Pliocene episodic exhumation and the significance of the Munsiari thrust in the northwestern Himalaya
Autor: | Rasmus Thiede, István Dunkl, Djordje Grujic, Konstanze Stübner, Patricia Eugster |
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Rok vydání: | 2018 |
Předmět: |
010504 meteorology & atmospheric sciences
Window (geology) Institut für Umweltwissenschaften und Geographie 010502 geochemistry & geophysics 01 natural sciences Thermochronology Paleontology Tectonics Geophysics Space and Planetary Science Geochemistry and Petrology Main Central Thrust ddc:550 Earth and Planetary Sciences (miscellaneous) Thrust fault Shear zone Accretion (geology) Geomorphology Geology 0105 earth and related environmental sciences Zircon |
Zdroj: | Earth and Planetary Science Letters. 481:273-283 |
ISSN: | 0012-821X |
DOI: | 10.1016/j.epsl.2017.10.036 |
Popis: | The Himalayan thrust belt comprises three in-sequence foreland-propagating orogen-scale faults, the Main Central thrust, the Main Boundary thrust, and the Main Frontal thrust. Recently, the Munsiari–Ramgarh–Shumar thrust system has been recognized as an additional, potentially orogen-scale shear zone in the proximal footwall of the Main Central thrust. The timing of the Munsiari, Ramgarh, and Shumar thrusts and their role in Himalayan tectonics are disputed. We present 31 new zircon (U–Th)/He ages from a profile across the central Himachal Himalaya in the Beas River area. Within a ∼40 km wide belt northeast of the Kullu–Larji–Rampur window, ages ranging from to constrain a distinct episode of rapid Pliocene to Present exhumation; north and south of this belt, zircon (U–Th)/He ages are older ( to ). We attribute the Pliocene rapid exhumation episode to basal accretion to the Himalayan thrust belt and duplex formation in the Lesser Himalayan sequence including initiation of the Munsiari thrust. Pecube thermokinematic modelling suggests exhumation rates of ∼2–3 mm/yr from 4–7 to 0 Ma above the duplex contrasting with lower ( |
Databáze: | OpenAIRE |
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