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Silicic frothy xenoliths (xeno-pumice) in recent volcanics from Gran Canaria, Canary Islands

Jägerup, S. B. (author)
Uppsala universitet,Naturresurser och hållbar utveckling,King Abdullah Univ Sci & Technol KAUST, Fac Phys Sci & Engn, Thuwal, Saudi Arabia.
Troll, Valentin R. (author)
Uppsala universitet,Naturresurser och hållbar utveckling,Univ Las Palmas de Gran Canaria ULPGC, Dept Phys GEOVOL, Las Palmas Gran Canaria, Canary Islands, Spain.
Geiger, Harri (author)
Uppsala universitet,Naturresurser och hållbar utveckling,Univ Freiburg, Inst Earth & Environm Sci, D-79104 Freiburg im Breisgau, Germany.
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Deegan, Frances (author)
Uppsala universitet,Naturresurser och hållbar utveckling
Harris, C. (author)
Univ Cape Town, Dept Geol Sci, ZA-7701 Rondebosch, South Africa.
Carracedo, J. C. (author)
Univ Las Palmas de Gran Canaria ULPGC, Dept Phys GEOVOL, Las Palmas Gran Canaria, Canary Islands, Spain.
Meade, Fiona C. (author)
Uppsala universitet,Naturresurser och hållbar utveckling
Omidian, S. (author)
Uppsala universitet,Naturresurser och hållbar utveckling
Pedroza, Kirsten (author)
Uppsala universitet,Naturresurser och hållbar utveckling
van der Zwan, F. M. (author)
King Abdullah Univ Sci & Technol KAUST, Fac Phys Sci & Engn, Thuwal, Saudi Arabia.
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 (creator_code:org_t)
Elsevier BV, 2023
2023
English.
In: Journal of Volcanology and Geothermal Research. - : Elsevier BV. - 0377-0273 .- 1872-6097. ; 440
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • The Quaternary small-volume alkaline magmatic episode on Gran Canaria erupted dominantly basanite and nephelinite lavas and scoria deposits that contain a range of mantle and crustal xenoliths. These xenoliths comprise peridotite nodules, partially melted plutonic and volcanic rock fragments, and a group of light colored, felsic, and commonly frothy quartz-bearing rock fragments (xeno-pumice) that show evidence for intense interaction with their host magmas. Here we study a selection of these felsic and, in part, glassy and vesicular xenoliths from North and North-East Gran Canaria, with the aim to unravel their ultimate origin and learn more about magma storage and ascent within and below the island. Inspection of textures, mineral assemblages and glass compositions reveal one group of felsic xenoliths with fresh to partly altered igneous phenocryst assemblages and relict magmatic textures in addition to 818O values of 3.6 to 6.6%o. This group is interpreted to be of igneous origin. A second group of frothy felsic xenoliths displays mineralogy and textural characteristics more similar to sedimentary rocks with frequent occurrence of quartz, a mineral usually not present as phenocrysts in magmatic rocks from the Canary Islands. This second group displays relatively high 818O values (8.1 to 16.8%o), more typical for sedimentary lithologies, and is thus interpreted to represent material derived from the extensive pre-island sedimentary part of the ocean crust. The investigated xenoliths from North Gran Canaria thus provide a snapshot of pre-island sedimentary geology as well as the island's "magmatic" interior. These new data help constrain the available subsurface compositional variations within and below the Canary Islands and will hence be useful in interpreting magma evolution trends and magma storage levels.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geologi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geology (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geokemi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geochemistry (hsv//eng)

Keyword

Gran Canaria
Alkaline volcanism
Xenoliths
Xeno-pumice
Magma-sediment interaction

Publication and Content Type

ref (subject category)
art (subject category)

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