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Tectonometamorphic discontinuities in the Greater Himalayan Sequence: a local or a regional feature?

Chiara Montomoli, Rodolfo Carosi and Salvatore Iaccarino
Geological Society, London, Special Publications, 412, 25-41, 18 September 2015, https://doi.org/10.1144/SP412.3
Chiara Montomoli
1Dipartimento di Scienze della Terra, Università di Pisa, v. S. Maria, 53 56126 Pisa, Italy
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Rodolfo Carosi
2Dipartimento di Scienze della Terra, Università di Torino, v. Valperga Caluso, 35 10125 Torino, Italy
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Salvatore Iaccarino
1Dipartimento di Scienze della Terra, Università di Pisa, v. S. Maria, 53 56126 Pisa, Italy
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Abstract

The Greater Himalayan Sequence (GHS) is one of the major tectonic units of the Himalaya running for more than 2400 km along-strike. It has been considered as a coherent tectonic unit bound by the South Tibetan Detachment (STD) and the Main Central Thrust (MCT). However, thrusts within it have been recognized in several places and have been mainly interpreted as out-of-sequence thrusts being active after the main phase of exhumation of the crystalline unit after the MCT activated. Recent integrated studies allow the recognition of several ductile shear zones in the core of the GHS, with top-to-the-SW-sense of shear (Higher Himalayan Discontinuity (HHD)). U–Th–Pb in situ monazite ages provide ages older than the MCT. Data on pressure and temperature evolution testify that these shear zones affected the tectonometamorphic evolution of the belt and different pressure and temperature conditions were recorded in the hanging wall and footwall of the HHD. The correlation of the WNW–ESE-trending HHD with other discontinuities recognized in the GHS led to the proposal that it is a tectonic feature running for several hundred kilometres, documented at the regional scale dividing the GHS in two different portions.

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Geological Society, London, Special Publications: 412 (1)
Geological Society, London, Special Publications
Volume 412
2015
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Tectonometamorphic discontinuities in the Greater Himalayan Sequence: a local or a regional feature?

Chiara Montomoli, Rodolfo Carosi and Salvatore Iaccarino
Geological Society, London, Special Publications, 412, 25-41, 18 September 2015, https://doi.org/10.1144/SP412.3
Chiara Montomoli
1Dipartimento di Scienze della Terra, Università di Pisa, v. S. Maria, 53 56126 Pisa, Italy
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  • For correspondence: [email protected]
Rodolfo Carosi
2Dipartimento di Scienze della Terra, Università di Torino, v. Valperga Caluso, 35 10125 Torino, Italy
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Salvatore Iaccarino
1Dipartimento di Scienze della Terra, Università di Pisa, v. S. Maria, 53 56126 Pisa, Italy
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Tectonometamorphic discontinuities in the Greater Himalayan Sequence: a local or a regional feature?

Chiara Montomoli, Rodolfo Carosi and Salvatore Iaccarino
Geological Society, London, Special Publications, 412, 25-41, 18 September 2015, https://doi.org/10.1144/SP412.3
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  • Article
    • Abstract
    • Geological setting
    • Discontinuities in the GHS
    • Tectonic and metamorphic discontinuities (P–T–t–D discontinuities)
    • Discussion
    • HHD and metamorphism in the GHS
    • Conclusion
    • Acknowledgments
    • References
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