About: The volcano-tectonic evolution of the Miocene Santa Lucía Volcano, Boaco district, Nicaragua     Goto   Sponge   NotDistinct   Permalink

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  • On the basis of field mapping, petrological and geochemical data, a new model for the evolution of the Santa Lucía Volcano is presented. The first stage consisted of a series of strong Sub-Plinian eruptions, which produced thick ignimbrite units. These events destroyed the pre-existing volcanic edifice. The second stage was dominated by large explosive eruptions producing mainly non-welded dacitic–andesitic ignimbrites. The next resulted in the formation of andesitic lava flows and minor tephra fall-out deposits, covered by voluminous basaltic lavas. Lahars probably triggered by volcanic and/or seismic events represent the final stage of volcanic activity. From the Miocene onwards, volcanic rocks became deeply weathered and locally eroded. Strongly weathered rocks are susceptible to landslides, and surficial modification by post-volcanic slope movements is observed on the slopes of the Santa Lucía Volcano.
  • On the basis of field mapping, petrological and geochemical data, a new model for the evolution of the Santa Lucía Volcano is presented. The first stage consisted of a series of strong Sub-Plinian eruptions, which produced thick ignimbrite units. These events destroyed the pre-existing volcanic edifice. The second stage was dominated by large explosive eruptions producing mainly non-welded dacitic–andesitic ignimbrites. The next resulted in the formation of andesitic lava flows and minor tephra fall-out deposits, covered by voluminous basaltic lavas. Lahars probably triggered by volcanic and/or seismic events represent the final stage of volcanic activity. From the Miocene onwards, volcanic rocks became deeply weathered and locally eroded. Strongly weathered rocks are susceptible to landslides, and surficial modification by post-volcanic slope movements is observed on the slopes of the Santa Lucía Volcano. (en)
Title
  • The volcano-tectonic evolution of the Miocene Santa Lucía Volcano, Boaco district, Nicaragua
  • The volcano-tectonic evolution of the Miocene Santa Lucía Volcano, Boaco district, Nicaragua (en)
skos:prefLabel
  • The volcano-tectonic evolution of the Miocene Santa Lucía Volcano, Boaco district, Nicaragua
  • The volcano-tectonic evolution of the Miocene Santa Lucía Volcano, Boaco district, Nicaragua (en)
skos:notation
  • RIV/00025798:_____/11:00000364!RIV12-MZP-00025798
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • V
http://linked.open...iv/cisloPeriodika
  • 2011
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
  • 239457
http://linked.open...ai/riv/idVysledku
  • RIV/00025798:_____/11:00000364
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • caldera, volcanostratigraphy, ignimbrite, Santa Lucía Volcano, Nicaraguan Interior Highlands (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • CZ - Česká republika
http://linked.open...ontrolniKodProRIV
  • [53AE73A6CD72]
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...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 56
http://linked.open...iv/tvurceVysledku
  • Buriánek, David
  • Hradecký, Petr
http://linked.open...ain/vavai/riv/wos
  • 000290046200003
issn
  • 1802-6222
number of pages
http://bibframe.org/vocab/doi
  • 10.3190/jgeosci.085
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