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Index Geophysics

Palaeomagnetism and the early magmatic history of Fuerteventura (Canary Islands)

Item

Title (Dublin Core)

en-US Palaeomagnetism and the early magmatic history of Fuerteventura (Canary Islands)

Description (Dublin Core)

en-US Thermal and alternating field demagnetization combined with studies of the convergence points of remagnetization circles have been carried out on a variety of rocks from Fuerteventura. The older (post-Albian) rocks, including the basement plutonics, the sheeted dike complex and the earliest subaerial lava sequence (lava Series I), have a multicomponent remanence while the younger lava Series II of Miocene/Pliocene age has dominantly a one-component magnetization. Comparison of the results with recent palaeomagnetic data from Gran Canaria/Tenerife and with results from continental Africa and Europe suggest a late Cretaceous origin of the basal intrusive rocks while the subaerial volcanism (lava Series I) most likely initiated at around the Cretaceous/Tertiary boundary. This implies that there is a nearly 50-m.y.-long period of volcanic quiescence and erosion between lava Series I and lava Series II. The apparent contradiction between these conclusions and the few K/Ar dates available is discussed.
          ARK: https://n2t.net/ark:/88439/y082688
Permalink: https://geophysicsjournal.com/article/281
 

Creator (Dublin Core)

Storetvedt, K.M.
Mongstad Vage, H.
Aase, S.
Lovlie, R.

Subject (Dublin Core)

en-US Palaeomagnetism
en-US Age of early Fuerteventura magmatism
en-US Geodynamics

Publisher (Dublin Core)

en-US Journal of Geophysics

Date (Dublin Core)

1979-04-26

Type (Dublin Core)

info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
en-US Peer-reviewed Article

Format (Dublin Core)

application/pdf

Identifier (Dublin Core)

https://journal.geophysicsjournal.com/JofG/article/view/281

Source (Dublin Core)

en-US Journal of Geophysics; Vol 46 No 1 (1979): Journal of Geophysics; 319-334
2643-2986
2643-9271

Language (Dublin Core)

eng

Relation (Dublin Core)

https://journal.geophysicsjournal.com/JofG/article/view/281/238