Digital repository of Slovenian research organisations

Show document
A+ | A- | Help | SLO | ENG

Title:Effect of undercooling on clinopyroxene crystallization in a high K basalt : implications for magma dynamics at Stromboli volcano
Authors:ID Colle, F. (Author)
ID Masotta, Matteo (Author)
ID Costa, S. (Author)
ID Mollo, Silvio (Author)
ID Landi, P. (Author)
ID Pontesilli, A. (Author)
ID Peres, S. (Author)
ID Mancini, Lucia (Author)
Files:URL URL - Source URL, visit https://doi.org/10.1016/j.lithos.2023.107327
 
.pdf PDF - Presentation file, download (6,46 MB)
MD5: 989ABB4EEE1FEED94CB4D501E89B352C
 
.docx DOCX - Supplement, download (3,09 MB)
MD5: 0269FF9CB7A47E7AD3DEAF89CD120A73
 
This document has even more files. Complete list of files is available below.
Language:English
Typology:1.01 - Original Scientific Article
Organization:Logo ZAG - Slovenian National Building and Civil Engineering Institute
Abstract: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.
Keywords:clinopyroxene, undercooling, hourglass, crystallization, microtomography
Publication status:Published
Publication version:Version of Record
Publication date:16.08.2023
Publisher:Elsevier
Year of publishing:2023
Number of pages:str. 1-11, [article no.] 107327
Numbering:Vol. 456-457
PID:20.500.12556/DiRROS-17193 New window
UDC:55
ISSN on article:0024-4937
DOI:10.1016/j.lithos.2023.107327 New window
COBISS.SI-ID:170230787 New window
Copyright:© 2023 The Authors. Published by Elsevier B.V.
Note:Opis vira z dne 27. 10. 2023;
Publication date in DiRROS:27.10.2023
Views:864
Downloads:522
Metadata:XML DC-XML DC-RDF
:
Copy citation
  
Share:Bookmark and Share


Hover the mouse pointer over a document title to show the abstract or click on the title to get all document metadata.

Record is a part of a journal

Title:Lithos
Shortened title:Lithos
Publisher:Elsevier
ISSN:0024-4937
COBISS.SI-ID:1235989 New window

Document is financed by a project

Funder:Other - Other funder or multiple funders
Project number:PRIN 2017J277S9
Name:Time scales of solidification in magmas: Applications to Volcanic Eruptions, Silicate Melts, Glasses, Glass-Ceramics

Licences

License:CC BY-NC-ND 4.0, Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International
Link:http://creativecommons.org/licenses/by-nc-nd/4.0/
Description:The most restrictive Creative Commons license. This only allows people to download and share the work for no commercial gain and for no other purposes.
Licensing start date:16.08.2023
Applies to:Text and Data Mining valid from 2023-11-01 Version of Record valid from 2023-08-16

Secondary language

Language:Slovenian
Keywords:klinopiroksen, podhladitev, peščena ura, kristalizacija, mikrotomografija


Files

Loading...

Back