SwePub
Sök i LIBRIS databas

  Utökad sökning

id:"swepub:oai:DiVA.org:uu-464383"
 

Sökning: id:"swepub:oai:DiVA.org:uu-464383" > Magma storage at Oc...

Magma storage at Ocean Islands : insights from Cape Verde

Barker, Abigail (författare)
Uppsala universitet,Mineralogi, petrologi och tektonik,Centre of Natural Hazards and Disaster Sciences, Uppsala, Sweden
Rydeblad, Elin M. (författare)
Uppsala universitet,Institutionen för geovetenskaper,Imperial College London
Silva, Sónia M. D. M. (författare)
University of Cape Verde
 (creator_code:org_t)
2021-05-21
2021
Engelska.
Ingår i: Crustal Magmatic System Evolution. - : American Geophysical Union (AGU). - 9781119564454 - 9781119564461 - 9781119564485 ; , s. 45-78
  • Bokkapitel (refereegranskat)
Abstract Ämnesord
Stäng  
  • The Cape Verde archipelago is a group of ocean islands in the Central Atlantic that forms two chains of islands trending northwest and southwest. Several of the islands are considered to be volcanically active, with frequent eruptions on Fogo. We examine the mineral chemistry and thermobarometry of the southern islands—Santiago, Fogo, and Brava—together with the Cadamosto Seamount. Our objective is to explore the magmatic storage system and implications for volcanic eruptions and associated hazards at Cape Verde. The volcanic rocks at Cape Verde are alkaline and dominantly mafic, whereas the island of Brava and the Cadamosto Seamount are unusually felsic. Clinopyroxene compositions range from 60 to 90 Mg# at Santiago and Fogo. In contrast, at Brava and the Cadamosto Seamount, the clinopyroxene compositions are 5 to 75 Mg#. Mineral chemistry and zonation records fractional crystallization, recharge, aggregation of crystals, magma mixing, and variations in thermal conditions of the magma at temperatures from 925 to 1250 °C. Magma storage depths at Santiago, Fogo, Brava, and the Cadamosto Seamount are between 12 and 40 km, forming deep sub-Moho magma storage zones. Transient magma storage in the crust is suggested by fluid inclusion re-equilibration and pre-eruption seismicity. A global compilation of magma storage at ocean islands suggests that deep magma storage is a common feature, and volcanic eruptions are often associated with rapid magma ascent through the crust. Shallow magma storage is more variable and likely reflects local variations in crustal structure, sediment supply, and tectonics. Petrological constraints on the magma plumbing system at Cape Verde and elsewhere are vital to integrate with deformation models and seismicity in order to improve understanding and mitigation of the volcanic hazards.

Ämnesord

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

Nyckelord

Magma storage
Cape Verde
Ocean islands
Magmatic processes
Volcanic hazards
Geovetenskap med inriktning mot mineralogi, petrologi och tektonik
Earth Science with specialization in Mineral Chemistry, Petrology and Tectonics

Publikations- och innehållstyp

ref (ämneskategori)
kap (ämneskategori)

Hitta via bibliotek

Till lärosätets databas

Hitta mer i SwePub

Av författaren/redakt...
Barker, Abigail
Rydeblad, Elin M ...
Silva, Sónia M. ...
Om ämnet
NATURVETENSKAP
NATURVETENSKAP
och Geovetenskap och ...
och Geologi
Artiklar i publikationen
Crustal Magmatic ...
Av lärosätet
Uppsala universitet

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