Extreme chemical conditions of crystallisation of Umbrian Melilitolites and wealth of rare, late stage/hydrothermal minerals
Melilitolites of the Umbria Latium Ultra-alkaline District display a complete crystallisation sequence of peculiar, late-stage mineral phases and hydrothermal/cement minerals, analogous to fractionated mineral associations from the Kola Peninsula. This paper summarises 20 years of research which has...
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Online Access: | http://hdl.handle.net/11564/600912 https://doi.org/10.2478/s13533-012-0190-z |
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ftunivchietiiris:oai:ricerca.unich.it:11564/600912 2024-04-21T08:06:35+00:00 Extreme chemical conditions of crystallisation of Umbrian Melilitolites and wealth of rare, late stage/hydrothermal minerals STOPPA, Francesco SCHIAZZA, MARIANGELA Stoppa, Francesco Schiazza, Mariangela 2014 ELETTRONICO http://hdl.handle.net/11564/600912 https://doi.org/10.2478/s13533-012-0190-z eng eng info:eu-repo/semantics/altIdentifier/wos/WOS:000340660600009 volume:6 issue:4 firstpage:549 lastpage:564 numberofpages:16 journal:CENTRAL EUROPEAN JOURNAL OF GEOSCIENCES http://hdl.handle.net/11564/600912 doi:10.2478/s13533-012-0190-z info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-84919951756 Melilitolite ultra peralkaline liquid Zr Ti mineral zeolite hydroxylated silicate sulphate carbonate Umbria Latium Ultra alkaline District info:eu-repo/semantics/article 2014 ftunivchietiiris https://doi.org/10.2478/s13533-012-0190-z 2024-03-25T01:35:47Z Melilitolites of the Umbria Latium Ultra-alkaline District display a complete crystallisation sequence of peculiar, late-stage mineral phases and hydrothermal/cement minerals, analogous to fractionated mineral associations from the Kola Peninsula. This paper summarises 20 years of research which has resulted in the identification of a large number of mineral species, some very rare or completely new and some not yet classified. The progressive increasing alkalinity of the residual liquid allowed the formation of Zr-Ti phases and further delhayelite-macdonaldite mineral crystallisation in the groundmass. The presence of leucite and kalsilite in the igneous assemblage is unusual and gives a kamafugitic nature to the rocks. Passage to non-igneous temperatures (T<600 °C) is marked by the metastable reaction and formation of a rare and complex zeolite association (T<300 °C). Circulation of low-temperature (T<100 °C) K-Ca-Ba-CO2-SO2-fluids led to the precipitation of sulphates and hydrated and/or hydroxylated silicate-sulphate-carbonates. As a whole, this mineral assemblage can be considered typical of ultra-alkaline carbonatitic rocks. Article in Journal/Newspaper kola peninsula ARUd'A - Archivio Istituzionale della ricerca dell'università Chieti-Pescara (IRIS) Open Geosciences 6 4 |
institution |
Open Polar |
collection |
ARUd'A - Archivio Istituzionale della ricerca dell'università Chieti-Pescara (IRIS) |
op_collection_id |
ftunivchietiiris |
language |
English |
topic |
Melilitolite ultra peralkaline liquid Zr Ti mineral zeolite hydroxylated silicate sulphate carbonate Umbria Latium Ultra alkaline District |
spellingShingle |
Melilitolite ultra peralkaline liquid Zr Ti mineral zeolite hydroxylated silicate sulphate carbonate Umbria Latium Ultra alkaline District STOPPA, Francesco SCHIAZZA, MARIANGELA Extreme chemical conditions of crystallisation of Umbrian Melilitolites and wealth of rare, late stage/hydrothermal minerals |
topic_facet |
Melilitolite ultra peralkaline liquid Zr Ti mineral zeolite hydroxylated silicate sulphate carbonate Umbria Latium Ultra alkaline District |
description |
Melilitolites of the Umbria Latium Ultra-alkaline District display a complete crystallisation sequence of peculiar, late-stage mineral phases and hydrothermal/cement minerals, analogous to fractionated mineral associations from the Kola Peninsula. This paper summarises 20 years of research which has resulted in the identification of a large number of mineral species, some very rare or completely new and some not yet classified. The progressive increasing alkalinity of the residual liquid allowed the formation of Zr-Ti phases and further delhayelite-macdonaldite mineral crystallisation in the groundmass. The presence of leucite and kalsilite in the igneous assemblage is unusual and gives a kamafugitic nature to the rocks. Passage to non-igneous temperatures (T<600 °C) is marked by the metastable reaction and formation of a rare and complex zeolite association (T<300 °C). Circulation of low-temperature (T<100 °C) K-Ca-Ba-CO2-SO2-fluids led to the precipitation of sulphates and hydrated and/or hydroxylated silicate-sulphate-carbonates. As a whole, this mineral assemblage can be considered typical of ultra-alkaline carbonatitic rocks. |
author2 |
Stoppa, Francesco Schiazza, Mariangela |
format |
Article in Journal/Newspaper |
author |
STOPPA, Francesco SCHIAZZA, MARIANGELA |
author_facet |
STOPPA, Francesco SCHIAZZA, MARIANGELA |
author_sort |
STOPPA, Francesco |
title |
Extreme chemical conditions of crystallisation of Umbrian Melilitolites and wealth of rare, late stage/hydrothermal minerals |
title_short |
Extreme chemical conditions of crystallisation of Umbrian Melilitolites and wealth of rare, late stage/hydrothermal minerals |
title_full |
Extreme chemical conditions of crystallisation of Umbrian Melilitolites and wealth of rare, late stage/hydrothermal minerals |
title_fullStr |
Extreme chemical conditions of crystallisation of Umbrian Melilitolites and wealth of rare, late stage/hydrothermal minerals |
title_full_unstemmed |
Extreme chemical conditions of crystallisation of Umbrian Melilitolites and wealth of rare, late stage/hydrothermal minerals |
title_sort |
extreme chemical conditions of crystallisation of umbrian melilitolites and wealth of rare, late stage/hydrothermal minerals |
publishDate |
2014 |
url |
http://hdl.handle.net/11564/600912 https://doi.org/10.2478/s13533-012-0190-z |
genre |
kola peninsula |
genre_facet |
kola peninsula |
op_relation |
info:eu-repo/semantics/altIdentifier/wos/WOS:000340660600009 volume:6 issue:4 firstpage:549 lastpage:564 numberofpages:16 journal:CENTRAL EUROPEAN JOURNAL OF GEOSCIENCES http://hdl.handle.net/11564/600912 doi:10.2478/s13533-012-0190-z info:eu-repo/semantics/altIdentifier/scopus/2-s2.0-84919951756 |
op_doi |
https://doi.org/10.2478/s13533-012-0190-z |
container_title |
Open Geosciences |
container_volume |
6 |
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4 |
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1796945982027464704 |