FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2146148521> ?p ?o ?g. }

• W2146148521 endingPage "504" @default.
• W2146148521 startingPage "483" @default.
• W2146148521 abstract "The east and west rupture directions of the 1943 and 1944 earthquakes on the North Anatolian Fault (NAF) are hypothesized to represent, respectively, long term preferred propagation directions on the corresponding sections of the NAF. Fault sections with preferred rupture direction are expected to have an asymmetric damage structure with respect to the slipping zone. To test the above hypothesis, we study geological and geomorphologic manifestations of structural asymmetry with respect to the active trace of the NAF along the 1943 and 1944 sections. The following fault zone elements are mapped: gouge fabric in the cm scale, fault core structure in a metre scale, and secondary faults and fault rocks in tens of metres scale. Mapping results at three sites on the 1943 rupture and one site on the 1944 rupture are consistent with accumulation of more rock damage on the south side of the 1943 section and on the north side of the 1944 section. Erosion patterns adjacent to the fault that are not correlated with the distribution of intrinsic and extrinsic erosion-controlling variables (e.g. rock type) are interpreted as morphologic responses to the damage content of rocks and its impact on rock erodibility. The valleys of 11 rivers are parallel to the studied fault sections. About 75 per cent of the total river valleys length along the 1943 rupture is on the south side of the fault, and about 89 per cent of the total river valleys length along the 1944 rupture is on the north side of the fault. Morphometric analysis of watersheds in two correlative terrains displaced along the 1944 rupture section shows that stream erosion is considerably more intense in the terrain north of the fault, with drainage density values almost double in the north compare to the south. Badland topography at two sites along the 1943 rupture section is substantially more developed at the ∼100 m scale on the south side of fault. Our observations along the 1943–1944 rupture sections, including various types of signals that span a large range of scales, are systematically compatible with an opposite sense of damage asymmetry between the two fault sections. These observations are consistent with opposite preferred direction of ruptures for the two sections, similar to the propagation directions of the two recent earthquakes. If those rupture directions are dictated by the velocity structure at depth, we infer that the south side of the 1943 rupture has faster seismic velocity at seismogenic depth than the north side, and that the sense of velocity contrast is reversed along the 1944 rupture zone." @default.
• W2146148521 created "2016-06-24" @default.
• W2146148521 creator A5002807424 @default.
• W2146148521 creator A5024635046 @default.
• W2146148521 creator A5029934147 @default.
• W2146148521 creator A5037816915 @default.
• W2146148521 creator A5046675979 @default.
• W2146148521 creator A5082528001 @default.
• W2146148521 creator A5091615003 @default.
• W2146148521 date "2008-05-01" @default.
• W2146148521 modified "2023-10-17" @default.
• W2146148521 title "Geological and geomorphologic asymmetry across the rupture zones of the 1943 and 1944 earthquakes on the North Anatolian Fault: possible signals for preferred earthquake propagation direction" @default.
• W2146148521 cites W1637028626 @default.
• W2146148521 cites W1974058309 @default.
• W2146148521 cites W1979148367 @default.
• W2146148521 cites W1984320874 @default.
• W2146148521 cites W1990436032 @default.
• W2146148521 cites W1991267034 @default.
• W2146148521 cites W1993284672 @default.
• W2146148521 cites W2001064920 @default.
• W2146148521 cites W2001719997 @default.
• W2146148521 cites W2003903842 @default.
• W2146148521 cites W2004906091 @default.
• W2146148521 cites W2005029752 @default.
• W2146148521 cites W2007109033 @default.
• W2146148521 cites W2008131857 @default.
• W2146148521 cites W2012972590 @default.
• W2146148521 cites W2023601105 @default.
• W2146148521 cites W2031052504 @default.
• W2146148521 cites W2032862640 @default.
• W2146148521 cites W2042682948 @default.
• W2146148521 cites W2044862038 @default.
• W2146148521 cites W2049508547 @default.
• W2146148521 cites W2052324772 @default.
• W2146148521 cites W2053348160 @default.
• W2146148521 cites W2055780760 @default.
• W2146148521 cites W2057042634 @default.
• W2146148521 cites W2058827292 @default.
• W2146148521 cites W2064982596 @default.
• W2146148521 cites W2065126285 @default.
• W2146148521 cites W2066091202 @default.
• W2146148521 cites W2070076047 @default.
• W2146148521 cites W2076779373 @default.
• W2146148521 cites W2082985172 @default.
• W2146148521 cites W2085424643 @default.
• W2146148521 cites W2096316748 @default.
• W2146148521 cites W2096884377 @default.
• W2146148521 cites W2100315066 @default.
• W2146148521 cites W2100855757 @default.
• W2146148521 cites W2113955130 @default.
• W2146148521 cites W2119117154 @default.
• W2146148521 cites W2119672799 @default.
• W2146148521 cites W2125171489 @default.
• W2146148521 cites W2134129319 @default.
• W2146148521 cites W2136975558 @default.
• W2146148521 cites W2139408535 @default.
• W2146148521 cites W2139604387 @default.
• W2146148521 cites W2141397675 @default.
• W2146148521 cites W2143064127 @default.
• W2146148521 cites W2146040473 @default.
• W2146148521 cites W2150161358 @default.
• W2146148521 cites W2152671523 @default.
• W2146148521 cites W2155128667 @default.
• W2146148521 cites W2155472085 @default.
• W2146148521 cites W2156316173 @default.
• W2146148521 cites W2160488308 @default.
• W2146148521 cites W2163010198 @default.
• W2146148521 cites W2345691993 @default.
• W2146148521 cites W245830586 @default.
• W2146148521 cites W4236245096 @default.
• W2146148521 cites W4302565032 @default.
• W2146148521 doi "https://doi.org/10.1111/j.1365-246x.2008.03709.x" @default.
• W2146148521 hasPublicationYear "2008" @default.
• W2146148521 type Work @default.
• W2146148521 sameAs 2146148521 @default.
• W2146148521 citedByCount "85" @default.
• W2146148521 countsByYear W21461485212012 @default.
• W2146148521 countsByYear W21461485212013 @default.
• W2146148521 countsByYear W21461485212014 @default.
• W2146148521 countsByYear W21461485212015 @default.
• W2146148521 countsByYear W21461485212016 @default.
• W2146148521 countsByYear W21461485212017 @default.
• W2146148521 countsByYear W21461485212018 @default.
• W2146148521 countsByYear W21461485212019 @default.
• W2146148521 countsByYear W21461485212020 @default.
• W2146148521 countsByYear W21461485212021 @default.
• W2146148521 countsByYear W21461485212022 @default.
• W2146148521 countsByYear W21461485212023 @default.
• W2146148521 crossrefType "journal-article" @default.
• W2146148521 hasAuthorship W2146148521A5002807424 @default.
• W2146148521 hasAuthorship W2146148521A5024635046 @default.
• W2146148521 hasAuthorship W2146148521A5029934147 @default.
• W2146148521 hasAuthorship W2146148521A5037816915 @default.
• W2146148521 hasAuthorship W2146148521A5046675979 @default.
• W2146148521 hasAuthorship W2146148521A5082528001 @default.
• W2146148521 hasAuthorship W2146148521A5091615003 @default.
• W2146148521 hasBestOaLocation W21461485211 @default.
• W2146148521 hasConcept C114679195 @default.

• next