Himalayan Frontal Thrust
E753967
The Himalayan Frontal Thrust is the youngest and most active major fault system along the southern front of the Himalayas, accommodating much of the ongoing convergence between the Indian and Eurasian tectonic plates.
All labels observed (1)
| Label | Occurrences |
|---|---|
| Himalayan Frontal Thrust canonical | 2 |
How this entity was disambiguated
This entity first appeared as the object of triple T8716726 — resolving that mention is where its identity was fixed. The disambiguator weighed these candidate entities and picked the highlighted one (or “None”, minting a new entity). This is how homonymy is resolved: the same surface form can point to different entities.
Target entity: Himalayan Frontal Thrust Context triple: [Main Boundary Thrust zone, olderThan, Himalayan Frontal Thrust]
-
A.
Indus-Tsangpo Suture Zone
The Indus-Tsangpo Suture Zone is a major tectonic boundary in the Himalayas marking the collision zone between the Indian and Eurasian plates, where remnants of the ancient Tethys Ocean crust are preserved.
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B.
Tethyan Himalaya
Tethyan Himalaya is the northernmost tectonostratigraphic zone of the Himalayas, composed mainly of marine sedimentary rocks that record the evolution and closure of the ancient Tethys Ocean.
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C.
Altyn Tagh Fault
The Altyn Tagh Fault is a major strike-slip fault system in northwestern China that plays a key role in accommodating the tectonic deformation of the Tibetan Plateau.
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D.
Alpine-Himalayan orogenic belt
The Alpine-Himalayan orogenic belt is a vast, tectonically active mountain-building zone stretching from southern Europe through the Middle East to Southeast Asia, encompassing major ranges such as the Alps and the Himalayas.
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E.
Karakoram orogeny
The Karakoram orogeny is the mountain-building event responsible for forming the high, rugged Karakoram Range in the western Himalayas through ongoing tectonic collision and uplift.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: Himalayan Frontal Thrust Target entity description: The Himalayan Frontal Thrust is the youngest and most active major fault system along the southern front of the Himalayas, accommodating much of the ongoing convergence between the Indian and Eurasian tectonic plates.
-
A.
Indus-Tsangpo Suture Zone
The Indus-Tsangpo Suture Zone is a major tectonic boundary in the Himalayas marking the collision zone between the Indian and Eurasian plates, where remnants of the ancient Tethys Ocean crust are preserved.
-
B.
Tethyan Himalaya
Tethyan Himalaya is the northernmost tectonostratigraphic zone of the Himalayas, composed mainly of marine sedimentary rocks that record the evolution and closure of the ancient Tethys Ocean.
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C.
Altyn Tagh Fault
The Altyn Tagh Fault is a major strike-slip fault system in northwestern China that plays a key role in accommodating the tectonic deformation of the Tibetan Plateau.
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D.
Alpine-Himalayan orogenic belt
The Alpine-Himalayan orogenic belt is a vast, tectonically active mountain-building zone stretching from southern Europe through the Middle East to Southeast Asia, encompassing major ranges such as the Alps and the Himalayas.
-
E.
Karakoram orogeny
The Karakoram orogeny is the mountain-building event responsible for forming the high, rugged Karakoram Range in the western Himalayas through ongoing tectonic collision and uplift.
- F. None of above. chosen
Statements (48)
| Predicate | Object |
|---|---|
| instanceOf |
active fault system
ⓘ
geologic structure ⓘ thrust fault ⓘ |
| accommodatesConvergenceBetween |
Eurasian Plate
NERFINISHED
ⓘ
Indian Plate NERFINISHED ⓘ |
| age | Quaternary ⓘ |
| alsoKnownAs |
Himalayan Frontal Fault
NERFINISHED
ⓘ
Main Frontal Thrust NERFINISHED ⓘ |
| associatedWith |
foreland basin sedimentation
ⓘ
growth of Siwalik Hills ⓘ |
| characteristic |
most active major fault along southern Himalayan front
ⓘ
youngest major Himalayan thrust system ⓘ |
| countryCrossed |
Bhutan
NERFINISHED
ⓘ
India NERFINISHED ⓘ Nepal NERFINISHED ⓘ Pakistan NERFINISHED ⓘ |
| deformationStyle |
fault-bend folding
ⓘ
fault-propagation folding ⓘ |
| displacementType | cumulative vertical uplift of Himalayan front ⓘ |
| formsBoundaryBetween |
Indo-Gangetic foreland basin
NERFINISHED
ⓘ
Sub-Himalaya (Siwalik Range) NERFINISHED ⓘ |
| formsPartOf | Himalayan megathrust system NERFINISHED ⓘ |
| geomorphicExpression |
fault scarps
ⓘ
folded alluvial fans ⓘ river terrace offsets ⓘ |
| kinematics | northward underthrusting of Indian Plate beneath Himalaya ⓘ |
| liesSouthOf | Main Boundary Thrust NERFINISHED ⓘ |
| locatedIn |
Bhutan
NERFINISHED
ⓘ
Himalayas ⓘ Nepal NERFINISHED ⓘ Pakistan ⓘ northern India ⓘ southern margin of the Tibetan Plateau ⓘ |
| orientation | east–west trending ⓘ |
| parallelTo |
Main Boundary Thrust
NERFINISHED
ⓘ
Main Central Thrust NERFINISHED ⓘ |
| partOf | Himalayan orogen NERFINISHED ⓘ |
| relativeMotionType |
reverse faulting
ⓘ
thrusting ⓘ |
| researchField |
seismology
ⓘ
structural geology ⓘ tectonics ⓘ |
| roleInOrogeny | accommodates a large fraction of present-day Himalayan shortening ⓘ |
| seismicHazard |
capable of surface-rupturing events
ⓘ
source of large earthquakes ⓘ |
| tectonicProcess |
continental collision
ⓘ
crustal shortening ⓘ |
| tectonicSetting | convergent plate boundary ⓘ |
How these facts were elicited
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You are a knowledge base construction expert. Given a subject entity and a description of it, return factual statements that you know for the subject as a JSON list of dictionaries(triples), where keys must be "subject", "predicate" and "object". The number of facts may be very high, between 25 to 50 or more, for very popular subjects. For less popular subjects, the number of facts can be very low, like 5 or 10. # Requirements - If you don't know the subject at all, return an empty list. - If the subject is not a named entity, return an empty list. - Include at least one triple where predicate is "instanceOf". - Do not get too wordy. - Separate several objects into multiple triples with one object.
Subject: Himalayan Frontal Thrust Description of subject: The Himalayan Frontal Thrust is the youngest and most active major fault system along the southern front of the Himalayas, accommodating much of the ongoing convergence between the Indian and Eurasian tectonic plates.
Referenced by (2)
Full triples — surface form annotated when it differs from this entity's canonical label.