institute held in Oxford, England, September 17–27, 1976 |
topic | Geography Geochemistry Earth Sciences Geografie Geowissenschaften Geologie (DE-588)4020227-6 gnd Thermodynamik (DE-588)4059827-5 gnd |
topic_facet | Geography Geochemistry Earth Sciences Geografie Geowissenschaften Geologie Thermodynamik Konferenzschrift 1976 Oxford |
url | https://doi.org/10.1007/978-94-010-1252-2 |
work_keys_str_mv | AT fraserdonaldg thermodynamicsingeologyproceedingsofthenatoadvancedstudyinstituteheldinoxfordenglandseptember17271976 AT fraserdonaldg proceedingsofthenatoadvancedstudyinstituteoxfordenglandseptember17271976 |