Highly siderophile and strongly chalcophile elements in high-temperature geochemistry and cosmochemistry:
Highly Siderophile and Strongly Chalcophile Elements in High Temperature Geochemistry and Cosmochemistry, Volume 81 This RiMG (Reviews in Mineralogy & Geochemistry) volume investigates the application of highly siderophile (HSE) and strongly chalcophile elements. This volume has its origin i...
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| Format: | Elektronisch E-Book |
| Sprache: | English |
| Veröffentlicht: |
[Berlin ; Boston]
De Gruyter
[2016]
Chantilly, Virginia, U.S.A. Mineralogical Society of America [2016] |
| Schriftenreihe: | Reviews in Mineralogy & Geochemistry
volume 81 |
| Schlagworte: | |
| Online-Zugang: | FAB01 FAW01 FHA01 FHR01 FKE01 FLA01 UBT01 UPA01 FCO01 Volltext |
| Zusammenfassung: | Highly Siderophile and Strongly Chalcophile Elements in High Temperature Geochemistry and Cosmochemistry, Volume 81 This RiMG (Reviews in Mineralogy & Geochemistry) volume investigates the application of highly siderophile (HSE) and strongly chalcophile elements. This volume has its origin in a short course sponsored by the Mineralogical Society of America and the Geochemical Society held in San Diego, California on the 11th and 12th December 2015, ahead of the American Geophysical Union’s Fall Meeting, which featured a session with the same title. Topics in this volume include: analytical methods and data quality experimental constraints applied to understanding HSE partitioning nucleosynthetic variations of siderophile and chalcophile elements HSE in the Earth, Moon, Mars and asteroidal bodies HSE and chalcophile elements in both cratonic and non-cratonic mantle, encompassing both sub-continental and sub-oceanic lithosphere the importance of the HSE for studying volcanic and magmatic processes, and an appraisal of the importance of magmatic HSE ore formation in Earth’s crust. Highly siderophile and strongly chalcophile elements comprise Re, Os, Ir, Ru, Pt, Rh, Pd, Au, Te, Se and S and are defined by their strong partitioning into the metallic phase, but will also strongly partition into sulfide phases, in the absence of metal. The chemical properties of the HSE mean that they are excellent tracers of key processes in high temperature geochemistry and cosmochemistry, having applications in virtually all areas of earth science. A key aspect of the HSE is that three long-lived, geologically useful decay systems exist with the HSE as parent (107Pd-107Ag), or parent-daughter isotopes ( |
| Beschreibung: | 1 Online-Ressource (XXIII, 774 Seiten) Illustrationen, Diagramme |
| ISBN: | 9781501502095 |
| DOI: | 10.1515/9781501502095 |
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| illustrated | Not Illustrated |
| indexdate | 2024-07-10T07:30:39Z |
| institution | BVB |
| isbn | 9781501502095 |
| language | English |
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| spelling | Highly siderophile and strongly chalcophile elements in high-temperature geochemistry and cosmochemistry editors Jason Harvey (University of Leeds, UK), James M.D. Day (Scripps Institution of Oceanography, USA) [Berlin ; Boston] De Gruyter [2016] Chantilly, Virginia, U.S.A. Mineralogical Society of America [2016] © 2016 1 Online-Ressource (XXIII, 774 Seiten) Illustrationen, Diagramme txt rdacontent c rdamedia cr rdacarrier Reviews in Mineralogy & Geochemistry volume 81 Highly Siderophile and Strongly Chalcophile Elements in High Temperature Geochemistry and Cosmochemistry, Volume 81 This RiMG (Reviews in Mineralogy & Geochemistry) volume investigates the application of highly siderophile (HSE) and strongly chalcophile elements. This volume has its origin in a short course sponsored by the Mineralogical Society of America and the Geochemical Society held in San Diego, California on the 11th and 12th December 2015, ahead of the American Geophysical Union’s Fall Meeting, which featured a session with the same title. Topics in this volume include: analytical methods and data quality experimental constraints applied to understanding HSE partitioning nucleosynthetic variations of siderophile and chalcophile elements HSE in the Earth, Moon, Mars and asteroidal bodies HSE and chalcophile elements in both cratonic and non-cratonic mantle, encompassing both sub-continental and sub-oceanic lithosphere the importance of the HSE for studying volcanic and magmatic processes, and an appraisal of the importance of magmatic HSE ore formation in Earth’s crust. Highly siderophile and strongly chalcophile elements comprise Re, Os, Ir, Ru, Pt, Rh, Pd, Au, Te, Se and S and are defined by their strong partitioning into the metallic phase, but will also strongly partition into sulfide phases, in the absence of metal. The chemical properties of the HSE mean that they are excellent tracers of key processes in high temperature geochemistry and cosmochemistry, having applications in virtually all areas of earth science. A key aspect of the HSE is that three long-lived, geologically useful decay systems exist with the HSE as parent (107Pd-107Ag), or parent-daughter isotopes ( Geochemie (DE-588)4020198-3 gnd rswk-swf Siderophiles Element (DE-588)4433794-2 gnd rswk-swf Geochemie (DE-588)4020198-3 s Siderophiles Element (DE-588)4433794-2 s DE-604 Harvey, Jason (DE-588)1082055727 edt Day, James M. D. (DE-588)1082091324 edt Erscheint auch als Druck-Ausgabe 978-0-939950-97-3 Erscheint auch als Online-Ausgabe, Bundle 978-1-5015-0210-1 Reviews in Mineralogy & Geochemistry volume 81 (DE-604)BV019787764 81 https://doi.org/10.1515/9781501502095 Verlag URL des Erstveröffentlichers Volltext |
| spellingShingle | Highly siderophile and strongly chalcophile elements in high-temperature geochemistry and cosmochemistry Reviews in Mineralogy & Geochemistry Geochemie (DE-588)4020198-3 gnd Siderophiles Element (DE-588)4433794-2 gnd |
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| title | Highly siderophile and strongly chalcophile elements in high-temperature geochemistry and cosmochemistry |
| title_auth | Highly siderophile and strongly chalcophile elements in high-temperature geochemistry and cosmochemistry |
| title_exact_search | Highly siderophile and strongly chalcophile elements in high-temperature geochemistry and cosmochemistry |
| title_full | Highly siderophile and strongly chalcophile elements in high-temperature geochemistry and cosmochemistry editors Jason Harvey (University of Leeds, UK), James M.D. Day (Scripps Institution of Oceanography, USA) |
| title_fullStr | Highly siderophile and strongly chalcophile elements in high-temperature geochemistry and cosmochemistry editors Jason Harvey (University of Leeds, UK), James M.D. Day (Scripps Institution of Oceanography, USA) |
| title_full_unstemmed | Highly siderophile and strongly chalcophile elements in high-temperature geochemistry and cosmochemistry editors Jason Harvey (University of Leeds, UK), James M.D. Day (Scripps Institution of Oceanography, USA) |
| title_short | Highly siderophile and strongly chalcophile elements in high-temperature geochemistry and cosmochemistry |
| title_sort | highly siderophile and strongly chalcophile elements in high temperature geochemistry and cosmochemistry |
| topic | Geochemie (DE-588)4020198-3 gnd Siderophiles Element (DE-588)4433794-2 gnd |
| topic_facet | Geochemie Siderophiles Element |
| url | https://doi.org/10.1515/9781501502095 |
| volume_link | (DE-604)BV019787764 |
| work_keys_str_mv | AT harveyjason highlysiderophileandstronglychalcophileelementsinhightemperaturegeochemistryandcosmochemistry AT dayjamesmd highlysiderophileandstronglychalcophileelementsinhightemperaturegeochemistryandcosmochemistry |