Reaction progress of clay minerals and carbonaceous matter in a contact metamorphic aureole (Torres del Paine intrusion, Chile)

<p>This study reports on reaction processes in a transition zone from contact to regional metamorphism by using Raman spectroscopy on carbonaceous matter (RSCM), illite “crystallinity” (Kübler index, KI), chlorite geothermometry, and thermal modeling. The thermal effect due to the emplacement...

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Main Authors: A. Süssenberger, S. T. Schmidt, F. H. Schmidt, M. F. G. Weinkauf
Format: Article
Language:English
Published: Copernicus Publications 2020-12-01
Series:European Journal of Mineralogy
Online Access:https://ejm.copernicus.org/articles/32/653/2020/ejm-32-653-2020.pdf
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spelling doaj-093990e710db433180701e445706ee432021-08-02T19:56:53ZengCopernicus PublicationsEuropean Journal of Mineralogy0935-12211617-40112020-12-013265367110.5194/ejm-32-653-2020Reaction progress of clay minerals and carbonaceous matter in a contact metamorphic aureole (Torres del Paine intrusion, Chile)A. Süssenberger0S. T. Schmidt1F. H. Schmidt2M. F. G. Weinkauf3Department of Earth Sciences, University of Geneva, Geneva, 1205, SwitzerlandDepartment of Earth Sciences, University of Geneva, Geneva, 1205, SwitzerlandDepartment of Otorhinolaryngology, University of Lübeck, Lübeck, 23538, GermanyInstitute of Geology and Palaeontology, Charles University in Prague, Prague, 128 43, Czech Republic<p>This study reports on reaction processes in a transition zone from contact to regional metamorphism by using Raman spectroscopy on carbonaceous matter (RSCM), illite “crystallinity” (Kübler index, KI), chlorite geothermometry, and thermal modeling. The thermal effect due to the emplacement of the Torres del Paine intrusion (TPI, assembly time of ca. 150&thinsp;kyr) had different consequences for inorganic and organic compounds of the host rock. The thermal alteration of the pre-intrusive regional metamorphosed host rock is documented by elevated RSCM temperatures, high-temperature chlorite generations, and the appearance of epidote and retrograde Fe-rich chlorite. Microprobe analysis on chlorite indicates incomplete re-equilibration as evidenced by various chlorite populations of individual contact metamorphic samples. This study indicates that the maturity of organic matter is the most reliable and unequivocal indicator on timescales of several thousand years to determine the lateral extension of the TPI contact aureole. Raman geothermometry reveals that the lateral extension of the contact-influenced zone expands up to a distance of 1.5&thinsp;km and, thus, expands to ca. 1.1&thinsp;km further out than the macroscopically mappable hornfels contact aureole. The best match between measured (Raman geothermometry) and calculated (thermal modeling) <span class="inline-formula">Δ<i>T</i><sub>max</sub></span> values (<span class="inline-formula">Δ<i>T</i>=54</span>&thinsp;<span class="inline-formula"><sup>∘</sup></span>C) is achieved with a total intrusion assembly time of 150&thinsp;kyr, a magmatic temperature of 800&thinsp;<span class="inline-formula"><sup>∘</sup></span>C, a two-batch model (batch repose time of 10&thinsp;kyr) with five pulses per batch, short heating durations (3&thinsp;kyr), and long pulse repose times (15&thinsp;kyr).</p>https://ejm.copernicus.org/articles/32/653/2020/ejm-32-653-2020.pdf
collection DOAJ
language English
format Article
sources DOAJ
author A. Süssenberger
S. T. Schmidt
F. H. Schmidt
M. F. G. Weinkauf
spellingShingle A. Süssenberger
S. T. Schmidt
F. H. Schmidt
M. F. G. Weinkauf
Reaction progress of clay minerals and carbonaceous matter in a contact metamorphic aureole (Torres del Paine intrusion, Chile)
European Journal of Mineralogy
author_facet A. Süssenberger
S. T. Schmidt
F. H. Schmidt
M. F. G. Weinkauf
author_sort A. Süssenberger
title Reaction progress of clay minerals and carbonaceous matter in a contact metamorphic aureole (Torres del Paine intrusion, Chile)
title_short Reaction progress of clay minerals and carbonaceous matter in a contact metamorphic aureole (Torres del Paine intrusion, Chile)
title_full Reaction progress of clay minerals and carbonaceous matter in a contact metamorphic aureole (Torres del Paine intrusion, Chile)
title_fullStr Reaction progress of clay minerals and carbonaceous matter in a contact metamorphic aureole (Torres del Paine intrusion, Chile)
title_full_unstemmed Reaction progress of clay minerals and carbonaceous matter in a contact metamorphic aureole (Torres del Paine intrusion, Chile)
title_sort reaction progress of clay minerals and carbonaceous matter in a contact metamorphic aureole (torres del paine intrusion, chile)
publisher Copernicus Publications
series European Journal of Mineralogy
issn 0935-1221
1617-4011
publishDate 2020-12-01
description <p>This study reports on reaction processes in a transition zone from contact to regional metamorphism by using Raman spectroscopy on carbonaceous matter (RSCM), illite “crystallinity” (Kübler index, KI), chlorite geothermometry, and thermal modeling. The thermal effect due to the emplacement of the Torres del Paine intrusion (TPI, assembly time of ca. 150&thinsp;kyr) had different consequences for inorganic and organic compounds of the host rock. The thermal alteration of the pre-intrusive regional metamorphosed host rock is documented by elevated RSCM temperatures, high-temperature chlorite generations, and the appearance of epidote and retrograde Fe-rich chlorite. Microprobe analysis on chlorite indicates incomplete re-equilibration as evidenced by various chlorite populations of individual contact metamorphic samples. This study indicates that the maturity of organic matter is the most reliable and unequivocal indicator on timescales of several thousand years to determine the lateral extension of the TPI contact aureole. Raman geothermometry reveals that the lateral extension of the contact-influenced zone expands up to a distance of 1.5&thinsp;km and, thus, expands to ca. 1.1&thinsp;km further out than the macroscopically mappable hornfels contact aureole. The best match between measured (Raman geothermometry) and calculated (thermal modeling) <span class="inline-formula">Δ<i>T</i><sub>max</sub></span> values (<span class="inline-formula">Δ<i>T</i>=54</span>&thinsp;<span class="inline-formula"><sup>∘</sup></span>C) is achieved with a total intrusion assembly time of 150&thinsp;kyr, a magmatic temperature of 800&thinsp;<span class="inline-formula"><sup>∘</sup></span>C, a two-batch model (batch repose time of 10&thinsp;kyr) with five pulses per batch, short heating durations (3&thinsp;kyr), and long pulse repose times (15&thinsp;kyr).</p>
url https://ejm.copernicus.org/articles/32/653/2020/ejm-32-653-2020.pdf
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