10/2/2023 0 Comments A strike slip fault![]() ![]() Si specifica inoltre che la simulazione contiene calcoli effettuati con dati e algoritmi di pubblico dominio e deve quindi essere considerata come un mero ausilio al calcolo svolgibile manualmente o con strumenti equivalenti. Cineca, l’Università di Modena e Reggio Emilia e il Focus Group IRIS non si assumono alcuna responsabilità in merito all’uso che il diretto interessato o terzi faranno della simulazione. La presente simulazione è stata realizzata sulla base delle specifiche raccolte sul tavolo ER del Focus Group IRIS coordinato dall’Università di Modena e Reggio Emilia e delle regole riportate nel DM 589/2018 e allegata Tabella A. Si consideri che Anvur calcola i valori degli indicatori all'ultima data utile per la presentazione delle domande. ![]() La simulazione può differire dall'esito di un’eventuale domanda ASN sia per errori di catalogazione e/o dati mancanti in IRIS, sia per la variabilità dei dati bibliometrici nel tempo. La simulazione si basa sui dati IRIS e sugli indicatori bibliometrici alla data indicata e non tiene conto di eventuali periodi di congedo obbligatorio, che in sede di domanda ASN danno diritto a incrementi percentuali dei valori. Si ricorda che il superamento dei valori soglia (almeno 2 su 3) è requisito necessario ma non sufficiente al conseguimento dell'abilitazione. Il report seguente simula gli indicatori relativi alla propria produzione scientifica in relazione alle soglie ASN 2021-2023 del proprio SC/SSD. Slip distribution of the FebruMw 7.8 and Mw 7.6, Kahramanmaraş, Turkey earthquake sequence in the East Anatolian Fault Zone Barbot Sylvain Luo Heng Wang Teng Hamiel Yariv Piatibratova Oksana Muhammad Tahir Braitenberg Carla Gurbuz Gokhan Abstract These events underscore the high seismic potential of immature fault systems. For the mainshock, rupture propagation stopped southward at the diffuse termination of the East Anatolian fault and tapered off northward into the Pütürge segment, some 20 km south of the 2020 Mw 6.8 Elaziğ earthquake, highlighting a potential seismic gap. Most aftershocks cluster at major fault bends, surround the regions of high coseismic slip, or extend outward of the ruptured faults. Coseismic slip extends from the surface to about 15 km depth with a shallow slip deficit. High-rate Global Navigation Satellite System data constrain each event separately. Pixel tracking of optical and synthetic aperture radar data of the Sentinel-2 and Sentinel-1 satellites, respectively, provide near-field surface displacements. We use remote-sensing observations to constrain the spatial distribution of coseismic slip for these two events and the February 20 Mw 6.4 aftershock near Antakya. The Mw 7.6 aftershock involved nearby left-lateral strike-slip faults of the East Anatolian Fault Zone, causing a 150 km-long rupture. The moment magnitude (Mw) 7.8 mainshock ruptured a 310 km-long segment of the left-lateral East Anatolian Fault, propagating through multiple releasing step-overs. On February 6, 2023, two large earthquakes occurred near the Turkish town of Kahramanmaraş. 1 Contributo in Rivista(Articolo Rivista).It can count higher than most cats.Į-mail C.E. This cat has just spotted some strike-slip fault motion. Because you have to step to the right to go from one side of the volcano to the other, this is a right-lateral strike-slip fault. This is the remains of a cinder cone that erupted along a strike-slip fault in the southern end of Death Valley, CA. A Creative Culinary Twist to Fault Line DemonstrationsSimulate and learn about the natural geological occurrences common on Earth with the geology models. If it requires a jog to the left, it was a left-lateral fault that did the offsetting. If you have to go to your right to make the connection, you have a right-lateral fault. To determine what type you've got, figure out which way a particular object, say a road or a fence, was offset by the fault motion. Strike-slip faults are either right-lateral or left-lateral. Strike slip faults involve motion in a horizontal plane: they are best spotted from the air! This makes them relatively easy to spot in a road cut or mountain side. (b) Hand sample of dextral strike-slip fault with slickolite characteristics. (a) Dextral strike-slip fault exhibits slickolite characteristics, including teeth pointing toward the right indicative of pressure-solution slip. Normal faults, reverse faults, and thrust faults all involve a substantial amount of vertical motion. Mesoscale strike-slip faults in Permian San Andres Formation (east of Mayhill, New Mexico, U.S.A.).
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