The April Sumatra shaker was a strike-slip earthquake, in which two parts of the Earth's crust slide past each other horizontally. "We were very excited to see this because an earthquake this large, involving this complicated a fault system, does not happen very often," Meng told OurAmazingPlanet.
This model does not exclude the possibility of some diffuse and smooth E‐W rupture components along conjugate strike‐slip faults at local scales, that might not be resolved by the back projection analysis. The rupture of these earthquakes occurred on multiple, almost orthogonal faults. 2 March 2016. image copyright AFP. On the extensional side, everything is looser and easier to break," Meng explained. High-frequency source imaging of the 2011 October 23 Van (Eastern Turkey) earthquake by backprojection of strong motion waveforms. [25] Heterogeneous initial stress distribution, suggested by the diffuse seismicity in this region, can control the triggered rupture locations, and the nearly instantaneous rupture initiation. The quake was not only the 11th largest quakerecorded by seismometers, it's also the largest strike-slip quake on the books. Back projection results for the Mw 8.6 mainshock. Analysis of the surface-wave amplitudes suggests that the Mw=8.2 aftershock had a large centroid depth between 30 km and 40 km. This work has been partly supported by the EU Initial Training Network QUEST (QUantitative estimation of Earth's seismic sources and STructure). The third fault (F3) started at 80s and ruptured unilaterally towards WNW. Seismologist Thorne Lay, who was not involved in the study, said the research has drawbacks because the imaging method can't resolve the earthquake's depth, nor the length each fault slipped. Composition and Structure, Atmospheric Transient rheology of the oceanic asthenosphere following the 2012 Indian Ocean Earthquake inferred from geodetic data. Areas subject to warnings included Tamil Nadu, Andhra Pradesh and the Union Territory of Andaman and Nicobar Islands. Understanding the conditions that caused such a strange quake could help scientists predict whether this mechanism is possible elsewhere on the planet. The April Sumatra shaker was a strike-slip earthquake, in which two parts of the Earth's crust slide past each other horizontally.
[26] The 11 April 2012, Mw 8.6 earthquake provides evidence – as revealed by back projection and Love wave analysis – of a complex rupture sequence reactivating inherited NNE‐trending left‐lateral strike‐slip faults of the oceanic fabric. [48], Six Andaman coast provinces urged people to go to high ground and stay away from areas that could be affected.
The April Sumatra shaker was a strike-slip earthquake, in which two parts of the Earth's crust slide past each other horizontally. Lay is one of hundreds of scientists dissecting the quake for what it can reveal about how oceanic plates form new boundaries.
Multi-fault Rupture and Dynamic Triggering During the 2012 Mw 8.6 Sumatra Earthquake.
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