SwePub
Sök i LIBRIS databas

  Utökad sökning

WFRF:(Menzies Andrew)
 

Sökning: WFRF:(Menzies Andrew) > (2015-2019) > The great escape :

The great escape : Petrogenesis of low-silica volcanism of Pliocene to Quaternary age associated with the Altiplano-Puna Volcanic Complex of northern Chile (21 degrees 10 '-22 degrees 50 ' S)

Gonzalez-Maurel, Osvaldo (författare)
Univ Catolica Norte, Dept Ciencias Geol, Ave Angamos 0610, Antofagasta, Chile;Univ Cape Town, Dept Geol Sci, ZA-7700 Rondebosch, South Africa
le Roux, Petrus (författare)
Univ Cape Town, Dept Geol Sci, ZA-7700 Rondebosch, South Africa
Godoy, Benigno (författare)
Univ Chile, CEGA, Plaza Ercilla 803, Santiago, Chile;Univ Chile, Fac Ciencias Fis & Matemat, Dept Geol, Plaza Ercilla 803, Santiago, Chile
visa fler...
Troll, Valentin R. (författare)
Uppsala universitet,Mineralogi, petrologi och tektonik,Uppsala Univ, Dept Earth Sci Nat Resources & Sustainable Dev, SE-75236 Uppsala, Sweden
Deegan, Frances (författare)
Uppsala universitet,Mineralogi, petrologi och tektonik
Menzies, Andrew (författare)
Bruker Nano GmbH, Studio 2D, D-12489 Berlin, Germany
visa färre...
 (creator_code:org_t)
ELSEVIER, 2019
2019
Engelska.
Ingår i: Lithos. - : ELSEVIER. - 0024-4937 .- 1872-6143. ; 346/347
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • The Pliocene to Quaternary volcanic arc of the Central Andes formed on 70-74 km thick continental crust. Physical interaction between mafic and acid magmas for this arc are therefore difficult to recognize due to the differentiation of mantle-derived magma during ascent through the thickened crust and a corresponding lack of erupted primitive lavas. However, a rare concentration of less evolved rocks is located marginal to the partially molten Altiplano-Puna Magma Body (APMB) in the Altiplano-Puna Volcanic Complex of northern Chile, between 21 degrees 10'S and 22 degrees 50'S. To unravel the relationship between this less evolved magmatism and the APMB, we present major and trace element data, and Sr and Nd isotope ratios of fourteen volcanoes. Whole-rock compositional and Sr and Nd isotope data reveal a large degree for compositional heterogeneity, e.g., SiO2 = 53.2 to 63.2 wt%, MgO = 1.74 to 6.08 wt%, Cr = 2 to 382 ppm, Sr = 304 to 885 ppm, (87)sr/(86)sr = 0.7055 to 0.7088, and Nd-143/Nd-144 = 0.5122 to 0.5125. The combined dataset points to magma spatial compositional changes resulting from magma mixing, fractional crystallization and crustal assimilation. The least evolved products erupted along the periphery of the APMB and are likely equivalent to the replenishing magmas that thermally sustain the large APMB system. We suggest that the mafic to intermediate eruptives we have investigated reflect mafic melt injections that underplate the APMB and escape along the side of the large felsic body to avoid significant compositional modifications during ascent, which helps to assess the evolution of the APMB through space and time. (C) 2019 Elsevier B.V. All rights reserved.

Ämnesord

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

Nyckelord

Low-silica volcanism
Altiplano-Puna Volcanic Complex
Altiplano-Puna Magma Body
Sr and Nd radiogenic isotopes

Publikations- och innehållstyp

ref (ämneskategori)
art (ämneskategori)

Hitta via bibliotek

  • Lithos (Sök värdpublikationen i LIBRIS)

Till lärosätets databas

Sök utanför SwePub

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Stäng

Kopiera och spara länken för att återkomma till aktuell vy