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Akademický článek

The felsic dikes of La Gomera (Canary Islands): identification of cone sheet and radial dike swarms

Autor: Ancochea, E, Brändle, J.L, Huertas, M.J, Cubas, C.R, Hernán, F

Publikováno v: In Journal of Volcanology and Geothermal Research 2003 120(3):197-206

Felsic Dykes Swarms on La Gomera Northern area (Canary Islands)

Autor: Huertas Coronel, María José, Brandle, J.L., Ancochea Soto, Eumenio, Hernán, F., Cubas, C.R.

Publikováno v: E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
E-Prints Complutense. Archivo Institucional de la UCM

The distributión offelsic dykes on La Gomera northern area corresponds to several swarms. The first radial dyke swarm is centered on the Tamargada area. The second radial dyke swarm center; located farther west, south of Vallehermoso is associated w

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::29a9d5591549bd2993e05932aa0a6d67
https://eprints.ucm.es/id/eprint/9926/1/2000_GOM_Diques_salicos_Geogaceta.pdf

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The geometry of the Vallehermoso Cone-sheet Complex La Gomera (Canary Islands)

Autor: Hernán, F., Cubas, C.R., Huertas Coronel, María José, Brandle, J.L., Ancochea Soto, Eumenio

Publikováno v: E-Prints Complutense. Archivo Institucional de la UCM
instname
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
Arias Montano. Repositorio Institucional de la Universidad de Huelva

A mainly phonolitic, 10 km in diameter, cone-sheet complex crops out on the northern area of La Gomera. The swarm intrudes into the Basal Complex, The Old BasaIts and other rocks of the Trachytic-phonolitic Complex to which they belong. The cone-shee

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::622588ebc817bbe5d2613a2f62eb8b67
https://eprints.ucm.es/id/eprint/9924/1/2000_GOM_Diques_conicos_Geogaceta.pdf

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Compositional features and fractionation processes in the Centrai Volcanic Complex (I and I I) of Fuerteventura (Canary Islands)

Autor: Ancochea Soto, Eumenio, Brandle, J.L., Huertas Coronel, María José, Hernán, F., Cubas, C.R.

Publikováno v: E-Prints Complutense. Archivo Institucional de la UCM
instname
Arias Montano. Repositorio Institucional de la Universidad de Huelva
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid

The Central Vólcanic Complex I (CVC-I) consists maihly of mildly alkaline basalts, many of them ankaramitic. The compositional differences observed are explained by fractíonation and extraction (rates between 20% and 30%) of clinopyroxene (60%), ol

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::1102dc14cfbcef6375b8df672b4a30e0
https://eprints.ucm.es/id/eprint/9922/1/1997_FTV_Composicion_CVC_I_y_II_Geogaceta.pdf

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Compositional features in the southern Volcanic Complex I of Fuerteventura (Canary Island)

Autor: Ancochea Soto, Eumenio, Brandle, J.L., Cubas, C.R., Hernán, F., Huertas Coronel, María José

Publikováno v: Arias Montano. Repositorio Institucional de la Universidad de Huelva
instname
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid
E-Prints Complutense. Archivo Institucional de la UCM

The Southern Volcanic Complex I consists mainly of basalts with scarce felsic members. On the basis of chemical and mineralogical compositional features two groups could be considered. 80th groups are alkaline, the first normal alkaline (in the Cofet

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::21a7f53fc16bac2b8b899a016ebddaa2
http://hdl.handle.net/10272/13366

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Serie Basáltica Antigua Inferior en el sector de Hermigua. Isla de la Gomera

Autor: Cubas, C.R., Hernán , F., Ancochea Soto, Eumenio, Huertas Coronel, María José

Publikováno v: E-Prints Complutense. Archivo Institucional de la UCM
instname
E-Prints Complutense: Archivo Institucional de la UCM
Universidad Complutense de Madrid

Lower Old Basaltic Series had only been described W of the Basal Complex in Alojera-Tazo area but it is also well exposed in other zones on Gomera as in Hermigua area E of the Basal Complex. Here, the basaltic lava flows alternate with poligenetic ag

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::46138c47764ce3a03189c1e95483874b
http://eprints.ucm.es/9910/

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Volcanic Édifices in the Old Basaltic Series of Fuerteveñtura: General features of the Central Edifice

Autor: Ancochea Soto, Eumenio, Cubas , C.R., Hernán , F., Brandle, J.L.

The Old Basaltic Series in Fuerteventura is formed by three main edifices: Northern, Central and Southern (or Jandía) Edifices. The Central Edifice, a shield volcano, extends from El Jable towards Valles Ortega area forming a semicircular shape arou

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::020129f9733d9efbb3e6854955538eb7
https://eprints.ucm.es/id/eprint/9892/1/1991_FTV_Edificio_Central_Geogaceta_.pdf

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Akademický článek

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