About: A unique volcanic field in Tharsis, Mars: Pyroclastic cones as evidence for explosive eruptions

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About: A unique volcanic field in Tharsis, Mars: Pyroclastic cones as evidence for explosive eruptions Goto Sponge NotDistinct Permalink

An Entity of Type : http://linked.opendata.cz/ontology/domain/vavai/Vysledek, within Data Space : linked.opendata.cz associated with source document(s)

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rdf:type	skos:Concept http://linked.opendata.cz/ontology/domain/vavai/Vysledek
Description	Based on theoretical grounds, explosive basaltic volcanism should be common on Mars, yet the available morphological evidence is sparse. We test this hypothesis by investigating a unique unnamed volcanic field north of the shield volcanoes Biblis Patera and Ulysses Patera on Mars, where we observe several small conical edifices and associated lava flows. Twenty-nine volcanic cones are identified and the morphometry of many of these edifices is determined using established morphometric parameters such as basal width, crater width, height, slope, and their respective ratios. Their morphology, morphometry, and a comparison to terrestrial analogues suggest that they are martian equivalents of terrestrial pyroclastic cones, the most common volcanoes on Earth. Based on theoretical grounds, explosive basaltic volcanism should be common on Mars, yet the available morphological evidence is sparse. We test this hypothesis by investigating a unique unnamed volcanic field north of the shield volcanoes Biblis Patera and Ulysses Patera on Mars, where we observe several small conical edifices and associated lava flows. Twenty-nine volcanic cones are identified and the morphometry of many of these edifices is determined using established morphometric parameters such as basal width, crater width, height, slope, and their respective ratios. Their morphology, morphometry, and a comparison to terrestrial analogues suggest that they are martian equivalents of terrestrial pyroclastic cones, the most common volcanoes on Earth. (en)
Title	A unique volcanic field in Tharsis, Mars: Pyroclastic cones as evidence for explosive eruptions A unique volcanic field in Tharsis, Mars: Pyroclastic cones as evidence for explosive eruptions (en)
skos:prefLabel	A unique volcanic field in Tharsis, Mars: Pyroclastic cones as evidence for explosive eruptions A unique volcanic field in Tharsis, Mars: Pyroclastic cones as evidence for explosive eruptions (en)
skos:notation	RIV/67985530:_____/12:00372853!RIV13-AV0-67985530
http://linked.open...avai/riv/aktivita	P Z
http://linked.open...avai/riv/aktivity	P(ME09011), Z(AV0Z30120515)
http://linked.open...iv/cisloPeriodika	1
http://linked.open...vai/riv/dodaniDat	2013
http://linked.open...aciTvurceVysledku	Brož, Petr
http://linked.open.../riv/druhVysledku	J - Článek v odborném periodiku
http://linked.open...iv/duvernostUdaju	S - Úplné a pravdivé údaje nepodléhající ochraně podle zvláštních právních předpisů
http://linked.open...titaPredkladatele	Geofyzikální ústav AV ČR, v. v. i.
http://linked.open...dnocenehoVysledku	120718
http://linked.open...ai/riv/idVysledku	RIV/67985530:_____/12:00372853
http://linked.open...riv/jazykVysledku	eng - angličtina
http://linked.open.../riv/klicovaSlova	Mars; volcanism; Mars surface (en)
http://linked.open.../riv/klicoveSlovo	Mars surface Mars volcanism
http://linked.open...odStatuVydavatele	US - Spojené státy americké
http://linked.open...ontrolniKodProRIV	[159DA166AA72]
http://linked.open...i/riv/nazevZdroje	Icarus
http://linked.open...in/vavai/riv/obor	DC
http://linked.open...ichTvurcuVysledku	1 (xsd:int)
http://linked.open...cetTvurcuVysledku	2 (xsd:int)
http://linked.open...vavai/riv/projekt	Subduction Factory: Earthquake Production and Magma Emplacement
http://linked.open...UplatneniVysledku	2012
http://linked.open...v/svazekPeriodika	218
http://linked.open...iv/tvurceVysledku	Brož, Petr Hauber, E.
http://linked.open...ain/vavai/riv/wos	000301637700008
http://linked.open...n/vavai/riv/zamer	Study of the internal structure and dynamics of the Earth
issn	0019-1035
number of pages	12 (xsd:int)
http://bibframe.org/vocab/doi	10.1016/j.icarus.2011.11.030

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