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Naslov:Effect of undercooling on clinopyroxene crystallization in a high K basalt : implications for magma dynamics at Stromboli volcano
Avtorji:ID Colle, F. (Avtor)
ID Masotta, Matteo (Avtor)
ID Costa, S. (Avtor)
ID Mollo, Silvio (Avtor)
ID Landi, P. (Avtor)
ID Pontesilli, A. (Avtor)
ID Peres, S. (Avtor)
ID Mancini, Lucia (Avtor)
Datoteke:URL URL - Izvorni URL, za dostop obiščite https://doi.org/10.1016/j.lithos.2023.107327
 
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Jezik:Angleški jezik
Tipologija:1.01 - Izvirni znanstveni članek
Organizacija:Logo ZAG - Zavod za gradbeništvo Slovenije
Povzetek:We present undercooling (∆T) experiments aimed at investigating the effect of growth kinetics on the textural and compositional evolution of clinopyroxene crystals growing from a high-K basalt erupted during the 2003 paroxysm of Stromboli volcano (Italy). The experiments were performed at P = 350 MPa, T = 1050–1210 °C, H2Omelt = 0–3 wt%, and fO2 = Ni-NiO + 1.5 buffer. An initial stage of supersaturation was imposed to the melt under nominally anhydrous (∆Tanh = 10–150 °C) and hydrous (∆Thyd = 25–125 °C) conditions. Afterwards, this supersaturation state was mitigated by melt relaxation phenomena over an annealing time of 24 h. Results show that plagioclase is the liquidus mineral phase of the high-K basalt at ∆Tanh = 10 °C and dominates the phase assemblage as the degree of undercooling increases. Conversely, clinopyroxene and spinel co-saturate the melt at ∆Thyd = 25 °C, followed by the subordinate formation of plagioclase. At ∆Tanh/hyd ≤ 50 °C, the textural maturation of clinopyroxene produces polyhedral crystals with {−111} (hourglass) and {hk0} (prism) sectors typical of a layer-by-layer growth mechanism governed by an interface-controlled crystallization regime. At ∆Tanh/hyd ≥ 75 °C, the attainment of dendritic and skeletal morphologies testifies to the establishment of diffusion-limited reactions at the crystal-melt interface. 3D reconstructions of synchrotron radiation X-ray microtomographic data reveal a composite growth history for clinopyroxene crystals obtained at ∆Tanh/hyd ≥ 95 °C. The early stage of melt supersaturation produces rosette-like structures composed of dendritic branches of clinopyroxene radiating from a common spinel grain, which acts as surface for heterogeneous nucleation. As diffusive relaxation phenomena progress over the annealing time, the elongate dendrites that constitute the inner crystal domain are partially infilled by the melt and develop skeletal overgrowths in the outer domain. With the increasing degree of undercooling, TAl and M1Ti cations are progressively incorporated in the lattice site of clinopyroxene at the expense of TSi and M1Mg cations. Because of the effect of H2Omelt on the liquidus depression and melt depolymerization, crystals obtained at ∆Thyd are also more enriched in TAl and M1Ti and depleted in TSi and M1Mg than those growing at ∆Tanh. The emerging picture is that the morphological and geochemical evolution of clinopyroxene is mutually controlled by the combined effects of melt supersaturation and relaxation phenomena. A new empirical relationship based on the cation exchange reactions in the lattice site of clinopyroxene is finally proposed to estimate the degree of undercooling governing the crystallization of augitic phenocrysts erupted during normal and violent explosions at Stromboli.
Ključne besede:clinopyroxene, undercooling, hourglass, crystallization, microtomography
Status publikacije:Objavljeno
Verzija publikacije:Objavljena publikacija
Datum objave:16.08.2023
Založnik:Elsevier
Leto izida:2023
Št. strani:str. 1-11, [article no.] 107327
Številčenje:Vol. 456-457
PID:20.500.12556/DiRROS-17193 Novo okno
UDK:55
ISSN pri članku:0024-4937
DOI:10.1016/j.lithos.2023.107327 Novo okno
COBISS.SI-ID:170230787 Novo okno
Avtorske pravice:© 2023 The Authors. Published by Elsevier B.V.
Opomba:Opis vira z dne 27. 10. 2023;
Datum objave v DiRROS:27.10.2023
Število ogledov:856
Število prenosov:519
Metapodatki:XML DC-XML DC-RDF
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Gradivo je del revije

Naslov:Lithos
Skrajšan naslov:Lithos
Založnik:Elsevier
ISSN:0024-4937
COBISS.SI-ID:1235989 Novo okno

Gradivo je financirano iz projekta

Financer:Drugi - Drug financer ali več financerjev
Številka projekta:PRIN 2017J277S9
Naslov:Time scales of solidification in magmas: Applications to Volcanic Eruptions, Silicate Melts, Glasses, Glass-Ceramics

Licence

Licenca:CC BY-NC-ND 4.0, Creative Commons Priznanje avtorstva-Nekomercialno-Brez predelav 4.0 Mednarodna
Povezava:http://creativecommons.org/licenses/by-nc-nd/4.0/deed.sl
Opis:Najbolj omejujoča licenca Creative Commons. Uporabniki lahko prenesejo in delijo delo v nekomercialne namene in ga ne smejo uporabiti za nobene druge namene.
Začetek licenciranja:16.08.2023
Vezano na:Text and Data Mining valid from 2023-11-01 Version of Record valid from 2023-08-16

Sekundarni jezik

Jezik:Slovenski jezik
Ključne besede:klinopiroksen, podhladitev, peščena ura, kristalizacija, mikrotomografija


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