FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3022233312> ?p ?o ?g. }

• W3022233312 endingPage "794" @default.
• W3022233312 startingPage "781" @default.
• W3022233312 abstract "SUMMARY We present results from complementary geological, topographic, seismic and electrical resistivity surveys at the Sagebrush Flat (SGB) site along the Clark fault (CF) strand of the San Jacinto fault zone trifurcation area southeast of Anza, California. Joint interpretation of these data sets, each with unique spatiotemporal sensitivities, allow us to better characterize the shallow (&lt;100 m) fault zone at this structurally complex site. Geological mapping at the surface shows the CF has three main subparallel strands within a &lt;100 m zone with varying degrees of rock damage. These strands intersect units of banded gneiss and tonalite, and various sedimentary units. Near the surface, the weathered but more intact tonalite and gneiss to the southwest have relatively high VP. The low-lying flat sedimentary basins around the two southwestern-most CF strands and elevated damaged gneiss to the northeast have lowest VP &lt;500 m s–1. The high relief of the northeast gneiss unit may in part be explained by its extensive damage and inferred increased relative rock uplift. Resistivity imaging shows the unconsolidated dry basin sediments (maximum &gt;1300 Ohm.m) contrasted against the compacted fine-grained (potentially wet) materials within the CF core and the Bautista Formation (minimum &lt;40 Ohm.m), which is slightly elevated above the flat basins. The inverse relationship between VP (increases) and resistivity (decreases) in the uppermost ∼15 m can be characterized as log–log linear with slopes of –2.6 to –4. At depths &gt;30 m, the velocity heterogeneity near the surface merges into larger-scale structures that are generally slower on the northeast side of the CF core compared to the southwest side (as much as ∼40 per cent reduction in average VP). A previous study revealed a 20–37 per cent variability in peak ground velocities across the SGB site from local earthquakes. The upper end of that range is associated with the near-surface unconsolidated sedimentary basins and northeast damaged gneiss unit. Preliminary analysis of time-dependent topography mostly shows effects of changing vegetation and anthropogenic activity." @default.
• W3022233312 created "2020-05-13" @default.
• W3022233312 creator A5002807424 @default.
• W3022233312 creator A5004304350 @default.
• W3022233312 creator A5010050328 @default.
• W3022233312 creator A5026928687 @default.
• W3022233312 creator A5029852137 @default.
• W3022233312 creator A5030482390 @default.
• W3022233312 creator A5034726474 @default.
• W3022233312 creator A5058734061 @default.
• W3022233312 creator A5065288025 @default.
• W3022233312 creator A5065806271 @default.
• W3022233312 date "2020-05-08" @default.
• W3022233312 modified "2023-10-17" @default.
• W3022233312 title "Characterizing the uppermost 100 m structure of the San Jacinto fault zone southeast of Anza, California, through joint analysis of geological, topographic, seismic and resistivity data" @default.
• W3022233312 cites W1912010173 @default.
• W3022233312 cites W1932721871 @default.
• W3022233312 cites W1968108815 @default.
• W3022233312 cites W1974058309 @default.
• W3022233312 cites W1989207350 @default.
• W3022233312 cites W2002636854 @default.
• W3022233312 cites W2003903842 @default.
• W3022233312 cites W2019705024 @default.
• W3022233312 cites W2052687779 @default.
• W3022233312 cites W2059330631 @default.
• W3022233312 cites W2072073142 @default.
• W3022233312 cites W2077208327 @default.
• W3022233312 cites W2078361545 @default.
• W3022233312 cites W2079641133 @default.
• W3022233312 cites W2092297207 @default.
• W3022233312 cites W2095145341 @default.
• W3022233312 cites W2097918861 @default.
• W3022233312 cites W2100016178 @default.
• W3022233312 cites W2103817435 @default.
• W3022233312 cites W2113482505 @default.
• W3022233312 cites W2116740019 @default.
• W3022233312 cites W2122938374 @default.
• W3022233312 cites W2127995641 @default.
• W3022233312 cites W2131732249 @default.
• W3022233312 cites W2139661095 @default.
• W3022233312 cites W2149511653 @default.
• W3022233312 cites W2150385097 @default.
• W3022233312 cites W2151019104 @default.
• W3022233312 cites W2156431740 @default.
• W3022233312 cites W2162496306 @default.
• W3022233312 cites W2163633222 @default.
• W3022233312 cites W2404231269 @default.
• W3022233312 cites W2530019569 @default.
• W3022233312 cites W2533457035 @default.
• W3022233312 cites W2597566553 @default.
• W3022233312 cites W2602008414 @default.
• W3022233312 cites W2756965174 @default.
• W3022233312 cites W2780513956 @default.
• W3022233312 cites W2793973629 @default.
• W3022233312 cites W2800091273 @default.
• W3022233312 cites W2891947898 @default.
• W3022233312 cites W2898845733 @default.
• W3022233312 cites W2900971158 @default.
• W3022233312 cites W2914139646 @default.
• W3022233312 cites W2935862809 @default.
• W3022233312 doi "https://doi.org/10.1093/gji/ggaa204" @default.
• W3022233312 hasPublicationYear "2020" @default.
• W3022233312 type Work @default.
• W3022233312 sameAs 3022233312 @default.
• W3022233312 citedByCount "15" @default.
• W3022233312 countsByYear W30222333122020 @default.
• W3022233312 countsByYear W30222333122021 @default.
• W3022233312 countsByYear W30222333122022 @default.
• W3022233312 countsByYear W30222333122023 @default.
• W3022233312 crossrefType "journal-article" @default.
• W3022233312 hasAuthorship W3022233312A5002807424 @default.
• W3022233312 hasAuthorship W3022233312A5004304350 @default.
• W3022233312 hasAuthorship W3022233312A5010050328 @default.
• W3022233312 hasAuthorship W3022233312A5026928687 @default.
• W3022233312 hasAuthorship W3022233312A5029852137 @default.
• W3022233312 hasAuthorship W3022233312A5030482390 @default.
• W3022233312 hasAuthorship W3022233312A5034726474 @default.
• W3022233312 hasAuthorship W3022233312A5058734061 @default.
• W3022233312 hasAuthorship W3022233312A5065288025 @default.
• W3022233312 hasAuthorship W3022233312A5065806271 @default.
• W3022233312 hasConcept C109007969 @default.
• W3022233312 hasConcept C114793014 @default.
• W3022233312 hasConcept C119599485 @default.
• W3022233312 hasConcept C127313418 @default.
• W3022233312 hasConcept C127413603 @default.
• W3022233312 hasConcept C165205528 @default.
• W3022233312 hasConcept C170154142 @default.
• W3022233312 hasConcept C171701179 @default.
• W3022233312 hasConcept C17409809 @default.
• W3022233312 hasConcept C175551986 @default.
• W3022233312 hasConcept C18555067 @default.
• W3022233312 hasConcept C26687426 @default.
• W3022233312 hasConcept C6494504 @default.
• W3022233312 hasConcept C69990965 @default.
• W3022233312 hasConceptScore W3022233312C109007969 @default.
• W3022233312 hasConceptScore W3022233312C114793014 @default.
• W3022233312 hasConceptScore W3022233312C119599485 @default.
• W3022233312 hasConceptScore W3022233312C127313418 @default.

• next