Main Frontal Thrust

Main Frontal Thrust
	Himalayan Frontal Thrust
Country	Nepal, India, Pakistan, Bhutan
Characteristics
Range	Himalayas
Length	2,400 km
Displacement	15-21 mm/yr
Tectonics
Status	Active
Type	Thrust

The Main Frontal Thrust (MFT), also known as the Himalayan Frontal Thrust (HFT) is a geological fault in the Himalayas

Figure 1. Satellite view of the Himalayas. The Main Frontal Thrust run parallel to the glaciated peaks, north of the Indo-Gangetic Plain.

that defines the boundary between the Indian and Eurasian Plates.[1] The fault is well expressed on the surface thus could be seen via satellite imagery. It is the youngest and southernmost thrust structure in the Himalaya deformation front. It is a splay branch of the Main Himalayan Thrust (MHT) as the root décollement.

It runs parallel to other major splays of the MHT; Main Boundary Thrust (MBT) and Main Central Thrust (MCT). The Sunda Megathrust, which extends from the Banda Islands to Myanmar is jointed with the MFT.[2] The fault strikes in a NW-SE direction and dips at an angle of 20° to 30° in the north.[3]

Main Boundary Thrust

The Main Boundary Thrust (MBT) is another major thrust fault in the Himalaya orogenic wedge that was active in the Cenozoic.[4] It runs parallel to the MFT with a spacing distance of about 20 km.

Shortening rate

Shortening rate varies across the MFT, these figures provide the speed in various locations.[2]


Region	Rate (mm/yr)
Pakistan	14 ± 4	minor components within the Himalayas also accounts for shortening
Northwestern India	10-14
Nepal	21 ± 1.5
Bhutan	15-20

Seismic activity

The MFT accommodates almost the entire rate of subduction of the Indian Plate therefore, it is no surprise that numerous earthquakes have occurred along this fault, and is expected to produce very big earthquakes in the future.[5] Many earthquakes associated with the MFT has resulted in visible ground ruptures, as seen in the Bihar earthquake of 1934 and 1505 magnitude 8.9 earthquake.

Reference

Paul, R.; Bhakuni, S.S. "Structural analysis of main boundary thrust and Himalayan frontal thrust around Dehra Dun, NW Himalaya: Implications of neotectonics". Summer Research Fellowship Programme of India's Science Academies. Retrieved 21 October 2020.
Burgess, W.P.; Yin, A.; Dubey, C.S.; Shen, Z–K.; Kelty, T.K. (2012). "Holocene shortening across the Main Frontal Thrust zone in the eastern Himalaya". Earth and Planetary Science Letters. 357–358: 152–167. doi:10.1016/j.epsl.2012.09.040.
Wesnousky, S.G.; Kumar, S.; Mohindra, R.; Thakur, V.C. (1999). "Uplift and convergence along the Himalayan Frontal Thrust of India". Tectonics. 18 (6): 967–976. doi:10.1029/1999TC900026.
Mugnier, J–L.; Huyghe, P.; Chalaron, E.; Mascle, G. (1994). "Recent movements along the Main Boundary Thrust of the Himalayas: Normal faulting in an over-critical thrust wedge?". Tectonophysics. 238 (1–4): 199–215. doi:10.1016/0040-1951(94)90056-6.
Bilham, R. "Himalayan earthquakes: a review of historical seismicity and early 21st century slip potential". In Treloar, P.J.; Searle, M.P. (eds.). Himalayan Tectonics: A Modern Synthesis. Geological Society, London, Special Publications. 483. pp. 423–482. doi:10.1144/SP483.16. ISBN 9781786204059.

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[Paul_&_Bhakuni_-1] Paul, R.; Bhakuni, S.S. "Structural analysis of main boundary thrust and Himalayan frontal thrust around Dehra Dun, NW Himalaya: Implications of neotectonics". Summer Research Fellowship Programme of India's Science Academies. Retrieved 21 October 2020.

[:0-2] Burgess, W.P.; Yin, A.; Dubey, C.S.; Shen, Z–K.; Kelty, T.K. (2012). "Holocene shortening across the Main Frontal Thrust zone in the eastern Himalaya". Earth and Planetary Science Letters. 357–358: 152–167. doi:10.1016/j.epsl.2012.09.040.

[Wesnousky_etal_1999-3] Wesnousky, S.G.; Kumar, S.; Mohindra, R.; Thakur, V.C. (1999). "Uplift and convergence along the Himalayan Frontal Thrust of India". Tectonics. 18 (6): 967–976. doi:10.1029/1999TC900026.

[Mugnier_etal_1994-4] Mugnier, J–L.; Huyghe, P.; Chalaron, E.; Mascle, G. (1994). "Recent movements along the Main Boundary Thrust of the Himalayas: Normal faulting in an over-critical thrust wedge?". Tectonophysics. 238 (1–4): 199–215. doi:10.1016/0040-1951(94)90056-6.

[Bilham-5] Bilham, R. "Himalayan earthquakes: a review of historical seismicity and early 21st century slip potential". In Treloar, P.J.; Searle, M.P. (eds.). Himalayan Tectonics: A Modern Synthesis. Geological Society, London, Special Publications. 483. pp. 423–482. doi:10.1144/SP483.16. ISBN 9781786204059.