Crystal chemistry of epidote-(Sr) in alkaline rocks of the teschenite association (Silesian Unit, Czech Republic)

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Marco E. Ciriotti
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Crystal chemistry of epidote-(Sr) in alkaline rocks of the teschenite association (Silesian Unit, Czech Republic)

Messaggio da Marco E. Ciriotti » sab 04 feb, 2023 9:44

Prossima pubblicazione.

Referenza:
▪ Kropáč, K., Dolníček, Z., Uher, P., Buriánek, D., Urubek, T. (2023): Crystal chemistry and origin of epidote-(Sr) in alkaline rocks of the teschenite association (Silesian Unit, Outer Western Carpathians, Czech Republic). Mineralogy and Petrology, 117, (in press).

Abstract:
A new occurrence of epidote-(Sr) [CaSrAl2Fe3+(Si2O7)(SiO4)(OH)], Sr-REE-rich epidote and Sr-rich allanite-(Ce) is located in Lower Cretaceous, Sr-rich hydrothermally altered leucocratic dykes penetrating alkaline igneous rocks (teschenites) near the Nový Jičín town (the Silesian Unit, Outer Western Carpathians). The dykes contain phenocrysts of pyroxene, amphibole, biotite, fluorapatite and dominant felsic groundmass consisting mostly of alkali feldspars and zeolites (analcime, natrolite and thomsonite-Ca). Accessory minerals include Ti-rich magnetite, prehnite, chamosite, pyrite, calcite, (OH, F)-rich grossular, epidote-group minerals, HFSE-, REE-rich minerals, Sr-rich baryte and slawsonite. The Sr-rich epidote forms columnar crystals or irregular aggregates which are mostly spatially related to chamosite pseudomorphs; it contains 0.15–0.81 apfu Sr, <0.53 apfu REE; Fe3+/(Fe3+ + Al) = 0.16–0.48. The Sr2+ substitutes Ca2+ in the A2 site by a coupled substitution involving other A2 (REE3+, Y3+, Th4+) or M (Al3+, Fe3+, Fe2+) cations. The Sr-rich epidote crystallized from hydrothermal solutions, probably at temperatures between ~250–300 °C, during cooling of the host rock. The dykes show higher Sr contents (5680–7830 ppm) and 87Sr/86Sri(120 Ma) ratios (~0.7046–0.7047) compared to host mesocratic teschenites (1310–1470 ppm Sr and ~0.7038–0.7045, respectively). The Sr isotopes indicate origin of most Sr from primary magmatic plagioclase in parent teschenite. Nevertheless, there participated fluids of external origin, derived from the Lower Cretaceous seawater or diagenetic waters related to associated siliciclastic sediments with 87Sr/86Sri(120 Ma) = ~0.7073–0.7083. These more radiogenic sources contributed at least 6–21 % of the bulk Sr budget of the studied Sr-rich epidote-bearing leucocratic dykes.
Marco E. Ciriotti

«Things are interesting only in so far as they relate themselves to other things»

giuseppe daniele
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Re: Crystal chemistry of epidote-(Sr) in alkaline rocks of the teschenite association (Silesian Unit, Czech Republic)

Messaggio da giuseppe daniele » mer 08 feb, 2023 1:24

Scusami Marco, ho trovato l'articolo completo su Internet ma mi pare che non si riportino i parametri di cella rifiniti dell'epidoto-(Sr)! Forse non li ho visti, ma sono riportati o no? Grazie. Giuseppe Daniele.

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Marco E. Ciriotti
Messaggi: 31675
Iscritto il: ven 25 giu, 2004 11:31
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Re: Crystal chemistry of epidote-(Sr) in alkaline rocks of the teschenite association (Silesian Unit, Czech Republic)

Messaggio da Marco E. Ciriotti » mer 08 feb, 2023 9:29

Corretto Giuseppe.
I dati di cella non sono presenti nel lavoro.
Marco E. Ciriotti

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