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References
30
[1]
Avouac, J.-P., Meng, L., Wei, S., Wang, T. & Ampuero, J.-P. Lower edge of locked Main Himalayan Thrust unzipped by the 2015 Gorkha earthquake. Nature Geosci. 8, 708–711 (2015). 10.1038/ngeo2518
[2]
Hayes, G. P. et al. Rapid characterization of the 2015 Mw 7.8 Nepal (Gorkha). Earthq. Seism. Res. Lett. 86, 1557–1567 (2015). 10.1785/0220150145
[3]
Lindsey, E. et al. Line of sight deformation from ALOS-2 interferometry: Mw 7.8 Gorkha earthquake and Mw 7.3 aftershock. Geophys. Res. Lett. 42, 6655–6661 (2015). 10.1002/2015gl065385
[4]
Galetzka, J. et al. Slip pulse and resonance of the Kathmandu Basin during the 2015 Gorkha earthquake, Nepal. Science 349, 1091–1095 (2015). 10.1126/science.aac6383
[5]
Grandin, R. et al. Rupture process of the Mw = 7.9 2015 Gorkha earthquake (Nepal): insights into Himalayan megathrust segmentation. Geophys. Res. Lett. 42, 8373–8382 (2015). 10.1002/2015gl066044
[6]
Wang, K. & Fialko, Y. Slip model of the 2015 Mw 7.8 Gorkha (Nepal) earthquake from inversions of ALOS-2 and GPS data. Geophys. Res. Lett. 42, 7452–7458 (2015). 10.1002/2015gl065201
[7]
Denolle, M. A., Fan, W. & Shearer, P. M. Dynamics of the 2015 M7.8 Nepal earthquake. Geophys. Res. Lett. 42, 7467–7475 (2015). 10.1002/2015gl065336
[8]
Elliott, J. R. et al. Geometry of the Main Himalayan Thrust. Nature Geosci. 9, 174–180 (2016). 10.1038/ngeo2623
[9]
Bilham, R., Larson, K., Freymueller, J. & Project Idylhim members. GPS measurements of present-day convergence across the Nepal Himalaya. Nature 386, 61–64 (1997). 10.1038/386061a0
[10]
Ader, T. et al. Convergence rate across the Nepal Himalaya and interseismic coupling on the Main Himalayan Thrust: implications for seismic hazard. J. Geophys. Res. 117, B044403 (2012). 10.1029/2011jb009071
[11]
Avouac, J. P. Mountain building, erosion, and the seismic cycle in the Nepal Himalaya. Adv. Geophys. 46, 1–80 (2003). 10.1016/s0065-2687(03)46001-9
[12]
Bilham, R. Earthquakes in India and the Himalaya: tectonics, geodesy and history. Ann. Geophys. 47, 839–855 (2004).
[13]
Sapkota, S. N. et al. Primary surface rupture of the great Himalayan earthquakes of 1255 and 1934. Nature Geosci. 6, 71–76 (2013). 10.1038/ngeo1669
[14]
Bollinger, L. et al. Estimating the return times of great Himalayan earthquakes in eastern Nepal: evidence from the Patu and Bardibas strands of the Main Frontal Thrust. J. Geophys. Res. 119, 7123–7163 (2014). 10.1002/2014jb010970
[15]
Kumar, S. et al. Paleoseismic evidence of great surface rupture earthquakes along the Indian Himalaya. J. Geophys. Res. 111, B03304 (2006).
[16]
Bettinelli, P. et al. Seasonal variations of seismicity and geodetic strain in the Himalaya induced by surface hydrology. Earth Planet. Sci. Lett. 266, 332–344 (2008). 10.1016/j.epsl.2007.11.021
[17]
Fu, Y & Freymueller, J. Seasonal and long-term vertical deformation in the Nepal Himalaya constrained by GPS and GRACE measurements. J. Geophys. Res. 117, 2156–2202 (2012).
[18]
Bilham, R. Location and magnitude of the 1833 Nepal earthquake and its relation to the rupture zones of contiguous great Himalayan earthquakes. Curr. Sci. 69, 101–127 (1995).
[19]
Bilham, R. & Wallace, K. Future Mw > 8 earthquakes in the Himalaya: implications from the 26 Dec 2004 Mw = 9.0 earthquake on India’s eastern plate margin. Geol. Surv. India Spl. Pub. 85, 1–14 (2005).
[20]
Mugnier, J.-L. et al. Structural interpretation of the great earthquakes of the last millennium in the central Himalaya. Earth Sci. Rev. 127, 30–47 (2013). 10.1016/j.earscirev.2013.09.003
[21]
Wallace, K., Bilham, R., Blume, F., Gaur, V. K. & Gahalaut, V. Surface deformation in the region of the 1905 Kangra Mw = 7.8 earthquake in the period 1846–2001. Geophys. Res. Lett. 32, L15307 (2005). 10.1029/2005gl022906
[22]
Avouac, J.-P. From geodetic imaging of seismic and aseismic fault slip to dynamic modeling of the seismic cycle. Ann. Rev. Earth Planet. Sci. 43, 233–271 (2015). 10.1146/annurev-earth-060614-105302
[23]
Jackson, M. & Bilham, R. Constraints on Himalayan deformation inferred from vertical velocity fields in Nepal and Tibet. J. Geophys. Res. 99, 13897–13912 (1994). 10.1029/94jb00714
[24]
Satyabala, S. P., Yang, Z. & Bilham, R. Stick–slip advance of the Kohat plateau Pakistan. Nature Geosci. 5, 147–150 (2012). 10.1038/ngeo1373
[25]
Scholz, C. H. & Campos, J. The seismic coupling of subduction zones revisited. J. Geophys. Res. 117, BO5310 (2012). 10.1029/2011jb009003
[26]
Feldl, N. & Bilham, R. Great Himalayan earthquakes and the Tibetan plateau. Nature 444, 165–170 (2006). 10.1038/nature05199
[27]
Stevens, V. L. & Avouac, J. P. Interseismic coupling of the Main Himalayan Thrust. Geophys. Res Lett. 42, 5828–5837 (2015). 10.1002/2015gl064845
[28]
Schiffman, C., Bali, B. S., Szeliga, W. & Bilham, R. Seismic slip deficit in the Kashmir Himalaya from GPS observations. Geophys. Res. Lett. 40, 5642–5645 (2013). 10.1002/2013gl057700
[29]
Ambraseys, N. & Jackson, D. A note on early earthquakes in northern India and southern Tibet. Curr. Sci. 84, 570–582 (2003).
[30]
Bollinger, L., Tapponier, P., Sapkota, S. N. & Klinger, Y. Slip deficit in central Nepal: omen for a repeat of the 1344 AD earthquake? Earth Planets Space 68, 1–12 (2016). 10.1186/s40623-016-0389-1
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Published
Jun 13, 2016
Vol/Issue
9(7)
Pages
533-537
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Cite This Article
David Mencin, Rebecca Bendick, Bishal Nath Upreti, et al. (2016). Himalayan strain reservoir inferred from limited afterslip following the Gorkha earthquake. Nature Geoscience, 9(7), 533-537. https://doi.org/10.1038/ngeo2734
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