Matches in SemOpenAlex for { <https://semopenalex.org/work/W2157859646> ?p ?o ?g. }
Showing items 1 to 75 of
75
with 100 items per page.
- W2157859646 endingPage "6" @default.
- W2157859646 startingPage "1" @default.
- W2157859646 abstract "Dating of shallow faults is crucial to understanding of the mechanism of earthquake generation and future seismic risk. However, radiometrie dating of low temperature authigenic minerals in shallow fault zones has been a major challenge because of the contamination of fault rocks by older mineral phases and the overprinting of the syn-tectonic isotopie signature by post-tectonic re-crystallisation events. We present a technique for a reliable dating of fault movements using a combined application of low temperature geochronology, mineralogy and isotope-trace element geochemistry. Such combined studies further allow constraining the origin and migration of seismically mobilised fluids along active fault zones. We investigated illitic clay minerals from fault gouges and late Quaternary carbonate deposits in co-seismic fissures along currently active fault zones in Turkey. Our results indicate that the North Anatolian Fault Zone has been active since the Late Paleocene – Early Eocene that followed immediately the continental collision related to the closure of the Neotethys Ocean. Fault movement is considered to have driven deeply sourced fluids, with metamorphic fluids being supplied by the compression along the Neotethyan orogenic suture zone. Precise dating of the late Quaternary carbonate deposits by U-series geochronology provide important constraints on the late Quaternary fissure generation related to the neotectonic processes and active faulting. Isotopie and trace element data indicate that the fissure carbonate deposits precipitated from deeply hydrothermal fluids. Mobilisation of deep fluids and their surface effusion is attributed to tectonic processes such as seismic pumping. K-Ar and U-series dating of clay and carbonate minerals respectively in seismically active areas is very promising for further studies for dating of major earthquake events and their recurrent intervals, with significant implications for the Australian active fault systems." @default.
- W2157859646 created "2016-06-24" @default.
- W2157859646 creator A5013101369 @default.
- W2157859646 creator A5025307595 @default.
- W2157859646 creator A5029439220 @default.
- W2157859646 creator A5033995989 @default.
- W2157859646 creator A5047310345 @default.
- W2157859646 creator A5048283310 @default.
- W2157859646 creator A5059216998 @default.
- W2157859646 creator A5088707527 @default.
- W2157859646 date "2006-12-01" @default.
- W2157859646 modified "2023-09-26" @default.
- W2157859646 title "Dating and geochemical tracing of paleoseismic events" @default.
- W2157859646 cites W1595855307 @default.
- W2157859646 cites W1968782051 @default.
- W2157859646 doi "https://doi.org/10.1071/aseg2006ab182" @default.
- W2157859646 hasPublicationYear "2006" @default.
- W2157859646 type Work @default.
- W2157859646 sameAs 2157859646 @default.
- W2157859646 citedByCount "0" @default.
- W2157859646 crossrefType "journal-article" @default.
- W2157859646 hasAuthorship W2157859646A5013101369 @default.
- W2157859646 hasAuthorship W2157859646A5025307595 @default.
- W2157859646 hasAuthorship W2157859646A5029439220 @default.
- W2157859646 hasAuthorship W2157859646A5033995989 @default.
- W2157859646 hasAuthorship W2157859646A5047310345 @default.
- W2157859646 hasAuthorship W2157859646A5048283310 @default.
- W2157859646 hasAuthorship W2157859646A5059216998 @default.
- W2157859646 hasAuthorship W2157859646A5088707527 @default.
- W2157859646 hasBestOaLocation W21578596461 @default.
- W2157859646 hasConcept C115393850 @default.
- W2157859646 hasConcept C127313418 @default.
- W2157859646 hasConcept C151730666 @default.
- W2157859646 hasConcept C160464908 @default.
- W2157859646 hasConcept C165205528 @default.
- W2157859646 hasConcept C17409809 @default.
- W2157859646 hasConcept C175551986 @default.
- W2157859646 hasConcept C197737763 @default.
- W2157859646 hasConcept C23295444 @default.
- W2157859646 hasConcept C26001220 @default.
- W2157859646 hasConcept C6494504 @default.
- W2157859646 hasConcept C77928131 @default.
- W2157859646 hasConceptScore W2157859646C115393850 @default.
- W2157859646 hasConceptScore W2157859646C127313418 @default.
- W2157859646 hasConceptScore W2157859646C151730666 @default.
- W2157859646 hasConceptScore W2157859646C160464908 @default.
- W2157859646 hasConceptScore W2157859646C165205528 @default.
- W2157859646 hasConceptScore W2157859646C17409809 @default.
- W2157859646 hasConceptScore W2157859646C175551986 @default.
- W2157859646 hasConceptScore W2157859646C197737763 @default.
- W2157859646 hasConceptScore W2157859646C23295444 @default.
- W2157859646 hasConceptScore W2157859646C26001220 @default.
- W2157859646 hasConceptScore W2157859646C6494504 @default.
- W2157859646 hasConceptScore W2157859646C77928131 @default.
- W2157859646 hasIssue "1" @default.
- W2157859646 hasLocation W21578596461 @default.
- W2157859646 hasOpenAccess W2157859646 @default.
- W2157859646 hasPrimaryLocation W21578596461 @default.
- W2157859646 hasRelatedWork W1990311000 @default.
- W2157859646 hasRelatedWork W2068207513 @default.
- W2157859646 hasRelatedWork W2121520662 @default.
- W2157859646 hasRelatedWork W2326305652 @default.
- W2157859646 hasRelatedWork W2347388628 @default.
- W2157859646 hasRelatedWork W2364571660 @default.
- W2157859646 hasRelatedWork W2365637645 @default.
- W2157859646 hasRelatedWork W2800280878 @default.
- W2157859646 hasRelatedWork W2900662913 @default.
- W2157859646 hasRelatedWork W3176522245 @default.
- W2157859646 hasVolume "2006" @default.
- W2157859646 isParatext "false" @default.
- W2157859646 isRetracted "false" @default.
- W2157859646 magId "2157859646" @default.
- W2157859646 workType "article" @default.