The Main Frontal Thrust (MFT), also known as the Himalayan Frontal Thrust (HFT), is a geological fault in the Himalayas that defines the boundary between the Himalayan foothills and Indo-Gangetic Plain.[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.
^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.
and 29 Related for: Main Frontal Thrust information
The MainFrontalThrust (MFT), also known as the Himalayan FrontalThrust (HFT), is a geological fault in the Himalayas that defines the boundary between...
along splay structures including the MainFrontalThrust (MFT), Main Boundary Thrust (MBT), Main Central Thrust (MCT) and possibly the South Tibetan Detachment...
faults are South Tibetan Detachment, the Main Central Thrust, the Main Boundary Thrust and the MainFrontalThrust. These units (figure 1), from south to...
faults separating them are the MainFrontalThrust (MFT), Subhimalaya Zone (also called Sivalik), Main Boundary Thrust (MBT), Lesser Himalaya (further...
"Calculations show that there is sufficient accumulated energy [in the MainFrontalThrust], now to produce an 8-magnitude earthquake. I cannot say when. It...
the décollement for the whole thrust system. The southernmost thrust that reaches the surface is the MainFrontalThrust (MFT), which joins with the MHT...
System, Japan (near Tokyo) Uemachi Fault System, Osaka Basin, Japan MainFrontalThrust, Himalaya 1902 Turkestan earthquake – Earthquake near the China–Kyrgyzstan...
Plate is thrusted beneath the continental crust of the Eurasian Plate, forming thrust faults along the collision zone. The MainFrontalThrust predominantly...
along a series of steep faults known as the Himalayan Frontal Fault or the MainFrontalThrust. It comprises several sub-basins and all of them are quite...
structures like the MainFrontalThrust, Main Boundary Thrust and Main Central Thrust, all splay branches of the Main Himalayan Thrust, accommodate the shortening...
is thrust southwestward in the rate of 10±6 mm/yr along the MainFrontalthrust during the Quaternary. Within the sequence, rocks have been thrust and...
old. They are bounded on the south by a fault system called the MainFrontalThrust, with steeper slopes on that side. Below this, the coarse alluvial...
The main structures involved in accommodating this convergence are large thrust faults, such as the Main Central Thrust and the MainFrontalThrust. Within...
Salt Range Thrust Bannu Fault Quetta-Chiltan Fault Allah Bund Fault Hoshab Fault Makran Coastal Fault Main Mantle ThrustMainFrontalThrust Jhelum Fault...
Plate. The degree to which this deformation is partitioned into zones of thrust tectonics (accommodating that part of the motion perpendicular to the boundary)...
At the surface, the Main Himalayan Thrust propagates along the MainFrontalThrust. These faults runs for approximately 2,300 km in an east-west direction...
paleoseismicity of the region is poorly studied. The MainFrontalThrust, Medlicott-Wadia (Riasi) Thrust, as well as the Kashmir Basin Fault (then the Balapur...
plate boundary, convergent (thrust), divergent (extensional) and transform (strike-slip). There are two main types of thrust tectonics, thin-skinned and...
formation of several thrust faults including the Main Central Thrust (MCT), the Main Boundary Thrust (MBT) and the MainFrontalThrust (MFT). The MCT consists...
steeper on their southern flanks because of faults are known as the MainFrontalThrust. This range is composed of poorly consolidated, coarse sediments...
considered highly risky against earthquake due to presence of MainFrontalThrust and Main Boundary Thrust in the immediate vicinity. The torrential rainfall on...
basin, in the form of blind thrust faults, and strike-slip faults. These faults reach over 37 km south of the MainFrontalThrust, and are responsible for...
The main structures involved in accommodating this convergence are large thrust faults, such as the Main Central Thrust and the MainFrontalThrust. Within...
Frontal lobe epilepsy (FLE) is a neurological disorder that is characterized by brief, recurring seizures arising in the frontal lobes of the brain, that...
Main Boundary Thrust, Main Central Thrust and South Tibetan Detachment. At the surface, the Main Himalayan Thrust propagates along the MainFrontal Thrust...
The Zagros fold and thrust belt (Zagros FTB) is an approximately 1,800-kilometre (1,100 mi) long zone of deformed crustal rocks, formed in the foreland...
Pagodas Fault West Andaman Fault Kabaw Fault Sunda megathrust Main Himalayan ThrustMainFrontalThrust Burma Plate Sunda Plate Indian Plate Eurasian Plate...
Pagodas Fault West Andaman Fault Kabaw Fault Sunda megathrust Main Himalayan ThrustMainFrontalThrust Burma Plate Sunda Plate Indian Plate Eurasian Plate...