FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2889478416> ?p ?o ?g. }

• W2889478416 endingPage "106439" @default.
• W2889478416 startingPage "106439" @default.
• W2889478416 abstract "The Hengill Triple Junction in Iceland is formed by the intersection of the Western Volcanic Zone (WVZ), Reykjanes Peninsula Oblique Rift (RPOR) and a transform zone, the South Iceland Seismic Zone (SISZ). The 19 × 13 km2 study area thus contains extensional structures related to volcanic systems of the two rift zones, Hengill and Hrómundartindur, as well as strike-slip structures characteristic of the transform zones. High definition aerial photographs, satellite images, and digital elevation models are used, supported by field studies, to accurately map and classify tectonic features in an effort to separate N-S trending strike-slip faults from the fissure swarms of the volcanic systems. A portion of the southern Hengill fissure swarm lies within the area. It trends NE-SW and exhibits extensional features characteristic of spreading ridges, i.e. normal faults, open fractures, and eruptive fissures. It is clearly delineated by surface fractures, and is traced a length of 28 km southwest from the central volcano, terminating before reaching the coastline. The fissure swarm is 2–3.5 km wide in the study area, widening southwards. Elevation profiles across the fissure swarm suggest a spreading rate comparable to the southern WVZ, which spreads at 4–5 mm/year. A portion of the Nesjahraun eruptive fissure is anomalously smooth and may represent secondary rifting. East-west shearing in the RPOR and SISZ is accomplished by many smaller and less conspicuous, northerly oriented strike-slip faults in a ‘bookshelf faulting’ manner. These parallel faults are overprinted on the volcano-tectonic structures of the RPOR. Evidence of 11 northerly striking strike-slip faults is found within the study area. The zone of bookshelf faulting is thus shown to be continuous across the triple junction area, from the SISZ to the RPOR. Finally, several structures (eruptive fissures, exposed dikes, and faults) strike near-perpendicular to the fissure swarm and may be the result of changes in the direction of maximum stress caused by rifting events, however, their tectonic significance remains uncertain." @default.
• W2889478416 created "2018-09-07" @default.
• W2889478416 creator A5004335931 @default.
• W2889478416 creator A5064676227 @default.
• W2889478416 creator A5071981679 @default.
• W2889478416 date "2020-02-01" @default.
• W2889478416 modified "2023-09-25" @default.
• W2889478416 title "Fault kinematics at the Hengill Triple Junction, SW-Iceland, derived from surface fracture pattern" @default.
• W2889478416 cites W1574452243 @default.
• W2889478416 cites W1626052267 @default.
• W2889478416 cites W1667447052 @default.
• W2889478416 cites W1970334697 @default.
• W2889478416 cites W1970873989 @default.
• W2889478416 cites W1977025915 @default.
• W2889478416 cites W1981989898 @default.
• W2889478416 cites W1990756051 @default.
• W2889478416 cites W2005797220 @default.
• W2889478416 cites W2008255332 @default.
• W2889478416 cites W2021542154 @default.
• W2889478416 cites W2023967092 @default.
• W2889478416 cites W2025276263 @default.
• W2889478416 cites W2027887028 @default.
• W2889478416 cites W2036767323 @default.
• W2889478416 cites W2037452070 @default.
• W2889478416 cites W2042619598 @default.
• W2889478416 cites W2048819061 @default.
• W2889478416 cites W2051046669 @default.
• W2889478416 cites W2068772241 @default.
• W2889478416 cites W2077872464 @default.
• W2889478416 cites W2079556103 @default.
• W2889478416 cites W2083829411 @default.
• W2889478416 cites W2084109837 @default.
• W2889478416 cites W2087460674 @default.
• W2889478416 cites W2087871969 @default.
• W2889478416 cites W2098642962 @default.
• W2889478416 cites W2098839042 @default.
• W2889478416 cites W2101538421 @default.
• W2889478416 cites W2103085975 @default.
• W2889478416 cites W2111065685 @default.
• W2889478416 cites W2120589127 @default.
• W2889478416 cites W2137759179 @default.
• W2889478416 cites W2143887830 @default.
• W2889478416 cites W2153613445 @default.
• W2889478416 cites W2164795160 @default.
• W2889478416 cites W2219122938 @default.
• W2889478416 cites W2219979661 @default.
• W2889478416 cites W2291847209 @default.
• W2889478416 cites W2312196794 @default.
• W2889478416 cites W2347455006 @default.
• W2889478416 cites W2497897242 @default.
• W2889478416 cites W2509668233 @default.
• W2889478416 cites W4322389010 @default.
• W2889478416 cites W4322391408 @default.
• W2889478416 cites W4322391479 @default.
• W2889478416 cites W4322579487 @default.
• W2889478416 doi "https://doi.org/10.1016/j.jvolgeores.2018.08.017" @default.
• W2889478416 hasPublicationYear "2020" @default.
• W2889478416 type Work @default.
• W2889478416 sameAs 2889478416 @default.
• W2889478416 citedByCount "11" @default.
• W2889478416 countsByYear W28894784162020 @default.
• W2889478416 countsByYear W28894784162021 @default.
• W2889478416 countsByYear W28894784162022 @default.
• W2889478416 countsByYear W28894784162023 @default.
• W2889478416 crossrefType "journal-article" @default.
• W2889478416 hasAuthorship W2889478416A5004335931 @default.
• W2889478416 hasAuthorship W2889478416A5064676227 @default.
• W2889478416 hasAuthorship W2889478416A5071981679 @default.
• W2889478416 hasConcept C106973953 @default.
• W2889478416 hasConcept C120806208 @default.
• W2889478416 hasConcept C127313418 @default.
• W2889478416 hasConcept C165205528 @default.
• W2889478416 hasConcept C169162353 @default.
• W2889478416 hasConcept C175551986 @default.
• W2889478416 hasConcept C2778282194 @default.
• W2889478416 hasConcept C2778677506 @default.
• W2889478416 hasConcept C32848823 @default.
• W2889478416 hasConcept C50682988 @default.
• W2889478416 hasConcept C52678131 @default.
• W2889478416 hasConcept C77928131 @default.
• W2889478416 hasConcept C8058405 @default.
• W2889478416 hasConceptScore W2889478416C106973953 @default.
• W2889478416 hasConceptScore W2889478416C120806208 @default.
• W2889478416 hasConceptScore W2889478416C127313418 @default.
• W2889478416 hasConceptScore W2889478416C165205528 @default.
• W2889478416 hasConceptScore W2889478416C169162353 @default.
• W2889478416 hasConceptScore W2889478416C175551986 @default.
• W2889478416 hasConceptScore W2889478416C2778282194 @default.
• W2889478416 hasConceptScore W2889478416C2778677506 @default.
• W2889478416 hasConceptScore W2889478416C32848823 @default.
• W2889478416 hasConceptScore W2889478416C50682988 @default.
• W2889478416 hasConceptScore W2889478416C52678131 @default.
• W2889478416 hasConceptScore W2889478416C77928131 @default.
• W2889478416 hasConceptScore W2889478416C8058405 @default.
• W2889478416 hasFunder F4320323298 @default.
• W2889478416 hasLocation W28894784161 @default.
• W2889478416 hasOpenAccess W2889478416 @default.
• W2889478416 hasPrimaryLocation W28894784161 @default.

• next