South Tibetan Detachment System
E753964
The South Tibetan Detachment System is a major normal fault system in the Himalaya that accommodated crustal extension and exhumation of high-grade metamorphic rocks above the Main Central Thrust.
All labels observed (1)
| Label | Occurrences |
|---|---|
| South Tibetan Detachment System canonical | 1 |
How this entity was disambiguated
This entity first appeared as the object of triple T8716685 — 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: South Tibetan Detachment System Context triple: [Main Central Thrust zone, relatedTo, South Tibetan Detachment System]
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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.
southwestern Tibet
Southwestern Tibet is a high-altitude region of the Tibetan Plateau characterized by rugged Himalayan terrain, sparse population, and proximity to the borders with Nepal and India.
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C.
eastern Tibet
Eastern Tibet is a high-altitude region on the eastern Tibetan Plateau characterized by rugged mountains, deep river gorges, and a mix of Tibetan and neighboring cultural influences.
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D.
Tien Shan glacial system
The Tien Shan glacial system is an extensive network of mountain glaciers in the Tien Shan range of Central Asia, serving as a major freshwater reservoir for the surrounding arid regions.
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E.
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.
- F. None of above. chosen
- G. Unsure - the case is ambiguous/there is not enough information to decide.
Target entity: South Tibetan Detachment System Target entity description: The South Tibetan Detachment System is a major normal fault system in the Himalaya that accommodated crustal extension and exhumation of high-grade metamorphic rocks above the Main Central 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.
-
B.
southwestern Tibet
Southwestern Tibet is a high-altitude region of the Tibetan Plateau characterized by rugged Himalayan terrain, sparse population, and proximity to the borders with Nepal and India.
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C.
eastern Tibet
Eastern Tibet is a high-altitude region on the eastern Tibetan Plateau characterized by rugged mountains, deep river gorges, and a mix of Tibetan and neighboring cultural influences.
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D.
Tien Shan glacial system
The Tien Shan glacial system is an extensive network of mountain glaciers in the Tien Shan range of Central Asia, serving as a major freshwater reservoir for the surrounding arid regions.
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E.
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.
- F. None of above. chosen
Statements (42)
| Predicate | Object |
|---|---|
| instanceOf |
detachment fault
ⓘ
extensional fault system ⓘ geological structure ⓘ normal fault system ⓘ |
| accommodates |
crustal extension
ⓘ
exhumation of high-grade metamorphic rocks ⓘ |
| activeDuring | Miocene ⓘ |
| age | Cenozoic ⓘ |
| associatedProcess | channel flow of mid-crustal rocks ⓘ |
| associatedWith |
Himalayan orogeny
ⓘ
exhumation of Greater Himalayan Crystalline complex ⓘ syn-orogenic extension ⓘ |
| boundedBy |
Greater Himalayan Sequence
NERFINISHED
ⓘ
Tethyan Himalayan Sequence NERFINISHED ⓘ |
| controls | exhumation level of metamorphic core of Himalaya ⓘ |
| deformationStyle | brittle-ductile ⓘ |
| dipDirection | north-dipping ⓘ |
| extendsAcross |
Bhutan Himalaya
NERFINISHED
ⓘ
Indian Himalaya NERFINISHED ⓘ Nepal Himalaya NERFINISHED ⓘ southern Tibet NERFINISHED ⓘ |
| formsBoundaryBetween | upper crustal sedimentary rocks and mid-crustal metamorphic rocks ⓘ |
| formsPartOf | Himalayan fault architecture ⓘ |
| hasAlternativeName |
South Tibetan Detachment
NERFINISHED
ⓘ
South Tibetan Detachment Fault System NERFINISHED ⓘ |
| kinematics |
top-to-the-north shear
ⓘ
top-to-the-northeast shear ⓘ |
| locatedIn |
Himalaya
NERFINISHED
ⓘ
Tibetan Plateau margin NERFINISHED ⓘ |
| mechanism | gravitational collapse of overthickened crust ⓘ |
| movementSense | normal faulting ⓘ |
| orientation | east–west striking ⓘ |
| overlies | Main Central Thrust NERFINISHED ⓘ |
| parallelTo | Main Central Thrust NERFINISHED ⓘ |
| relatedTo |
Main Central Thrust
NERFINISHED
ⓘ
North Himalayan domes NERFINISHED ⓘ |
| separates | Tethyan sedimentary sequence from Greater Himalayan Crystalline complex ⓘ |
| significance | major structure in Himalayan tectonic evolution ⓘ |
| studiedInDiscipline |
metamorphic geology
ⓘ
structural geology ⓘ tectonics ⓘ |
| tectonicSetting | collisional orogen ⓘ |
How these facts were elicited
The pipeline generated the facts above by prompting gpt-5.1 with this entity's name + description and the instruction below.
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: South Tibetan Detachment System Description of subject: The South Tibetan Detachment System is a major normal fault system in the Himalaya that accommodated crustal extension and exhumation of high-grade metamorphic rocks above the Main Central Thrust.
Referenced by (1)
Full triples — surface form annotated when it differs from this entity's canonical label.