FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2068328265> ?p ?o ?g. }

• W2068328265 endingPage "233" @default.
• W2068328265 startingPage "207" @default.
• W2068328265 abstract "Abstract Hudson Volcano (45°54′S, 72°58′W) represents the southernmost central volcano of the South Andean Volcanic Zone (SVZ). It lies about 280 km east of Nazca–Antarctic–South American Plate Triple Junction, where the Chile spreading ridge enters the Chile Trench. Hudson is located on the border of a volcanic gap separating the Southern from the Austral Volcanic Zone (AVZ), which is commonly interpreted as linked to a slab window. The volcano is characterised by a volcano-tectonic depression about 10 km wide, set in a morphological high of the Patagonian Batholith. The scarce pre-caldera products are made up of mafic lavas interbedded with hyaloclastite. The majority of the volcanic products out from the caldera rims consist of thick deposits of lahars or hyaloclastitic breccias, subordinate lava flows and pyroclastic deposits linked to historical large explosive eruptions. Rough volume calculations on pre-caldera and post-caldera products suggest that the caldera formed in steps in the lifetime of the volcano and that it is mainly linked to a volcano-tectonic collapse during partial emptying of the magma chamber. The monogenetic cones surrounding Hudson (Rio Ibanez and Murta) erupted primitive basalts that gave important clues on magma sources. The volcanic products of Hudson, with composition ranging from basalts to dacites, have a calc-alkaline signature. Nevertheless, they have distinctly higher K2O, TiO2, Na2O, LILE, HFSE and REE than the calc-alkaline rocks of SVZ. The basaltic lavas from the monogenetic cones show La/Nb, Ba/Nb and Th/Ta significantly lower than the calc-alkaline lavas. Furthermore, they have some ratios as Th/Yb and La/Yb remarkably low, with values approaching those of MORB-like basalts. All the geochemical characteristics of Rio Ibanez and Murta cones are very similar to those of the basalts dredged in the Chile Ridge. Geochemical modeling suggests that the Hudson basalts may derive from the basalts erupted at the Rio Ibanez centre through an assimilation plus fractional crystallisation process. On the basis of these data, we propose a geodynamical model. In correspondence to the monogenetic centres, close to the border of the incipient opening of the slab window, the magma features are still those of the depleted asthenosphere under the subducting ridge. In this zone, remnant fragments of subducted oceanic crust undergo partial melting processes, while the mantle wedge is deeply modified by subduction-related components. In correspondence to Hudson and the nearby monogenetic centres, the MORB-type primary source component is modified by altered oceanic crust and variably mixed with andesitic magmas having a calc-alkaline signature. A contribution from partial melting of the continental lithosphere may be present in the complex source mixing process at the border of the slab window." @default.
• W2068328265 created "2016-06-24" @default.
• W2068328265 creator A5038907107 @default.
• W2068328265 creator A5047396865 @default.
• W2068328265 creator A5052935512 @default.
• W2068328265 creator A5057709474 @default.
• W2068328265 creator A5062594769 @default.
• W2068328265 date "2005-07-01" @default.
• W2068328265 modified "2023-10-14" @default.
• W2068328265 title "The Hudson Volcano and surrounding monogenetic centres (Chilean Patagonia): An example of volcanism associated with ridge–trench collision environment" @default.
• W2068328265 cites W1964420377 @default.
• W2068328265 cites W1965545777 @default.
• W2068328265 cites W1966162447 @default.
• W2068328265 cites W1969859799 @default.
• W2068328265 cites W1978158257 @default.
• W2068328265 cites W1980254060 @default.
• W2068328265 cites W1983626964 @default.
• W2068328265 cites W1987166327 @default.
• W2068328265 cites W1988790976 @default.
• W2068328265 cites W1989698386 @default.
• W2068328265 cites W1997142214 @default.
• W2068328265 cites W2000508096 @default.
• W2068328265 cites W2009637151 @default.
• W2068328265 cites W2010543048 @default.
• W2068328265 cites W2021987309 @default.
• W2068328265 cites W2024575502 @default.
• W2068328265 cites W2025798495 @default.
• W2068328265 cites W2037771237 @default.
• W2068328265 cites W2055168533 @default.
• W2068328265 cites W2057015318 @default.
• W2068328265 cites W2058788512 @default.
• W2068328265 cites W2060535206 @default.
• W2068328265 cites W2060823328 @default.
• W2068328265 cites W2088644964 @default.
• W2068328265 cites W2091757178 @default.
• W2068328265 cites W2093843532 @default.
• W2068328265 cites W2115393563 @default.
• W2068328265 cites W2124389830 @default.
• W2068328265 cites W2128353510 @default.
• W2068328265 cites W2166777370 @default.
• W2068328265 cites W2167887033 @default.
• W2068328265 cites W2277036915 @default.
• W2068328265 cites W4245638129 @default.
• W2068328265 doi "https://doi.org/10.1016/j.jvolgeores.2005.01.014" @default.
• W2068328265 hasPublicationYear "2005" @default.
• W2068328265 type Work @default.
• W2068328265 sameAs 2068328265 @default.
• W2068328265 citedByCount "71" @default.
• W2068328265 countsByYear W20683282652012 @default.
• W2068328265 countsByYear W20683282652013 @default.
• W2068328265 countsByYear W20683282652014 @default.
• W2068328265 countsByYear W20683282652015 @default.
• W2068328265 countsByYear W20683282652016 @default.
• W2068328265 countsByYear W20683282652017 @default.
• W2068328265 countsByYear W20683282652018 @default.
• W2068328265 countsByYear W20683282652019 @default.
• W2068328265 countsByYear W20683282652020 @default.
• W2068328265 countsByYear W20683282652021 @default.
• W2068328265 countsByYear W20683282652022 @default.
• W2068328265 countsByYear W20683282652023 @default.
• W2068328265 crossrefType "journal-article" @default.
• W2068328265 hasAuthorship W2068328265A5038907107 @default.
• W2068328265 hasAuthorship W2068328265A5047396865 @default.
• W2068328265 hasAuthorship W2068328265A5052935512 @default.
• W2068328265 hasAuthorship W2068328265A5057709474 @default.
• W2068328265 hasAuthorship W2068328265A5062594769 @default.
• W2068328265 hasConcept C109902934 @default.
• W2068328265 hasConcept C120806208 @default.
• W2068328265 hasConcept C121704057 @default.
• W2068328265 hasConcept C127313418 @default.
• W2068328265 hasConcept C151730666 @default.
• W2068328265 hasConcept C155310634 @default.
• W2068328265 hasConcept C165205528 @default.
• W2068328265 hasConcept C17409809 @default.
• W2068328265 hasConcept C178790620 @default.
• W2068328265 hasConcept C185592680 @default.
• W2068328265 hasConcept C1965285 @default.
• W2068328265 hasConcept C2779227376 @default.
• W2068328265 hasConcept C32277403 @default.
• W2068328265 hasConcept C38652104 @default.
• W2068328265 hasConcept C41008148 @default.
• W2068328265 hasConcept C6363049 @default.
• W2068328265 hasConcept C77928131 @default.
• W2068328265 hasConceptScore W2068328265C109902934 @default.
• W2068328265 hasConceptScore W2068328265C120806208 @default.
• W2068328265 hasConceptScore W2068328265C121704057 @default.
• W2068328265 hasConceptScore W2068328265C127313418 @default.
• W2068328265 hasConceptScore W2068328265C151730666 @default.
• W2068328265 hasConceptScore W2068328265C155310634 @default.
• W2068328265 hasConceptScore W2068328265C165205528 @default.
• W2068328265 hasConceptScore W2068328265C17409809 @default.
• W2068328265 hasConceptScore W2068328265C178790620 @default.
• W2068328265 hasConceptScore W2068328265C185592680 @default.
• W2068328265 hasConceptScore W2068328265C1965285 @default.
• W2068328265 hasConceptScore W2068328265C2779227376 @default.
• W2068328265 hasConceptScore W2068328265C32277403 @default.
• W2068328265 hasConceptScore W2068328265C38652104 @default.
• W2068328265 hasConceptScore W2068328265C41008148 @default.

• next