FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2005751807> ?p ?o ?g. }

• W2005751807 abstract "La Reunion Island is located east of Madagascar, on the eastern rim of the tectonically inactive Mascarene Basin. This island is composed of three shield volcanoes of which only Piton de la Fournaise is currently active. Although the magmatic activity is restricted to Piton de la Fournaise, a scattered seismicity occurs on the whole 200 km wide volcanic edifice and in the underlying oceanic crust. We carried out a multiscale analysis to understand (1) the origin of the seismicity in the geodynamic context and (2) the role of the oceanic lithosphere in the deformation of Piton de la Fournaise and La Reunion Island. Analysis of the magmatic system suggests that the magma ascent is controlled by large N25–30 and N125–130 fracture zones located below the Enclos depression. We also show that the orientation difference between the eruptive fissures and the related dykes result from a rotation of the main principal stress s 1 from vertical to downslope through the surface. Combining a Digital Elevation Model (DEM) analysis, field observations and the geophysical data reveals that the volcano is affected by large fault zones. The fault distribution indicates the predominance of a main N70–80 trend. Magnetic data show the same N80 orientation characterizing the remnant part of the Alizes volcano. Such parallel alignment suggests a control exerted by the underlying Alizes volcano on Piton de la Fournaise. Furthermore, the alignment between the crustal orientations and the structures determined on the island suggests a control of the crustal structures in La Reunion 's volcano-tectonic activity. Contrary to several volcanic islands such as Hawaii and Tenerife, La Reunion volcanoes lie on an upbending crust. Then, we interpret the reactivation of the crustal faults as resulting from a crustal uplift related to the thermal erosion of the base of the lithosphere and/or to strong underplating. The upward deformation may prevent the spreading of the volcanoes, as no evidence of such a mechanism is observed in the bathymetry and the seismic data around the island." @default.
• W2005751807 created "2016-06-24" @default.
• W2005751807 creator A5026201680 @default.
• W2005751807 creator A5041940576 @default.
• W2005751807 creator A5062807772 @default.
• W2005751807 creator A5064124759 @default.
• W2005751807 creator A5068546731 @default.
• W2005751807 date "2007-04-01" @default.
• W2005751807 modified "2023-10-16" @default.
• W2005751807 title "Role of the structural inheritance of the oceanic lithosphere in the magmato-tectonic evolution of Piton de la Fournaise volcano (La Réunion Island)" @default.
• W2005751807 cites W1964830279 @default.
• W2005751807 cites W1969043522 @default.
• W2005751807 cites W1972876155 @default.
• W2005751807 cites W1975865189 @default.
• W2005751807 cites W1983044404 @default.
• W2005751807 cites W1984633020 @default.
• W2005751807 cites W1987202851 @default.
• W2005751807 cites W1987469482 @default.
• W2005751807 cites W1987475016 @default.
• W2005751807 cites W1988526773 @default.
• W2005751807 cites W1989157479 @default.
• W2005751807 cites W1992392416 @default.
• W2005751807 cites W1993066972 @default.
• W2005751807 cites W1996722139 @default.
• W2005751807 cites W2002390968 @default.
• W2005751807 cites W2003065810 @default.
• W2005751807 cites W2003929138 @default.
• W2005751807 cites W2007976460 @default.
• W2005751807 cites W2009666852 @default.
• W2005751807 cites W2012761784 @default.
• W2005751807 cites W2013766868 @default.
• W2005751807 cites W2020207541 @default.
• W2005751807 cites W2021644533 @default.
• W2005751807 cites W2021959819 @default.
• W2005751807 cites W2023293621 @default.
• W2005751807 cites W2024628346 @default.
• W2005751807 cites W2024739660 @default.
• W2005751807 cites W2029385518 @default.
• W2005751807 cites W2033303468 @default.
• W2005751807 cites W2035476330 @default.
• W2005751807 cites W2037569275 @default.
• W2005751807 cites W2037694551 @default.
• W2005751807 cites W2040173943 @default.
• W2005751807 cites W2046209518 @default.
• W2005751807 cites W2047651020 @default.
• W2005751807 cites W2055046013 @default.
• W2005751807 cites W2056566505 @default.
• W2005751807 cites W2056602094 @default.
• W2005751807 cites W2060680501 @default.
• W2005751807 cites W2066817069 @default.
• W2005751807 cites W2070118294 @default.
• W2005751807 cites W2071369812 @default.
• W2005751807 cites W2078364333 @default.
• W2005751807 cites W2079932865 @default.
• W2005751807 cites W2088129046 @default.
• W2005751807 cites W2093702694 @default.
• W2005751807 cites W2095073065 @default.
• W2005751807 cites W2095404506 @default.
• W2005751807 cites W2100740530 @default.
• W2005751807 cites W2105439983 @default.
• W2005751807 cites W2124698015 @default.
• W2005751807 cites W2134401338 @default.
• W2005751807 cites W2153846210 @default.
• W2005751807 cites W2153941554 @default.
• W2005751807 cites W2162389023 @default.
• W2005751807 cites W4251205546 @default.
• W2005751807 doi "https://doi.org/10.1029/2006jb004598" @default.
• W2005751807 hasPublicationYear "2007" @default.
• W2005751807 type Work @default.
• W2005751807 sameAs 2005751807 @default.
• W2005751807 citedByCount "45" @default.
• W2005751807 countsByYear W20057518072012 @default.
• W2005751807 countsByYear W20057518072013 @default.
• W2005751807 countsByYear W20057518072014 @default.
• W2005751807 countsByYear W20057518072015 @default.
• W2005751807 countsByYear W20057518072016 @default.
• W2005751807 countsByYear W20057518072017 @default.
• W2005751807 countsByYear W20057518072018 @default.
• W2005751807 countsByYear W20057518072019 @default.
• W2005751807 countsByYear W20057518072020 @default.
• W2005751807 countsByYear W20057518072021 @default.
• W2005751807 countsByYear W20057518072022 @default.
• W2005751807 crossrefType "journal-article" @default.
• W2005751807 hasAuthorship W2005751807A5026201680 @default.
• W2005751807 hasAuthorship W2005751807A5041940576 @default.
• W2005751807 hasAuthorship W2005751807A5062807772 @default.
• W2005751807 hasAuthorship W2005751807A5064124759 @default.
• W2005751807 hasAuthorship W2005751807A5068546731 @default.
• W2005751807 hasBestOaLocation W20057518072 @default.
• W2005751807 hasConcept C104317684 @default.
• W2005751807 hasConcept C120806208 @default.
• W2005751807 hasConcept C127313418 @default.
• W2005751807 hasConcept C165205528 @default.
• W2005751807 hasConcept C16942324 @default.
• W2005751807 hasConcept C185592680 @default.
• W2005751807 hasConcept C2780902518 @default.
• W2005751807 hasConcept C55493867 @default.
• W2005751807 hasConcept C77928131 @default.
• W2005751807 hasConcept C8058405 @default.
• W2005751807 hasConceptScore W2005751807C104317684 @default.

• next