Journal article Open Access
M. Schiazza; Francesco Stoppa
<?xml version='1.0' encoding='UTF-8'?> <record xmlns="http://www.loc.gov/MARC21/slim"> <leader>00000nam##2200000uu#4500</leader> <datafield tag="540" ind1=" " ind2=" "> <subfield code="u">https://creativecommons.org/licenses/by-nc-nd/4.0/</subfield> <subfield code="a">Creative Commons Attribution-NonCommercial-NoDerivatives</subfield> </datafield> <datafield tag="542" ind1=" " ind2=" "> <subfield code="l">open</subfield> </datafield> <datafield tag="980" ind1=" " ind2=" "> <subfield code="a">publication</subfield> <subfield code="b">article</subfield> </datafield> <controlfield tag="001">118589</controlfield> <datafield tag="520" ind1=" " ind2=" "> <subfield code="a">Abstract 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 delhayelitemacdonaldite 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&lt;600 °C) is marked by the metastable reaction and formation of a rare and complex zeolite association (T&lt;300 °C). Circulation of low-temperature (T&lt;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.</subfield> </datafield> <datafield tag="245" ind1=" " ind2=" "> <subfield code="a">Extreme chemical conditions of crystallisation of Umbrian Melilitolites and wealth of rare, late stage/hydrothermal minerals</subfield> </datafield> <datafield tag="980" ind1=" " ind2=" "> <subfield code="a">user-itmirror</subfield> </datafield> <datafield tag="650" ind1="1" ind2="7"> <subfield code="a">cc-by</subfield> <subfield code="2">opendefinition.org</subfield> </datafield> <datafield tag="700" ind1=" " ind2=" "> <subfield code="a">Francesco Stoppa</subfield> </datafield> <datafield tag="653" ind1=" " ind2=" "> <subfield code="a">NEANIAS Atmospheric Research Community</subfield> </datafield> <datafield tag="653" ind1=" " ind2=" "> <subfield code="a">General Earth and Planetary Sciences</subfield> </datafield> <datafield tag="653" ind1=" " ind2=" "> <subfield code="a">Environmental Science (miscellaneous)</subfield> </datafield> <controlfield tag="005">20230927074727.0</controlfield> <datafield tag="024" ind1=" " ind2=" "> <subfield code="a">10.2478/s13533-012-0190-z</subfield> <subfield code="2">doi</subfield> </datafield> <datafield tag="100" ind1=" " ind2=" "> <subfield code="a">M. Schiazza</subfield> </datafield> <datafield tag="856" ind1="4" ind2=" "> <subfield code="s">10811456</subfield> <subfield code="u">https://www.openaccessrepository.it/record/118589/files/fulltext.pdf</subfield> <subfield code="z">md5:fda4da467c50a6a95f5e4dd3d4e17290</subfield> </datafield> <datafield tag="041" ind1=" " ind2=" "> <subfield code="a">eng</subfield> </datafield> <datafield tag="260" ind1=" " ind2=" "> <subfield code="c">2014-08-17</subfield> </datafield> </record>
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