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...
Main Authors: | , , , |
---|---|
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 |
id |
doaj-093990e710db433180701e445706ee43 |
---|---|
record_format |
Article |
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 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 km and, thus, expands to ca. 1.1 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> <span class="inline-formula"><sup>∘</sup></span>C) is achieved with a total intrusion assembly time of 150 kyr, a magmatic temperature of 800 <span class="inline-formula"><sup>∘</sup></span>C, a two-batch model (batch repose time of 10 kyr) with five pulses per batch, short heating durations (3 kyr), and long pulse repose times (15 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 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 km
and, thus, expands to ca. 1.1 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> <span class="inline-formula"><sup>∘</sup></span>C) is achieved with a total intrusion
assembly time of 150 kyr, a magmatic temperature of 800 <span class="inline-formula"><sup>∘</sup></span>C, a
two-batch model (batch repose time of 10 kyr) with five pulses per batch,
short heating durations (3 kyr), and long pulse repose times (15 kyr).</p> |
url |
https://ejm.copernicus.org/articles/32/653/2020/ejm-32-653-2020.pdf |
work_keys_str_mv |
AT asussenberger reactionprogressofclaymineralsandcarbonaceousmatterinacontactmetamorphicaureoletorresdelpaineintrusionchile AT stschmidt reactionprogressofclaymineralsandcarbonaceousmatterinacontactmetamorphicaureoletorresdelpaineintrusionchile AT fhschmidt reactionprogressofclaymineralsandcarbonaceousmatterinacontactmetamorphicaureoletorresdelpaineintrusionchile AT mfgweinkauf reactionprogressofclaymineralsandcarbonaceousmatterinacontactmetamorphicaureoletorresdelpaineintrusionchile |
_version_ |
1721227350514860032 |