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  • Volcanism in the area was controlled by intersection of three tectonic structures: Central Graben, Comayagua Graben and Guayape Fault Zone. The basement is built of rhyolitic Playitas ignimbrite. The pyroclastic rocks of La Unión unit (13.3 Ma) display signs of mingling between basalt and dacite. Rocks of the subsequent Pozo unit are strongly altered. Pilón Lavas are dominated by andesite and basaltic andesite. Pleistocene volcanic activity is represented by the Pre-Conchagua edifice (1.6 Ma), Cerro Montoso and Juana-Pancha. Some lavas of the Pre-Conchagua – Juana-Pancha are compositionally distinct from common volcanic front products, resembling the lavas of Tegucigalpa volcanic field. Behind-arc extension could have facilitated the magma genesis via decompression melting of the mantle. The current Conchagua Volcano is built by repeated Strombolian eruptions associated with basaltic lavas.
  • Volcanism in the area was controlled by intersection of three tectonic structures: Central Graben, Comayagua Graben and Guayape Fault Zone. The basement is built of rhyolitic Playitas ignimbrite. The pyroclastic rocks of La Unión unit (13.3 Ma) display signs of mingling between basalt and dacite. Rocks of the subsequent Pozo unit are strongly altered. Pilón Lavas are dominated by andesite and basaltic andesite. Pleistocene volcanic activity is represented by the Pre-Conchagua edifice (1.6 Ma), Cerro Montoso and Juana-Pancha. Some lavas of the Pre-Conchagua – Juana-Pancha are compositionally distinct from common volcanic front products, resembling the lavas of Tegucigalpa volcanic field. Behind-arc extension could have facilitated the magma genesis via decompression melting of the mantle. The current Conchagua Volcano is built by repeated Strombolian eruptions associated with basaltic lavas. (en)
Title
  • Volcanic history of the Conchagua Peninsula (eastern El Salvador)
  • Volcanic history of the Conchagua Peninsula (eastern El Salvador) (en)
skos:prefLabel
  • Volcanic history of the Conchagua Peninsula (eastern El Salvador)
  • Volcanic history of the Conchagua Peninsula (eastern El Salvador) (en)
skos:notation
  • RIV/00025798:_____/10:00000089!RIV11-GA0-00025798
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • I, P(GA205/06/1680), Z(MZP0002579801)
http://linked.open...iv/cisloPeriodika
  • 2
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
http://linked.open.../riv/druhVysledku
http://linked.open...iv/duvernostUdaju
http://linked.open...titaPredkladatele
http://linked.open...dnocenehoVysledku
  • 296644
http://linked.open...ai/riv/idVysledku
  • RIV/00025798:_____/10:00000089
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • La Unión, Conchagua Volcano, volcanism, volcanostratigraphy, Central American volcanic chain, Comayagua Graben (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [683201C5AA3D]
http://linked.open...i/riv/nazevZdroje
  • Journal of Geosciences
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
http://linked.open...cetTvurcuVysledku
http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 55
http://linked.open...iv/tvurceVysledku
  • Erban, Vojtěch
  • Kopačková, Veronika
  • Rapprich, Vladislav
  • Fárová, Kateřina
  • Bellon, Hervé
  • Hernández, Walter
http://linked.open...ain/vavai/riv/wos
  • 000286341800002
http://linked.open...n/vavai/riv/zamer
issn
  • 1802-6222
number of pages
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