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| | From intra-oceanic convergence to post-collisional evolution |
 | | It is dated at 75-65 Ma by plutonism developing along the Shyok Suture Zone, earlier in Kohistan (~ 75 Ma, Petterson and Windley, 1985), and later in eastern Ladakh (Tirit granite, 73.6-68 Ma; Weinberg and Dunlap, 2000; Weinberg et al., 2000). |
 | | The stages that directly preceded, or accompanied, the accretion, are coeval with intense magmatism, with emplacement of granodiorite to granite plutons along the Kohistan-Ladakh Batholith. |
 | | This late magmatism largely overprints the arc structure, being responsible for granulite-facies metamorphism in the central part of Ladakh (Raz and Honegger, 1989; Rolland et al., 2000) and amphibolite to epidote-amphibolite metamorphism along the northern suture (Hanson, 1989; Rolfo et al., 1997). |
| www.virtualexplorer.com.au /journal/2002/08/rolland/paper3.html (1453 words) |
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