Seismotectonics of the April–May 2015 Nepal earthquakes: An assessment based on the aftershock patterns, surface effects and deformational characteristics

• Published in: Journal of Asian earth sciences 2015-11, Vol.111, p.161-174
• Main Authors: Parameswaran, Revathy M., Natarajan, Thulasiraman, Rajendran, Kusala, Rajendran, C.P., Mallick, Rishav, Wood, Matthew, Lekhak, Harish C.
• Format: Article
• Language: English
• Subjects: Aftershocks; Earthquakes; Nepal Himalaya; Out-of-sequence thrust; Physiographic transition; Seismicity; Surface deformation
• ISSN: 1367-9120; 1878-5786
• DOI: 10.1016/j.jseaes.2015.07.030

•The paper presents observations on the 2015 Nepal earthquakes.•Analyses the spatial temporal pattern of aftershocks.•Association of slip accommodation and surface deformation to a physiographic break is the new idea proposed.•Presents evidence for potential coseismic surface deformation.•Focuses on the importance of damage to heritage structures. Occurrence of the April 25, 2015 (Mw 7.8) earthquake near Gorkha, central Nepal, and another one that followed on May 12 (Mw 7.3), located ∼140km to its east, provides an exceptional opportunity to understand some new facets of Himalayan earthquakes. Here we attempt to assess the seismotectonics of these earthquakes based on the deformational field generated by these events, along with the spatial and temporal characteristics of their aftershocks. When integrated with some of the post-earthquake field observations, including the localization of damage and surface deformation, it became obvious that although the mainshock slip was mostly limited to the Main Himalayan Thrust (MHT), the rupture did not propagate to the Main Frontal Thrust (MFT). Field evidence, supported by the available InSAR imagery of the deformation field, suggests that a component of slip could have emerged through a previously identified out-of-sequence thrust/active thrust in the region that parallels the Main Central Thrust (MCT), known in the literature as a co-linear physiographic transitional zone called PT2. Termination of the first rupture, triggering of the second large earthquake, and distribution of aftershocks are also spatially constrained by the eastern extremity of PT2. Mechanism of the 2015 sequence demonstrates that the out-of-sequence thrusts may accommodate part of the slip, an aspect that needs to be considered in the current understanding of the mechanism of earthquakes originating on the MHT.