K-Ar Radiometric Age Determinations of White Micas from the Piemont Zone, French-Italian Western Alps

Abstract K - Ar radiometric data are presented suggesting a different metamorphic history for both parts of the Piemont zone in the Western Alps: the Combin zone to the west, considered to have escaped the late Cretaceous metamorphic event, and the Zermatt-Saas zone to the east, where ophiolites pre...
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Autor*in:	Delaloye, Michel [verfasserIn] Desmons, Jacqueline

Format:	Artikel
Sprache:	Englisch

Erschienen:	1976

Systematik:	TE 1000

Anmerkung:	© Springer-Verlag 1976

Übergeordnetes Werk:	Enthalten in: Contributions to mineralogy and petrology - Springer Berlin Heidelberg, 1966, 57(1976), 3 vom: 01. Sept., Seite 297-303
Übergeordnetes Werk:	volume:57 ; year:1976 ; number:3 ; day:01 ; month:09 ; pages:297-303

Links:	Volltext

DOI / URN:	10.1007/BF03542939

Katalog-ID:	OLC2070489361

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allfields	10.1007/BF03542939 doi (DE-627)OLC2070489361 (DE-He213)BF03542939-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Delaloye, Michel verfasserin aut K-Ar Radiometric Age Determinations of White Micas from the Piemont Zone, French-Italian Western Alps 1976 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1976 Abstract K - Ar radiometric data are presented suggesting a different metamorphic history for both parts of the Piemont zone in the Western Alps: the Combin zone to the west, considered to have escaped the late Cretaceous metamorphic event, and the Zermatt-Saas zone to the east, where ophiolites predominate, and which has been affected by a first metamorphism during late Cretaceous. Paragonite lenses within serpentinite give an isotopic ratio dating a serpentinization phase, or representing mixed ages. Late Cretaceous ages are found in the Zermatt-Saas zone and in the melange areas. The Combin zone gives only Eocene-Oligocene ages, as well as that part of the Zermatt-Saas zone that is closer to the Lepontine thermal high (dated as 38 m.y.). No late Oligocene-early Miocene ages (as previously obtained on Na-amphiboles) have been found among the investigated micas. Desmons, Jacqueline aut Enthalten in Contributions to mineralogy and petrology Springer Berlin Heidelberg, 1966 57(1976), 3 vom: 01. Sept., Seite 297-303 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:57 year:1976 number:3 day:01 month:09 pages:297-303 https://doi.org/10.1007/BF03542939 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2001 GBV_ILN_2004 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4323 TE 1000 AR 57 1976 3 01 09 297-303
spelling	10.1007/BF03542939 doi (DE-627)OLC2070489361 (DE-He213)BF03542939-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Delaloye, Michel verfasserin aut K-Ar Radiometric Age Determinations of White Micas from the Piemont Zone, French-Italian Western Alps 1976 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1976 Abstract K - Ar radiometric data are presented suggesting a different metamorphic history for both parts of the Piemont zone in the Western Alps: the Combin zone to the west, considered to have escaped the late Cretaceous metamorphic event, and the Zermatt-Saas zone to the east, where ophiolites predominate, and which has been affected by a first metamorphism during late Cretaceous. Paragonite lenses within serpentinite give an isotopic ratio dating a serpentinization phase, or representing mixed ages. Late Cretaceous ages are found in the Zermatt-Saas zone and in the melange areas. The Combin zone gives only Eocene-Oligocene ages, as well as that part of the Zermatt-Saas zone that is closer to the Lepontine thermal high (dated as 38 m.y.). No late Oligocene-early Miocene ages (as previously obtained on Na-amphiboles) have been found among the investigated micas. Desmons, Jacqueline aut Enthalten in Contributions to mineralogy and petrology Springer Berlin Heidelberg, 1966 57(1976), 3 vom: 01. Sept., Seite 297-303 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:57 year:1976 number:3 day:01 month:09 pages:297-303 https://doi.org/10.1007/BF03542939 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2001 GBV_ILN_2004 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4323 TE 1000 AR 57 1976 3 01 09 297-303
allfields_unstemmed	10.1007/BF03542939 doi (DE-627)OLC2070489361 (DE-He213)BF03542939-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Delaloye, Michel verfasserin aut K-Ar Radiometric Age Determinations of White Micas from the Piemont Zone, French-Italian Western Alps 1976 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1976 Abstract K - Ar radiometric data are presented suggesting a different metamorphic history for both parts of the Piemont zone in the Western Alps: the Combin zone to the west, considered to have escaped the late Cretaceous metamorphic event, and the Zermatt-Saas zone to the east, where ophiolites predominate, and which has been affected by a first metamorphism during late Cretaceous. Paragonite lenses within serpentinite give an isotopic ratio dating a serpentinization phase, or representing mixed ages. Late Cretaceous ages are found in the Zermatt-Saas zone and in the melange areas. The Combin zone gives only Eocene-Oligocene ages, as well as that part of the Zermatt-Saas zone that is closer to the Lepontine thermal high (dated as 38 m.y.). No late Oligocene-early Miocene ages (as previously obtained on Na-amphiboles) have been found among the investigated micas. Desmons, Jacqueline aut Enthalten in Contributions to mineralogy and petrology Springer Berlin Heidelberg, 1966 57(1976), 3 vom: 01. Sept., Seite 297-303 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:57 year:1976 number:3 day:01 month:09 pages:297-303 https://doi.org/10.1007/BF03542939 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2001 GBV_ILN_2004 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4323 TE 1000 AR 57 1976 3 01 09 297-303
allfieldsGer	10.1007/BF03542939 doi (DE-627)OLC2070489361 (DE-He213)BF03542939-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Delaloye, Michel verfasserin aut K-Ar Radiometric Age Determinations of White Micas from the Piemont Zone, French-Italian Western Alps 1976 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1976 Abstract K - Ar radiometric data are presented suggesting a different metamorphic history for both parts of the Piemont zone in the Western Alps: the Combin zone to the west, considered to have escaped the late Cretaceous metamorphic event, and the Zermatt-Saas zone to the east, where ophiolites predominate, and which has been affected by a first metamorphism during late Cretaceous. Paragonite lenses within serpentinite give an isotopic ratio dating a serpentinization phase, or representing mixed ages. Late Cretaceous ages are found in the Zermatt-Saas zone and in the melange areas. The Combin zone gives only Eocene-Oligocene ages, as well as that part of the Zermatt-Saas zone that is closer to the Lepontine thermal high (dated as 38 m.y.). No late Oligocene-early Miocene ages (as previously obtained on Na-amphiboles) have been found among the investigated micas. Desmons, Jacqueline aut Enthalten in Contributions to mineralogy and petrology Springer Berlin Heidelberg, 1966 57(1976), 3 vom: 01. Sept., Seite 297-303 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:57 year:1976 number:3 day:01 month:09 pages:297-303 https://doi.org/10.1007/BF03542939 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2001 GBV_ILN_2004 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4323 TE 1000 AR 57 1976 3 01 09 297-303
allfieldsSound	10.1007/BF03542939 doi (DE-627)OLC2070489361 (DE-He213)BF03542939-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Delaloye, Michel verfasserin aut K-Ar Radiometric Age Determinations of White Micas from the Piemont Zone, French-Italian Western Alps 1976 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1976 Abstract K - Ar radiometric data are presented suggesting a different metamorphic history for both parts of the Piemont zone in the Western Alps: the Combin zone to the west, considered to have escaped the late Cretaceous metamorphic event, and the Zermatt-Saas zone to the east, where ophiolites predominate, and which has been affected by a first metamorphism during late Cretaceous. Paragonite lenses within serpentinite give an isotopic ratio dating a serpentinization phase, or representing mixed ages. Late Cretaceous ages are found in the Zermatt-Saas zone and in the melange areas. The Combin zone gives only Eocene-Oligocene ages, as well as that part of the Zermatt-Saas zone that is closer to the Lepontine thermal high (dated as 38 m.y.). No late Oligocene-early Miocene ages (as previously obtained on Na-amphiboles) have been found among the investigated micas. Desmons, Jacqueline aut Enthalten in Contributions to mineralogy and petrology Springer Berlin Heidelberg, 1966 57(1976), 3 vom: 01. Sept., Seite 297-303 (DE-627)129068721 (DE-600)1616-0 (DE-576)014400367 0010-7999 nnns volume:57 year:1976 number:3 day:01 month:09 pages:297-303 https://doi.org/10.1007/BF03542939 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_22 GBV_ILN_30 GBV_ILN_31 GBV_ILN_40 GBV_ILN_62 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2001 GBV_ILN_2004 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4028 GBV_ILN_4035 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4277 GBV_ILN_4302 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4311 GBV_ILN_4319 GBV_ILN_4320 GBV_ILN_4323 TE 1000 AR 57 1976 3 01 09 297-303
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source	Enthalten in Contributions to mineralogy and petrology 57(1976), 3 vom: 01. Sept., Seite 297-303 volume:57 year:1976 number:3 day:01 month:09 pages:297-303
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author	Delaloye, Michel
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title	K-Ar Radiometric Age Determinations of White Micas from the Piemont Zone, French-Italian Western Alps
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title_full	K-Ar Radiometric Age Determinations of White Micas from the Piemont Zone, French-Italian Western Alps
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title_sort	k-ar radiometric age determinations of white micas from the piemont zone, french-italian western alps
title_auth	K-Ar Radiometric Age Determinations of White Micas from the Piemont Zone, French-Italian Western Alps
abstract	Abstract K - Ar radiometric data are presented suggesting a different metamorphic history for both parts of the Piemont zone in the Western Alps: the Combin zone to the west, considered to have escaped the late Cretaceous metamorphic event, and the Zermatt-Saas zone to the east, where ophiolites predominate, and which has been affected by a first metamorphism during late Cretaceous. Paragonite lenses within serpentinite give an isotopic ratio dating a serpentinization phase, or representing mixed ages. Late Cretaceous ages are found in the Zermatt-Saas zone and in the melange areas. The Combin zone gives only Eocene-Oligocene ages, as well as that part of the Zermatt-Saas zone that is closer to the Lepontine thermal high (dated as 38 m.y.). No late Oligocene-early Miocene ages (as previously obtained on Na-amphiboles) have been found among the investigated micas. © Springer-Verlag 1976
abstractGer	Abstract K - Ar radiometric data are presented suggesting a different metamorphic history for both parts of the Piemont zone in the Western Alps: the Combin zone to the west, considered to have escaped the late Cretaceous metamorphic event, and the Zermatt-Saas zone to the east, where ophiolites predominate, and which has been affected by a first metamorphism during late Cretaceous. Paragonite lenses within serpentinite give an isotopic ratio dating a serpentinization phase, or representing mixed ages. Late Cretaceous ages are found in the Zermatt-Saas zone and in the melange areas. The Combin zone gives only Eocene-Oligocene ages, as well as that part of the Zermatt-Saas zone that is closer to the Lepontine thermal high (dated as 38 m.y.). No late Oligocene-early Miocene ages (as previously obtained on Na-amphiboles) have been found among the investigated micas. © Springer-Verlag 1976
abstract_unstemmed	Abstract K - Ar radiometric data are presented suggesting a different metamorphic history for both parts of the Piemont zone in the Western Alps: the Combin zone to the west, considered to have escaped the late Cretaceous metamorphic event, and the Zermatt-Saas zone to the east, where ophiolites predominate, and which has been affected by a first metamorphism during late Cretaceous. Paragonite lenses within serpentinite give an isotopic ratio dating a serpentinization phase, or representing mixed ages. Late Cretaceous ages are found in the Zermatt-Saas zone and in the melange areas. The Combin zone gives only Eocene-Oligocene ages, as well as that part of the Zermatt-Saas zone that is closer to the Lepontine thermal high (dated as 38 m.y.). No late Oligocene-early Miocene ages (as previously obtained on Na-amphiboles) have been found among the investigated micas. © Springer-Verlag 1976
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title_short	K-Ar Radiometric Age Determinations of White Micas from the Piemont Zone, French-Italian Western Alps
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