Short-duration regional metamorphic event recorded in a Variscan subduction channel (Malpica–Tui eclogites, NW Iberia)

Abstract An isotopic resetting event is disclosed at ca. 350 Ma, based on Rb–Sr isotopic analyses (whole rock, garnet, clinopyroxene and phengite fractions) of eclogites with coronitic garnet and planolinear eclogites from the Malpica–Tui Allochthonous Complex (NW Iberia). The eclogites were buried,...
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Autor*in:	Beranoaguirre, A. [verfasserIn] Puelles, P. [verfasserIn] Ábalos, B. [verfasserIn] Gil Ibarguchi, J. I. [verfasserIn] García de Madinabeitia, S. [verfasserIn]

Format:	E-Artikel
Sprache:	Englisch

Erschienen:	2019

Schlagwörter:	Eclogite Petrochronology Variscan Malpica–Tui NW Iberia

Übergeordnetes Werk:	Enthalten in: Geologische Rundschau - Berlin : Springer, 1910, 108(2019), 6 vom: 19. Juli, Seite 2037-2046
Übergeordnetes Werk:	volume:108 ; year:2019 ; number:6 ; day:19 ; month:07 ; pages:2037-2046

Links:	Volltext

DOI / URN:	10.1007/s00531-019-01747-1

Katalog-ID:	SPR006732070

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520			\|a Abstract An isotopic resetting event is disclosed at ca. 350 Ma, based on Rb–Sr isotopic analyses (whole rock, garnet, clinopyroxene and phengite fractions) of eclogites with coronitic garnet and planolinear eclogites from the Malpica–Tui Allochthonous Complex (NW Iberia). The eclogites were buried, deformed/recrystallized and subsequently exhumed in a Late Devonian subduction channel. Lu–Hf and Sm–Nd isotopes date a ca. 375-Ma metamorphic peak of the subduction–exhumation cycle that occurred under ~ 2.6 GPa and 610–640 °C and was overprinted by the 350-Ma event, which occurred still under high-pressure conditions. The latter resetting is interpreted as a very short-duration regional metamorphic phenomenon recorded by high-pressure rocks in the west European Variscan belt at time scales shorter than those characteristic of orogenic lithosphere in subduction/collision cycles.
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allfields	10.1007/s00531-019-01747-1 doi (DE-627)SPR006732070 (SPR)s00531-019-01747-1-e DE-627 ger DE-627 rakwb eng 550 ASE 38.10 bkl Beranoaguirre, A. verfasserin aut Short-duration regional metamorphic event recorded in a Variscan subduction channel (Malpica–Tui eclogites, NW Iberia) 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract An isotopic resetting event is disclosed at ca. 350 Ma, based on Rb–Sr isotopic analyses (whole rock, garnet, clinopyroxene and phengite fractions) of eclogites with coronitic garnet and planolinear eclogites from the Malpica–Tui Allochthonous Complex (NW Iberia). The eclogites were buried, deformed/recrystallized and subsequently exhumed in a Late Devonian subduction channel. Lu–Hf and Sm–Nd isotopes date a ca. 375-Ma metamorphic peak of the subduction–exhumation cycle that occurred under ~ 2.6 GPa and 610–640 °C and was overprinted by the 350-Ma event, which occurred still under high-pressure conditions. The latter resetting is interpreted as a very short-duration regional metamorphic phenomenon recorded by high-pressure rocks in the west European Variscan belt at time scales shorter than those characteristic of orogenic lithosphere in subduction/collision cycles. Eclogite (dpeaa)DE-He213 Petrochronology (dpeaa)DE-He213 Variscan (dpeaa)DE-He213 Malpica–Tui (dpeaa)DE-He213 NW Iberia (dpeaa)DE-He213 Puelles, P. verfasserin aut Ábalos, B. verfasserin aut Gil Ibarguchi, J. I. verfasserin aut García de Madinabeitia, S. verfasserin aut Enthalten in Geologische Rundschau Berlin : Springer, 1910 108(2019), 6 vom: 19. Juli, Seite 2037-2046 (DE-627)47265019X (DE-600)2168407-8 1432-1149 nnns volume:108 year:2019 number:6 day:19 month:07 pages:2037-2046 https://dx.doi.org/10.1007/s00531-019-01747-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 38.10 ASE AR 108 2019 6 19 07 2037-2046
spelling	10.1007/s00531-019-01747-1 doi (DE-627)SPR006732070 (SPR)s00531-019-01747-1-e DE-627 ger DE-627 rakwb eng 550 ASE 38.10 bkl Beranoaguirre, A. verfasserin aut Short-duration regional metamorphic event recorded in a Variscan subduction channel (Malpica–Tui eclogites, NW Iberia) 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract An isotopic resetting event is disclosed at ca. 350 Ma, based on Rb–Sr isotopic analyses (whole rock, garnet, clinopyroxene and phengite fractions) of eclogites with coronitic garnet and planolinear eclogites from the Malpica–Tui Allochthonous Complex (NW Iberia). The eclogites were buried, deformed/recrystallized and subsequently exhumed in a Late Devonian subduction channel. Lu–Hf and Sm–Nd isotopes date a ca. 375-Ma metamorphic peak of the subduction–exhumation cycle that occurred under ~ 2.6 GPa and 610–640 °C and was overprinted by the 350-Ma event, which occurred still under high-pressure conditions. The latter resetting is interpreted as a very short-duration regional metamorphic phenomenon recorded by high-pressure rocks in the west European Variscan belt at time scales shorter than those characteristic of orogenic lithosphere in subduction/collision cycles. Eclogite (dpeaa)DE-He213 Petrochronology (dpeaa)DE-He213 Variscan (dpeaa)DE-He213 Malpica–Tui (dpeaa)DE-He213 NW Iberia (dpeaa)DE-He213 Puelles, P. verfasserin aut Ábalos, B. verfasserin aut Gil Ibarguchi, J. I. verfasserin aut García de Madinabeitia, S. verfasserin aut Enthalten in Geologische Rundschau Berlin : Springer, 1910 108(2019), 6 vom: 19. Juli, Seite 2037-2046 (DE-627)47265019X (DE-600)2168407-8 1432-1149 nnns volume:108 year:2019 number:6 day:19 month:07 pages:2037-2046 https://dx.doi.org/10.1007/s00531-019-01747-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 38.10 ASE AR 108 2019 6 19 07 2037-2046
allfields_unstemmed	10.1007/s00531-019-01747-1 doi (DE-627)SPR006732070 (SPR)s00531-019-01747-1-e DE-627 ger DE-627 rakwb eng 550 ASE 38.10 bkl Beranoaguirre, A. verfasserin aut Short-duration regional metamorphic event recorded in a Variscan subduction channel (Malpica–Tui eclogites, NW Iberia) 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract An isotopic resetting event is disclosed at ca. 350 Ma, based on Rb–Sr isotopic analyses (whole rock, garnet, clinopyroxene and phengite fractions) of eclogites with coronitic garnet and planolinear eclogites from the Malpica–Tui Allochthonous Complex (NW Iberia). The eclogites were buried, deformed/recrystallized and subsequently exhumed in a Late Devonian subduction channel. Lu–Hf and Sm–Nd isotopes date a ca. 375-Ma metamorphic peak of the subduction–exhumation cycle that occurred under ~ 2.6 GPa and 610–640 °C and was overprinted by the 350-Ma event, which occurred still under high-pressure conditions. The latter resetting is interpreted as a very short-duration regional metamorphic phenomenon recorded by high-pressure rocks in the west European Variscan belt at time scales shorter than those characteristic of orogenic lithosphere in subduction/collision cycles. Eclogite (dpeaa)DE-He213 Petrochronology (dpeaa)DE-He213 Variscan (dpeaa)DE-He213 Malpica–Tui (dpeaa)DE-He213 NW Iberia (dpeaa)DE-He213 Puelles, P. verfasserin aut Ábalos, B. verfasserin aut Gil Ibarguchi, J. I. verfasserin aut García de Madinabeitia, S. verfasserin aut Enthalten in Geologische Rundschau Berlin : Springer, 1910 108(2019), 6 vom: 19. Juli, Seite 2037-2046 (DE-627)47265019X (DE-600)2168407-8 1432-1149 nnns volume:108 year:2019 number:6 day:19 month:07 pages:2037-2046 https://dx.doi.org/10.1007/s00531-019-01747-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 38.10 ASE AR 108 2019 6 19 07 2037-2046
allfieldsGer	10.1007/s00531-019-01747-1 doi (DE-627)SPR006732070 (SPR)s00531-019-01747-1-e DE-627 ger DE-627 rakwb eng 550 ASE 38.10 bkl Beranoaguirre, A. verfasserin aut Short-duration regional metamorphic event recorded in a Variscan subduction channel (Malpica–Tui eclogites, NW Iberia) 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract An isotopic resetting event is disclosed at ca. 350 Ma, based on Rb–Sr isotopic analyses (whole rock, garnet, clinopyroxene and phengite fractions) of eclogites with coronitic garnet and planolinear eclogites from the Malpica–Tui Allochthonous Complex (NW Iberia). The eclogites were buried, deformed/recrystallized and subsequently exhumed in a Late Devonian subduction channel. Lu–Hf and Sm–Nd isotopes date a ca. 375-Ma metamorphic peak of the subduction–exhumation cycle that occurred under ~ 2.6 GPa and 610–640 °C and was overprinted by the 350-Ma event, which occurred still under high-pressure conditions. The latter resetting is interpreted as a very short-duration regional metamorphic phenomenon recorded by high-pressure rocks in the west European Variscan belt at time scales shorter than those characteristic of orogenic lithosphere in subduction/collision cycles. Eclogite (dpeaa)DE-He213 Petrochronology (dpeaa)DE-He213 Variscan (dpeaa)DE-He213 Malpica–Tui (dpeaa)DE-He213 NW Iberia (dpeaa)DE-He213 Puelles, P. verfasserin aut Ábalos, B. verfasserin aut Gil Ibarguchi, J. I. verfasserin aut García de Madinabeitia, S. verfasserin aut Enthalten in Geologische Rundschau Berlin : Springer, 1910 108(2019), 6 vom: 19. Juli, Seite 2037-2046 (DE-627)47265019X (DE-600)2168407-8 1432-1149 nnns volume:108 year:2019 number:6 day:19 month:07 pages:2037-2046 https://dx.doi.org/10.1007/s00531-019-01747-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 38.10 ASE AR 108 2019 6 19 07 2037-2046
allfieldsSound	10.1007/s00531-019-01747-1 doi (DE-627)SPR006732070 (SPR)s00531-019-01747-1-e DE-627 ger DE-627 rakwb eng 550 ASE 38.10 bkl Beranoaguirre, A. verfasserin aut Short-duration regional metamorphic event recorded in a Variscan subduction channel (Malpica–Tui eclogites, NW Iberia) 2019 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract An isotopic resetting event is disclosed at ca. 350 Ma, based on Rb–Sr isotopic analyses (whole rock, garnet, clinopyroxene and phengite fractions) of eclogites with coronitic garnet and planolinear eclogites from the Malpica–Tui Allochthonous Complex (NW Iberia). The eclogites were buried, deformed/recrystallized and subsequently exhumed in a Late Devonian subduction channel. Lu–Hf and Sm–Nd isotopes date a ca. 375-Ma metamorphic peak of the subduction–exhumation cycle that occurred under ~ 2.6 GPa and 610–640 °C and was overprinted by the 350-Ma event, which occurred still under high-pressure conditions. The latter resetting is interpreted as a very short-duration regional metamorphic phenomenon recorded by high-pressure rocks in the west European Variscan belt at time scales shorter than those characteristic of orogenic lithosphere in subduction/collision cycles. Eclogite (dpeaa)DE-He213 Petrochronology (dpeaa)DE-He213 Variscan (dpeaa)DE-He213 Malpica–Tui (dpeaa)DE-He213 NW Iberia (dpeaa)DE-He213 Puelles, P. verfasserin aut Ábalos, B. verfasserin aut Gil Ibarguchi, J. I. verfasserin aut García de Madinabeitia, S. verfasserin aut Enthalten in Geologische Rundschau Berlin : Springer, 1910 108(2019), 6 vom: 19. Juli, Seite 2037-2046 (DE-627)47265019X (DE-600)2168407-8 1432-1149 nnns volume:108 year:2019 number:6 day:19 month:07 pages:2037-2046 https://dx.doi.org/10.1007/s00531-019-01747-1 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-ASE GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_152 GBV_ILN_161 GBV_ILN_171 GBV_ILN_187 GBV_ILN_224 GBV_ILN_250 GBV_ILN_267 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_647 GBV_ILN_702 38.10 ASE AR 108 2019 6 19 07 2037-2046
language	English
source	Enthalten in Geologische Rundschau 108(2019), 6 vom: 19. Juli, Seite 2037-2046 volume:108 year:2019 number:6 day:19 month:07 pages:2037-2046
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authorswithroles_txt_mv	Beranoaguirre, A. @@aut@@ Puelles, P. @@aut@@ Ábalos, B. @@aut@@ Gil Ibarguchi, J. I. @@aut@@ García de Madinabeitia, S. @@aut@@
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author	Beranoaguirre, A.
spellingShingle	Beranoaguirre, A. ddc 550 bkl 38.10 misc Eclogite misc Petrochronology misc Variscan misc Malpica–Tui misc NW Iberia Short-duration regional metamorphic event recorded in a Variscan subduction channel (Malpica–Tui eclogites, NW Iberia)
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topic_title	550 ASE 38.10 bkl Short-duration regional metamorphic event recorded in a Variscan subduction channel (Malpica–Tui eclogites, NW Iberia) Eclogite (dpeaa)DE-He213 Petrochronology (dpeaa)DE-He213 Variscan (dpeaa)DE-He213 Malpica–Tui (dpeaa)DE-He213 NW Iberia (dpeaa)DE-He213
topic	ddc 550 bkl 38.10 misc Eclogite misc Petrochronology misc Variscan misc Malpica–Tui misc NW Iberia
topic_unstemmed	ddc 550 bkl 38.10 misc Eclogite misc Petrochronology misc Variscan misc Malpica–Tui misc NW Iberia
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title	Short-duration regional metamorphic event recorded in a Variscan subduction channel (Malpica–Tui eclogites, NW Iberia)
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title_full	Short-duration regional metamorphic event recorded in a Variscan subduction channel (Malpica–Tui eclogites, NW Iberia)
author_sort	Beranoaguirre, A.
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author_browse	Beranoaguirre, A. Puelles, P. Ábalos, B. Gil Ibarguchi, J. I. García de Madinabeitia, S.
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title_sort	short-duration regional metamorphic event recorded in a variscan subduction channel (malpica–tui eclogites, nw iberia)
title_auth	Short-duration regional metamorphic event recorded in a Variscan subduction channel (Malpica–Tui eclogites, NW Iberia)
abstract	Abstract An isotopic resetting event is disclosed at ca. 350 Ma, based on Rb–Sr isotopic analyses (whole rock, garnet, clinopyroxene and phengite fractions) of eclogites with coronitic garnet and planolinear eclogites from the Malpica–Tui Allochthonous Complex (NW Iberia). The eclogites were buried, deformed/recrystallized and subsequently exhumed in a Late Devonian subduction channel. Lu–Hf and Sm–Nd isotopes date a ca. 375-Ma metamorphic peak of the subduction–exhumation cycle that occurred under ~ 2.6 GPa and 610–640 °C and was overprinted by the 350-Ma event, which occurred still under high-pressure conditions. The latter resetting is interpreted as a very short-duration regional metamorphic phenomenon recorded by high-pressure rocks in the west European Variscan belt at time scales shorter than those characteristic of orogenic lithosphere in subduction/collision cycles.
abstractGer	Abstract An isotopic resetting event is disclosed at ca. 350 Ma, based on Rb–Sr isotopic analyses (whole rock, garnet, clinopyroxene and phengite fractions) of eclogites with coronitic garnet and planolinear eclogites from the Malpica–Tui Allochthonous Complex (NW Iberia). The eclogites were buried, deformed/recrystallized and subsequently exhumed in a Late Devonian subduction channel. Lu–Hf and Sm–Nd isotopes date a ca. 375-Ma metamorphic peak of the subduction–exhumation cycle that occurred under ~ 2.6 GPa and 610–640 °C and was overprinted by the 350-Ma event, which occurred still under high-pressure conditions. The latter resetting is interpreted as a very short-duration regional metamorphic phenomenon recorded by high-pressure rocks in the west European Variscan belt at time scales shorter than those characteristic of orogenic lithosphere in subduction/collision cycles.
abstract_unstemmed	Abstract An isotopic resetting event is disclosed at ca. 350 Ma, based on Rb–Sr isotopic analyses (whole rock, garnet, clinopyroxene and phengite fractions) of eclogites with coronitic garnet and planolinear eclogites from the Malpica–Tui Allochthonous Complex (NW Iberia). The eclogites were buried, deformed/recrystallized and subsequently exhumed in a Late Devonian subduction channel. Lu–Hf and Sm–Nd isotopes date a ca. 375-Ma metamorphic peak of the subduction–exhumation cycle that occurred under ~ 2.6 GPa and 610–640 °C and was overprinted by the 350-Ma event, which occurred still under high-pressure conditions. The latter resetting is interpreted as a very short-duration regional metamorphic phenomenon recorded by high-pressure rocks in the west European Variscan belt at time scales shorter than those characteristic of orogenic lithosphere in subduction/collision cycles.
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title_short	Short-duration regional metamorphic event recorded in a Variscan subduction channel (Malpica–Tui eclogites, NW Iberia)
url	https://dx.doi.org/10.1007/s00531-019-01747-1
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author2	Puelles, P. Ábalos, B. Gil Ibarguchi, J. I. García de Madinabeitia, S.
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up_date	2024-07-04T00:23:47.199Z
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The latter resetting is interpreted as a very short-duration regional metamorphic phenomenon recorded by high-pressure rocks in the west European Variscan belt at time scales shorter than those characteristic of orogenic lithosphere in subduction/collision cycles.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Eclogite</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Petrochronology</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Variscan</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Malpica–Tui</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">NW Iberia</subfield><subfield code="7">(dpeaa)DE-He213</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Puelles, P.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Ábalos, B.</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Gil Ibarguchi, J. 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Short-duration regional metamorphic event recorded in a Variscan subduction channel (Malpica–Tui eclogites, NW Iberia)

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