Departament de Mineralogia, Museu de Ciències Naturals de Barcelona, Passeig Picasso s/n, 08003, Barcelona, Spain.
Instituto de Oceanografía y Cambio Global, IOCAG, Dept. de Física, Universidad de Las Palmas de Gran Canaria, 35017, Las Palmas de Gran Canaria, Spain.
Sci Rep. 2023 Apr 18;13(1):6336. doi: 10.1038/s41598-023-33387-6.
The present work aims to characterize the ephemeral mineral assemblage related to the fumarolic fields of the Tajogaite volcano, formed in 2021 in La Palma Island (Canary Islands, Spain). A set of 73 samples was obtained after two sampling campaigns in different fumarole sectors of the studied area. Mineralization related to these fumaroles formed efflorescent patches located at variable distance from the main volcanic craters. Distal patches are predominantly whitish, while in the vicinities they typically show yellowish to orange colours. Field observations also revealed that fumaroles usually occur in elevated topographic areas as well as over fractured and porous volcanic pyroclastic materials. The mineralogical and textural characterisation of the Tajogaite fumaroles unfolds a complex mineral assemblage, comprising cryptocrystalline phases related to low (< 200 °C) and medium temperature (200-400 °C) conditions. In Tajogaite, we propose a classification of three different fumarolic mineralization types: (1) fluorides and chlorides located in proximal fumarolic areas (~ 300-180 °C); (2) native sulphur associated with gypsum, mascagnite and salammoniac (~ 120-100 °C) and (3) sulphates and alkaline carbonates typically occurred in distal fumarolic areas (< 100 °C). Finally, we present a schematic model of the formation of Tajogaite fumarolic mineralization and their compositional evolution developed during the cooling of the volcanic system.
本工作旨在对 Tajogaite 火山喷气孔相关的瞬态矿物组合进行特征描述,该火山于 2021 年在拉帕尔马岛(西班牙加那利群岛)形成。在对研究区不同喷气孔扇区进行两次采样后,获得了一组 73 个样本。与这些喷气孔相关的矿化作用形成了位于主火山口不同距离处的花状斑块。远景区的斑块主要呈白色,而近景区则通常呈黄至橙色。野外观察还表明,喷气孔通常出现在地形较高的地区以及断裂和多孔的火山碎屑物质上。Tajogaite 喷气孔的矿物学和结构特征揭示了一个复杂的矿物组合,包括与低温(<200°C)和中温(200-400°C)条件有关的隐晶质相。在 Tajogaite 中,我们提出了三种不同喷气孔矿化类型的分类:(1)位于近景区的氟化物和氯化物(300-180°C);(2)与石膏、mascagnite 和 salammoniac 伴生的自然硫(120-100°C)和(3)通常出现在远景区的硫酸盐和碱性碳酸盐(<100°C)。最后,我们提出了 Tajogaite 喷气孔矿化作用形成的示意图模型及其在火山系统冷却过程中发生的成分演化。