Andean Magmatism: Chemical and Isotopic Constraints
Destructive plate margin magmagenesis is one of the most intensely studied and widely debated topics in the earth sciences at present. Calc-alkaline volcanic and plutonic rocks in orogenic settings exhibit such a diversity of composition and character that the subducted oceanic lithosphere, the over...
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| Format: | Elektronisch E-Book |
| Sprache: | English |
| Veröffentlicht: |
Boston, MA
Birkhuser Boston
1984
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| Online-Zugang: | BTU01 Volltext |
| Zusammenfassung: | Destructive plate margin magmagenesis is one of the most intensely studied and widely debated topics in the earth sciences at present. Calc-alkaline volcanic and plutonic rocks in orogenic settings exhibit such a diversity of composition and character that the subducted oceanic lithosphere, the overlying 'enriched' lithospheric mantle and the lower continental crust all have been advocated recently as the primary source region for island-arc and continental-margin basaltic to andesitic magmas. The role of the upper continental crust is also a matter of continuing controversy. It is clear that crustal contamination is a common, but not universal, feature of destructive plate margin magmatism. Whether this contamination is introduced at source by subduction-related processes or occurs during magma transit by bulk anatexis and magma mixing, selective contamination or coupled fractional crystallization-assimilation mechanisms is central to most current discussions of andesite petrogenesis. This book presents a series of papers which directly address these and other important geological and geochemical problems within the context of the Mesozoic-Cenozoic calc-alkaline magmatism characteristic of the Andean Cordillera of western South America. Although it is aimed primarily at postgraduate students and researchers familiar with the Andes, it is also a useful general reference for workers in other fields who wish to gain an insight into current thoughts, ideas and speculations on 'andesitic' magmatism at destructive plate margins |
| Beschreibung: | 1 Online-Ressource (X, 252 p) |
| ISBN: | 9781468473353 |
| DOI: | 10.1007/978-1-4684-7335-3 |
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| 520 | |a Destructive plate margin magmagenesis is one of the most intensely studied and widely debated topics in the earth sciences at present. Calc-alkaline volcanic and plutonic rocks in orogenic settings exhibit such a diversity of composition and character that the subducted oceanic lithosphere, the overlying 'enriched' lithospheric mantle and the lower continental crust all have been advocated recently as the primary source region for island-arc and continental-margin basaltic to andesitic magmas. The role of the upper continental crust is also a matter of continuing controversy. It is clear that crustal contamination is a common, but not universal, feature of destructive plate margin magmatism. Whether this contamination is introduced at source by subduction-related processes or occurs during magma transit by bulk anatexis and magma mixing, selective contamination or coupled fractional crystallization-assimilation mechanisms is central to most current discussions of andesite petrogenesis. This book presents a series of papers which directly address these and other important geological and geochemical problems within the context of the Mesozoic-Cenozoic calc-alkaline magmatism characteristic of the Andean Cordillera of western South America. Although it is aimed primarily at postgraduate students and researchers familiar with the Andes, it is also a useful general reference for workers in other fields who wish to gain an insight into current thoughts, ideas and speculations on 'andesitic' magmatism at destructive plate margins | ||
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| 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 |
| doi_str_mv | 10.1007/978-1-4684-7335-3 |
| format | Electronic eBook |
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S. Harmon, B. A. Barreiro</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="a">Boston, MA</subfield><subfield code="b">Birkhuser Boston</subfield><subfield code="c">1984</subfield></datafield><datafield tag="300" ind1=" " ind2=" "><subfield code="a">1 Online-Ressource (X, 252 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="520" ind1=" " ind2=" "><subfield code="a">Destructive plate margin magmagenesis is one of the most intensely studied and widely debated topics in the earth sciences at present. 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| id | DE-604.BV045178285 |
| illustrated | Not Illustrated |
| indexdate | 2024-07-10T08:10:48Z |
| institution | BVB |
| isbn | 9781468473353 |
| language | English |
| oai_aleph_id | oai:aleph.bib-bvb.de:BVB01-030567515 |
| oclc_num | 1053822990 |
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| physical | 1 Online-Ressource (X, 252 p) |
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| publishDate | 1984 |
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| publisher | Birkhuser Boston |
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| spelling | Andean Magmatism Chemical and Isotopic Constraints edited by R. S. Harmon, B. A. Barreiro Boston, MA Birkhuser Boston 1984 1 Online-Ressource (X, 252 p) txt rdacontent c rdamedia cr rdacarrier Destructive plate margin magmagenesis is one of the most intensely studied and widely debated topics in the earth sciences at present. Calc-alkaline volcanic and plutonic rocks in orogenic settings exhibit such a diversity of composition and character that the subducted oceanic lithosphere, the overlying 'enriched' lithospheric mantle and the lower continental crust all have been advocated recently as the primary source region for island-arc and continental-margin basaltic to andesitic magmas. The role of the upper continental crust is also a matter of continuing controversy. It is clear that crustal contamination is a common, but not universal, feature of destructive plate margin magmatism. Whether this contamination is introduced at source by subduction-related processes or occurs during magma transit by bulk anatexis and magma mixing, selective contamination or coupled fractional crystallization-assimilation mechanisms is central to most current discussions of andesite petrogenesis. This book presents a series of papers which directly address these and other important geological and geochemical problems within the context of the Mesozoic-Cenozoic calc-alkaline magmatism characteristic of the Andean Cordillera of western South America. Although it is aimed primarily at postgraduate students and researchers familiar with the Andes, it is also a useful general reference for workers in other fields who wish to gain an insight into current thoughts, ideas and speculations on 'andesitic' magmatism at destructive plate margins Earth Sciences Geochemistry Science, general Earth sciences Science Harmon, R. S. edt Barreiro, B. A. edt Erscheint auch als Druck-Ausgabe 9781468473377 https://doi.org/10.1007/978-1-4684-7335-3 Verlag URL des Erstveröffentlichers Volltext |
| spellingShingle | Andean Magmatism Chemical and Isotopic Constraints Earth Sciences Geochemistry Science, general Earth sciences Science |
| title | Andean Magmatism Chemical and Isotopic Constraints |
| title_auth | Andean Magmatism Chemical and Isotopic Constraints |
| title_exact_search | Andean Magmatism Chemical and Isotopic Constraints |
| title_full | Andean Magmatism Chemical and Isotopic Constraints edited by R. S. Harmon, B. A. Barreiro |
| title_fullStr | Andean Magmatism Chemical and Isotopic Constraints edited by R. S. Harmon, B. A. Barreiro |
| title_full_unstemmed | Andean Magmatism Chemical and Isotopic Constraints edited by R. S. Harmon, B. A. Barreiro |
| title_short | Andean Magmatism |
| title_sort | andean magmatism chemical and isotopic constraints |
| title_sub | Chemical and Isotopic Constraints |
| topic | Earth Sciences Geochemistry Science, general Earth sciences Science |
| topic_facet | Earth Sciences Geochemistry Science, general Earth sciences Science |
| url | https://doi.org/10.1007/978-1-4684-7335-3 |
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