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• W2080878082 abstract "In Indian plate rocks defining the footwall of the Indo-Asian suture in the Upper Kaghan Valley (UKV) of northern Pakistan, we resolve four phases in a continuum of Himalayan metamorphism and deformation, with peak metamorphic pressures of 7.2 ± 0.7 kbar and a minimum estimate for peak temperature of approximately 540°C. To attach an absolute age to Himalayan metamorphism, we used the SHRIMP ion microprobe to obtain U-Pb ages on the rims of zircons from granites metamorphosed during the earliest phase of Himalayan orogeny. Four granite samples give a mean U-Pb age of 47 ± 3 Ma. Zircons from the Malakand Granite of the Swat region (200 km west of the UKV) have rims that also give a mean U-Pb age of 47 ± 3 Ma. Cores of these zircons yield U-Pb ages of 254-291 Ma which approach the previously published Rb/Sr isochron age of 297 ± 4 Ma for the Peshawar Plain Igneous Province, suggesting an expanded areal extent of this Carboniferous igneous suite. The metamorphic ages of 47 ± 3 Ma document that the thermal culmination of Himalayan metamorphism must have developed within, at most, only a few million years following Indo-Asian collision, commonly dated at 50 Ma, or that the continental crust of the Indian plate was undergoing thickening well before 50 Ma. We favor the latter, viewing our data as corroborating previous suggestions that initial contact between India and Asia was established in the NW Himalaya by 65 Ma." @default.
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• W2080878082 date "1994-09-01" @default.
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• W2080878082 title "Timing and Duration of Himalayan Metamorphism within the Indian Plate, Northwest Himalaya, Pakistan" @default.
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• W2080878082 doi "https://doi.org/10.1086/629694" @default.
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