References
Aitchison JC, Ali JR, Davis AM (2007) When and where did India and Asia collide? J Geophys Res 112:1–19. doi:10.1029/2006JB004706
Chappell BW, White AJR (1974) Two contrasting granite types. Pac Geol 8:173–174
Chappell B, White A (1992) I-and S-type granites in the Lachlan Fold Belt. Trans R Soc Edinb Earth Sci 83:1–26
Chappell B, White A (2001) Two contrasting granite types: 25 years later. Aust J Earth Sci 48:489–499
Collins WJ (2002) Hot orogens, tectonic switching, and creation of continental crust. Geology 30:535–538
Collins WJ, Richards S (2008) Geodynamic significance of S-type granites in circum-Pacific orogens. Geology 36:559
Forster MA, White LT, Ahmad T (2011) Thermal history of a pebble in the Indus Molasse at the margin of a Himalayan metamorphic core complex. J Virtual Explor 38:1–21. doi:10.3809/jvirtex.2011.00267
Ickert RB, Williams IS (2011) U-Pb zircon geochronology of Silurian–Devonian granites in southeastern Australia: implications for the timing of the Benambran Orogeny and the I–S dichotomy. Aust J Earth Sci 58:501–516. doi:10.1080/08120099.2011.562922
Lister G, Forster MA (2009) Tectonic mode switches and the nature of orogenesis. Lithos 113:274–291
Paterson SR, Fowler TK Jr, Schmidt KL et al (1998) Interpreting magmatic fabric patterns in plutons. Lithos 44:53–82
Raz U, Honegger K (1989) Magmatic and tectonic evolution of the Ladakh block from field studies. Tectonophysics 161:107–118
Rolland Y, Picard C, Pecher A, Lapierre H (2002) The cretaceous Ladakh arc of NW Himalaya—slab melting and melt–mantle interaction during fast northward drift of Indian plate. Chem Geol 182:139–178
Searle M, Windley B, Coward M (1987) The closing of Tethys and the tectonics of the Himalaya. Geol Soc Am Bull 98:678–701
Searle MP, Cooper D, Rex AJ et al (1988) Collision Tectonics of the Ladakh–Zanskar Himalaya [and discussion]. Philos Trans R Soc London A 326:117–150
Sen K, Collins AS (2012) Dextral transpression and late Eocene magmatism in the trans-Himalayan Ladakh Batholith (North India): implications for tectono-magmatic evolution of the Indo-Eurasian collisional arc. Int J Earth Sci (Geol Rundsch). doi:10.1007/s00531-012-0826-8
Sen K, Mukherjee BK, Sachan HK (2009) Field and microstructural analysis of the Pangong Granodiorite, Ladakh (NW India): implications for tectonics along the Karakoram Fault Zone. Curr Sci 96:1124–1130
St-Onge MR, Rayner N, Searle MP (2010) Zircon age determinations for the Ladakh batholith at Chumathang (Northwest India): implications for the age of the India–Asia collision in the Ladakh Himalaya. Tectonophysics 495:1–13. doi:10.1016/j.tecto.2010.09.010
Weinberg RF, Dunlap W (2000) Growth and deformation of the Ladakh Batholith, Northwest Himalayas: implications for timing of continental collision and origin of calc-alkaline batholiths. J Geol 108:303–320
White LT, Ahmad T, Ireland TR et al (2011) Deconvolving episodic age spectra from zircons of the Ladakh Batholith, northwest Indian Himalaya. Chem Geol 289:179–196. doi:10.1016/j.chemgeo.2011.07.024
White LT, Ahmad T, Lister GS et al (2012) Is the switch from I- to S-type magmatism in the Himalayan Orogen indicative of the collision of India and Eurasia? Aust J Earth Sci 59:321–340. doi:10.1080/08120099.2012.652670
Acknowledgments
L. White is financially supported by the SE Asia Research Group through funding provided by a consortium of oil companies. M. Forster acknowledges the support of an Australian Research Fellowship provided by the Australian Research Council.
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White, L.T., Lister, G.S., Ahmad, T. et al. Comment on “Dextral transpression and late-Eocene magmatism in the trans-Himalayan Ladakh Batholith (North India): implications for tectono-magmatic evolution of the Indo-Eurasian collisional arc”. Int J Earth Sci (Geol Rundsch) 102, 969–972 (2013). https://doi.org/10.1007/s00531-013-0862-z
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DOI: https://doi.org/10.1007/s00531-013-0862-z