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.

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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

Referenced by (1)

Full triples — surface form annotated when it differs from this entity's canonical label.

Main Central Thrust zone relatedTo South Tibetan Detachment System