FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1969936638> ?p ?o ?g. }

• W1969936638 endingPage "23370" @default.
• W1969936638 startingPage "23353" @default.
• W1969936638 abstract "We use the GPS velocity field (1988–1998) for eastern Mediterranean and Asia Minor to determine the crustal deformation strain rate field in an area bounded by 35°N and 43°N, and 20°E and 48°E. We calculate the normal and shear strain rate components associated with the major faults and compare these qualitatively with seismological data. Uncertainties in the calculation of the strain rates reach 50 nstrain yr−1 in sparsely observed parts of Anatolia, whereas we estimate errors <20 nstrain yr−1 in the Aegean and Marmara regions. The largest compressional strain rate components in the eastern part of the study area occur along the Greater Caucasus mountain front reaching 70 nstrain yr−1. (1 nstrain yr−1 = 0.0317 × 10−15 s−1). The North Anatolian Fault Zone is the clearest feature in the shear strain rate field. It is expressed as a pronounced dextral strike-slip fault zone, reaching rates of up to 170 nstrain yr−1. This holds true also for the Izmit area, where the August 17, 1999, earthquake occurred. Central Anatolia is almost strain-free, whereas extension prevails in western Anatolia. The principal axes of extension vary around the N-S direction with strain rates of up to 85 nstrain yr−1. These extensional areas coincide with graben features and normal faulting earthquakes. The central and southwestern Aegean Sea is strain-free with values far below 40 nstrain yr−1. The seismic cluster around the Dodekanissa islands, southeastern Aegean Sea, coincides with NW-SE oriented extension, attaining strain rates of up to 90 nstrain yr−1. This area of extension also exhibits recent active volcanism. The entire Hellenic arc shows compressional strain rates perpendicular to the arc. The Pliny-Strabo troughs along the eastern segment of the arc show left-lateral shear strain rates reaching 80 nstrain yr−1. Significant extension is found in central Greece, with a NNE-SSW oriented maximum of 120 nstrain yr−1 centered around the Gulf of Corinthos. The Kephalonia Fault Zone in NW Greece is a distinct dextral fault zone, separating Apulia from the rapidly moving Aegean microplate. Right-lateral shear strain rates reach 150 nstrain yr−1." @default.
• W1969936638 created "2016-06-24" @default.
• W1969936638 creator A5026396690 @default.
• W1969936638 creator A5033642531 @default.
• W1969936638 creator A5035218837 @default.
• W1969936638 creator A5042014141 @default.
• W1969936638 creator A5043886045 @default.
• W1969936638 creator A5054007079 @default.
• W1969936638 creator A5067826702 @default.
• W1969936638 date "2000-10-10" @default.
• W1969936638 modified "2023-09-29" @default.
• W1969936638 title "GPS-derived strain rate field within the boundary zones of the Eurasian, African, and Arabian Plates" @default.
• W1969936638 cites W1563372296 @default.
• W1969936638 cites W1968051197 @default.
• W1969936638 cites W1969303804 @default.
• W1969936638 cites W1975955960 @default.
• W1969936638 cites W1982538753 @default.
• W1969936638 cites W1986043684 @default.
• W1969936638 cites W1987733050 @default.
• W1969936638 cites W1988610900 @default.
• W1969936638 cites W1990633455 @default.
• W1969936638 cites W1992492706 @default.
• W1969936638 cites W1994104267 @default.
• W1969936638 cites W2003235102 @default.
• W1969936638 cites W2003360552 @default.
• W1969936638 cites W2003387798 @default.
• W1969936638 cites W2009922398 @default.
• W1969936638 cites W2010639218 @default.
• W1969936638 cites W2011625549 @default.
• W1969936638 cites W2012416853 @default.
• W1969936638 cites W2014655678 @default.
• W1969936638 cites W2017786436 @default.
• W1969936638 cites W2018314772 @default.
• W1969936638 cites W2020504122 @default.
• W1969936638 cites W2023815011 @default.
• W1969936638 cites W2024301974 @default.
• W1969936638 cites W2025021642 @default.
• W1969936638 cites W2027287476 @default.
• W1969936638 cites W2028093597 @default.
• W1969936638 cites W2033237879 @default.
• W1969936638 cites W2036974706 @default.
• W1969936638 cites W2039641351 @default.
• W1969936638 cites W2045147022 @default.
• W1969936638 cites W2048403692 @default.
• W1969936638 cites W2065204617 @default.
• W1969936638 cites W2067566353 @default.
• W1969936638 cites W2068018576 @default.
• W1969936638 cites W2075357542 @default.
• W1969936638 cites W2079902474 @default.
• W1969936638 cites W2084027353 @default.
• W1969936638 cites W2090710885 @default.
• W1969936638 cites W2091247096 @default.
• W1969936638 cites W2093035173 @default.
• W1969936638 cites W2095108374 @default.
• W1969936638 cites W2098845756 @default.
• W1969936638 cites W2100464589 @default.
• W1969936638 cites W2112406160 @default.
• W1969936638 cites W2114233384 @default.
• W1969936638 cites W2119013072 @default.
• W1969936638 cites W2119117154 @default.
• W1969936638 cites W2120270422 @default.
• W1969936638 cites W2122341820 @default.
• W1969936638 cites W2122562158 @default.
• W1969936638 cites W2123560443 @default.
• W1969936638 cites W2124826797 @default.
• W1969936638 cites W2130884704 @default.
• W1969936638 cites W2135494568 @default.
• W1969936638 cites W2146315248 @default.
• W1969936638 cites W2150075840 @default.
• W1969936638 cites W2154259004 @default.
• W1969936638 cites W2154927979 @default.
• W1969936638 cites W2155472085 @default.
• W1969936638 cites W2156701839 @default.
• W1969936638 cites W2163013223 @default.
• W1969936638 cites W2166074915 @default.
• W1969936638 cites W2167738573 @default.
• W1969936638 cites W2168504837 @default.
• W1969936638 cites W2169010106 @default.
• W1969936638 cites W2169912626 @default.
• W1969936638 cites W2174857550 @default.
• W1969936638 doi "https://doi.org/10.1029/2000jb900238" @default.
• W1969936638 hasPublicationYear "2000" @default.
• W1969936638 type Work @default.
• W1969936638 sameAs 1969936638 @default.
• W1969936638 citedByCount "201" @default.
• W1969936638 countsByYear W19699366382012 @default.
• W1969936638 countsByYear W19699366382013 @default.
• W1969936638 countsByYear W19699366382014 @default.
• W1969936638 countsByYear W19699366382015 @default.
• W1969936638 countsByYear W19699366382016 @default.
• W1969936638 countsByYear W19699366382017 @default.
• W1969936638 countsByYear W19699366382018 @default.
• W1969936638 countsByYear W19699366382019 @default.
• W1969936638 countsByYear W19699366382020 @default.
• W1969936638 countsByYear W19699366382021 @default.
• W1969936638 countsByYear W19699366382022 @default.
• W1969936638 countsByYear W19699366382023 @default.
• W1969936638 crossrefType "journal-article" @default.

• next