Petrography and geochemistry of late- to post-Variscan vaugnerite series rocks and calc-alkaline lamprophyres within a cordierite-bearing monzogranite (Sierra Bermeja Pluton, southern Iberian Massif)
The Sierra Bermeja Pluton (southern Central Iberian Zone, Iberian Massif) is a late-Variscan intrusive constituted by cordierite-bearing peraluminous monzogranites. Detailed field mapping has allowed to disclose the presence of several NE–SW trending longitudinal composite bodies, formed by either a...
| Authors: | , , , , |
|---|---|
| Format: | article |
| Publication Date: | 2018 |
| Country: | España |
| Institution: | Universidad del País Vasco |
| Repository: | Addi. Archivo Digital para la Docencia y la Investigación |
| OAI Identifier: | oai:addi.ehu.eus:10810/75554 |
| Online Access: | http://hdl.handle.net/10810/75554 |
| Access Level: | Open access |
| Keyword: | calc-alkaline lamprophyre Vaugnerite series redwitzite cordierite-bearing granite Iberian Massif |
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Petrography and geochemistry of late- to post-Variscan vaugnerite series rocks and calc-alkaline lamprophyres within a cordierite-bearing monzogranite (Sierra Bermeja Pluton, southern Iberian Massif)Errandonea Martín, JonSarrionandia-Ibarra Eguidazu, FernandoCarracedo Sánchez, ManuelGil Ibarguchi, José IgnacioEguíluz Alarcón, Luiscalc-alkaline lamprophyreVaugnerite seriesredwitzitecordierite-bearing graniteIberian MassifThe Sierra Bermeja Pluton (southern Central Iberian Zone, Iberian Massif) is a late-Variscan intrusive constituted by cordierite-bearing peraluminous monzogranites. Detailed field mapping has allowed to disclose the presence of several NE–SW trending longitudinal composite bodies, formed by either aphanitic or phaneritic mesocratic rocks. According to their petrography and geochemistry these rocks are categorized as calc-alkaline lamprophyres and vaugnerite series rocks. Their primary mineralogy is characterized by variable amounts of plagioclase, amphibole, clinopyroxene, biotite, K-feldspar, quartz and apatite. Broadly, they show low SiO2 content (49–56wt.%), and high MgO+FeOt (10–17wt.%), K2O (3–5wt.%), Ba (963–2095ppm), Sr (401–1149ppm) and Cr (87–330ppm) contents. Field scale observations suggest that vaugneritic rocks and lamprophyres would constitute two independent magma pulses. Vaugneritic dioritoids intruded as syn-plutonic dykes, whereas lamprophyres were emplaced after the almost complete consolidation of the host monzogranites. In this way, vaugnerite series rocks would be an evidence for the contemporaneity of crustal- and mantle-melting processes during a late-Variscan stage, while lamprophyres would represent the ending of this stage.This work has been supported financially by the Spanish Ministerio de Ciencia e Innovación (MINECO, grant CGL2015-63530-P) and the University of the Basque Country (UPV/EHU, Grupo Consolidado project GIU15/05).UB202520252018info:eu-repo/semantics/articleapplication/pdfhttp://hdl.handle.net/10810/75554reponame:Addi. Archivo Digital para la Docencia y la Investigacióninstname:Universidad del País VascoIngléshttps://revistes.ub.edu/index.php/GEOACTA/article/view/GeologicaActa2018.16.3.1info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-sa/4.0/(c) 2018 Geologica Acta. This work is licensed under a Creative Commons Attribution-ShareAlike 4.0 International License.oai:addi.ehu.eus:10810/755542026-06-18T09:23:17Z |
| dc.title.none.fl_str_mv |
Petrography and geochemistry of late- to post-Variscan vaugnerite series rocks and calc-alkaline lamprophyres within a cordierite-bearing monzogranite (Sierra Bermeja Pluton, southern Iberian Massif) |
| title |
Petrography and geochemistry of late- to post-Variscan vaugnerite series rocks and calc-alkaline lamprophyres within a cordierite-bearing monzogranite (Sierra Bermeja Pluton, southern Iberian Massif) |
| spellingShingle |
Petrography and geochemistry of late- to post-Variscan vaugnerite series rocks and calc-alkaline lamprophyres within a cordierite-bearing monzogranite (Sierra Bermeja Pluton, southern Iberian Massif) Errandonea Martín, Jon calc-alkaline lamprophyre Vaugnerite series redwitzite cordierite-bearing granite Iberian Massif |
| title_short |
Petrography and geochemistry of late- to post-Variscan vaugnerite series rocks and calc-alkaline lamprophyres within a cordierite-bearing monzogranite (Sierra Bermeja Pluton, southern Iberian Massif) |
| title_full |
Petrography and geochemistry of late- to post-Variscan vaugnerite series rocks and calc-alkaline lamprophyres within a cordierite-bearing monzogranite (Sierra Bermeja Pluton, southern Iberian Massif) |
| title_fullStr |
Petrography and geochemistry of late- to post-Variscan vaugnerite series rocks and calc-alkaline lamprophyres within a cordierite-bearing monzogranite (Sierra Bermeja Pluton, southern Iberian Massif) |
| title_full_unstemmed |
Petrography and geochemistry of late- to post-Variscan vaugnerite series rocks and calc-alkaline lamprophyres within a cordierite-bearing monzogranite (Sierra Bermeja Pluton, southern Iberian Massif) |
| title_sort |
Petrography and geochemistry of late- to post-Variscan vaugnerite series rocks and calc-alkaline lamprophyres within a cordierite-bearing monzogranite (Sierra Bermeja Pluton, southern Iberian Massif) |
| dc.creator.none.fl_str_mv |
Errandonea Martín, Jon Sarrionandia-Ibarra Eguidazu, Fernando Carracedo Sánchez, Manuel Gil Ibarguchi, José Ignacio Eguíluz Alarcón, Luis |
| author |
Errandonea Martín, Jon |
| author_facet |
Errandonea Martín, Jon Sarrionandia-Ibarra Eguidazu, Fernando Carracedo Sánchez, Manuel Gil Ibarguchi, José Ignacio Eguíluz Alarcón, Luis |
| author_role |
author |
| author2 |
Sarrionandia-Ibarra Eguidazu, Fernando Carracedo Sánchez, Manuel Gil Ibarguchi, José Ignacio Eguíluz Alarcón, Luis |
| author2_role |
author author author author |
| dc.subject.none.fl_str_mv |
calc-alkaline lamprophyre Vaugnerite series redwitzite cordierite-bearing granite Iberian Massif |
| topic |
calc-alkaline lamprophyre Vaugnerite series redwitzite cordierite-bearing granite Iberian Massif |
| description |
The Sierra Bermeja Pluton (southern Central Iberian Zone, Iberian Massif) is a late-Variscan intrusive constituted by cordierite-bearing peraluminous monzogranites. Detailed field mapping has allowed to disclose the presence of several NE–SW trending longitudinal composite bodies, formed by either aphanitic or phaneritic mesocratic rocks. According to their petrography and geochemistry these rocks are categorized as calc-alkaline lamprophyres and vaugnerite series rocks. Their primary mineralogy is characterized by variable amounts of plagioclase, amphibole, clinopyroxene, biotite, K-feldspar, quartz and apatite. Broadly, they show low SiO2 content (49–56wt.%), and high MgO+FeOt (10–17wt.%), K2O (3–5wt.%), Ba (963–2095ppm), Sr (401–1149ppm) and Cr (87–330ppm) contents. Field scale observations suggest that vaugneritic rocks and lamprophyres would constitute two independent magma pulses. Vaugneritic dioritoids intruded as syn-plutonic dykes, whereas lamprophyres were emplaced after the almost complete consolidation of the host monzogranites. In this way, vaugnerite series rocks would be an evidence for the contemporaneity of crustal- and mantle-melting processes during a late-Variscan stage, while lamprophyres would represent the ending of this stage. |
| publishDate |
2018 |
| dc.date.none.fl_str_mv |
2018 2025 2025 |
| dc.type.none.fl_str_mv |
info:eu-repo/semantics/article |
| format |
article |
| dc.identifier.none.fl_str_mv |
http://hdl.handle.net/10810/75554 |
| url |
http://hdl.handle.net/10810/75554 |
| dc.language.none.fl_str_mv |
Inglés |
| language_invalid_str_mv |
Inglés |
| dc.relation.none.fl_str_mv |
https://revistes.ub.edu/index.php/GEOACTA/article/view/GeologicaActa2018.16.3.1 |
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info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-sa/4.0/ |
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openAccess |
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http://creativecommons.org/licenses/by-sa/4.0/ |
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application/pdf |
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UB |
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UB |
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reponame:Addi. Archivo Digital para la Docencia y la Investigación instname:Universidad del País Vasco |
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