About: Geochemistry and genesis of behind-arc basaltic lavas from eastern Nicaragua     Goto   Sponge   NotDistinct   Permalink

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  • The petrology and chemistry of the Behind the Volcanic Front (BVF) lavas from eastern Nicaragua illustrate the complex nature of sources and processes. The older, Early Miocene (~17 Ma) low-Ti basalts–andesites are characterized by a strong LILE/HFSE depletion. They are interpreted as relics of Early Miocene volcanic arc, largely analogous to the extinct Coyol arc further W. The prevalent high-Ti lavas are represented both by alkaline (Quaternary trachybasalts: Volcán Azul and Kukra Hill) and subalkaline (basalts–basaltic andesites: Late Miocene, ~ 11 Ma Great Corn Island and Quaternary, Pearl Lagoon) volcanic rocks. All probably represent small-volume decompression melts of an OIB-like source with a strong Galápagos mantle imprint. The positive Sr–Nd isotopic correlation indicates an interaction between this component and a depleted mantle modified slightly by subduction-related influx of mainly Sr and Li. This feeble signal stems most likely from the Miocene convergence episode.
  • The petrology and chemistry of the Behind the Volcanic Front (BVF) lavas from eastern Nicaragua illustrate the complex nature of sources and processes. The older, Early Miocene (~17 Ma) low-Ti basalts–andesites are characterized by a strong LILE/HFSE depletion. They are interpreted as relics of Early Miocene volcanic arc, largely analogous to the extinct Coyol arc further W. The prevalent high-Ti lavas are represented both by alkaline (Quaternary trachybasalts: Volcán Azul and Kukra Hill) and subalkaline (basalts–basaltic andesites: Late Miocene, ~ 11 Ma Great Corn Island and Quaternary, Pearl Lagoon) volcanic rocks. All probably represent small-volume decompression melts of an OIB-like source with a strong Galápagos mantle imprint. The positive Sr–Nd isotopic correlation indicates an interaction between this component and a depleted mantle modified slightly by subduction-related influx of mainly Sr and Li. This feeble signal stems most likely from the Miocene convergence episode. (en)
Title
  • Geochemistry and genesis of behind-arc basaltic lavas from eastern Nicaragua
  • Geochemistry and genesis of behind-arc basaltic lavas from eastern Nicaragua (en)
skos:prefLabel
  • Geochemistry and genesis of behind-arc basaltic lavas from eastern Nicaragua
  • Geochemistry and genesis of behind-arc basaltic lavas from eastern Nicaragua (en)
skos:notation
  • RIV/00025798:_____/10:00000111!RIV11-GA0-00025798
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • I, P(GA205/06/1680), P(GA205/06/1811), S, Z(MSM 113100005), Z(MZP0002579801)
http://linked.open...iv/cisloPeriodika
  • 3-4
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
  • 260586
http://linked.open...ai/riv/idVysledku
  • RIV/00025798:_____/10:00000111
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • Back-arc volcanism, Central American Volcanic Arc, whole-rock geochemistry, Li-Sr-Nd-Pb isotopes, K-Ar dating (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • NL - Nizozemsko
http://linked.open...ontrolniKodProRIV
  • [E7989AC52A07]
http://linked.open...i/riv/nazevZdroje
  • Journal of Volcanology and Geothermal Research
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
  • 192
http://linked.open...iv/tvurceVysledku
  • Erban, Vojtěch
  • Holub, František
  • Janoušek, Vojtěch
  • Magna, Tomáš
  • Mlčoch, Bedřich
  • Rapprich, Vladislav
  • Wiechert, Uwe
  • Bellon, Hervé
http://linked.open...ain/vavai/riv/wos
  • 000277923700009
http://linked.open...n/vavai/riv/zamer
issn
  • 0377-0273
number of pages
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