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(2015) Structural, geochronological and geochemical evidence for two distinct thrust sheets in the ‘Main Central thrust zone’, the Main Central thrust and Ramgarh–Munsiari thrust: implications for upper crustal shortening in central Nepal. Special Publication, 412. Geological Society of London. 221-245 doi:10.1144/sp412.2

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TitleStructural, geochronological and geochemical evidence for two distinct thrust sheets in the ‘Main Central thrust zone’, the Main Central thrust and Ramgarh–Munsiari thrust: implications for upper crustal shortening in central Nepal
ReportSpecial Publication
Year2015Volume412
PublisherGeological Society of London
DOIdoi:10.1144/sp412.2Search in ResearchGate
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Mindat Ref. ID440296Long-form Identifiermindat:1:5:440296:5
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Full Reference(2015) Structural, geochronological and geochemical evidence for two distinct thrust sheets in the ‘Main Central thrust zone’, the Main Central thrust and Ramgarh–Munsiari thrust: implications for upper crustal shortening in central Nepal. Special Publication, 412. Geological Society of London. 221-245 doi:10.1144/sp412.2
Plain Text(2015) Structural, geochronological and geochemical evidence for two distinct thrust sheets in the ‘Main Central thrust zone’, the Main Central thrust and Ramgarh–Munsiari thrust: implications for upper crustal shortening in central Nepal. Special Publication, 412. Geological Society of London. 221-245 doi:10.1144/sp412.2
InMukherjee, S.; Carosi, R.; Beek, P.A. van der; Mukherjee, B.K.; Robinson, D.M. - Eds. (2015) Tectonics of the Himalaya. Special Publication Vol. 412. Geological Society of London

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(2006) Exhumation of Greater Himalayan rock along the Main Central Thrust in Nepal: implications for channel flow. Special Publication, 268. Geological Society of London. 255-267 doi:10.1144/gsl.sp.2006.268.01.12
(1993) Deformation and metamorphism within the Main Central Thrust zone, Arun Tectonic Window, eastern Nepal. Special Publication, 74. Geological Society of London. 511-523 doi:10.1144/gsl.sp.1993.074.01.34
(2013) Sedimentary and structural evidence for two-phase Upper Cretaceous and Eocene emplacement of the Tauride thrust sheets in central southern Turkey. Special Publication, 372. Geological Society of London. 299-322 doi:10.1144/sp372.2
(2015) Redefining the tectonostratigraphic and structural architecture of the Almora klippe and the Ramgarh–Munsiari thrust sheet in NW India. Special Publication, 412. Geological Society of London. 247-269 doi:10.1144/sp412.6
(2019) Dating protracted fault activities: microstructures, microchemistry and geochronology of the Vaikrita Thrust, Main Central Thrust zone, Garhwal Himalaya, NW India. Special Publication, 481. Geological Society of London. 127-146 doi:10.1144/sp481.3
(1993) A study of illite crystallinity and fluid inclusions in the Kathmandu Klippe and the Main Central Thrust zone, Nepal. Special Publication, 74. Geological Society of London. 525-540 doi:10.1144/gsl.sp.1993.074.01.35
(2015) Quaternary shortening at the orogenic front of the Central Andes of Argentina: the Las Peñas Thrust System. Special Publication, 399. Geological Society of London. 245-266 doi:10.1144/sp399.5
(1993) Pressure, temperature and time constraints on metamorphism across the Main Central Thrust zone and High Himalayan Slab in the Garhwal Himalaya. Special Publication, 74. Geological Society of London. 485-509 doi:10.1144/gsl.sp.1993.074.01.33
(2019) A new occurrence of lazulite from the Main Central Thrust in Kumaun Himalaya, India: fluid inclusion, EPMA and Raman spectroscopy focusing on lazulite in a highly tectonized zone. Special Publication, 481. Geological Society of London. 211-230 doi:10.1144/sp481-2018-117
(1993) The Main Boundary Thrust and propagation of deformation into the foreland fold-and-thrust belt in northern Pakistan near the Indus River. Special Publication, 74. Geological Society of London. 581-588 doi:10.1144/gsl.sp.1993.074.01.38
(2000) The Main Mantle Thrust in Pakistan: its character and extent. Special Publication, 170. Geological Society of London. 375-393 doi:10.1144/gsl.sp.2000.170.01.20
 
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