Domal structures and high‐grade metamorphism in the Higher Himalayan Crystalline, Zanskar Region, north‐west Himalaya, India

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Abstract
In the main Himalayan range in the Ladakh‐Zanskar area, domal structures have been observed at structurally deeper levels in the tectonic unit of the Higher Himalayan Crystalline. Their formation occurred during a second, temperature‐dominated phase (M2) of high‐grade regional metamorphism, characterized by the semipelitic paragenesis of sillimanite‐K‐feldspar and incipient anatexis. The doming event reveals a local system of synmetamorphic uplift superimposed on a regional system of northeast‐southwest trending compression. In the main Himalayan range the development of the dominant S2 foliation is related to deformation during the doming phase, which started early in the M2 event. The deformation propagated continuously north‐east and south‐west with time. In the north‐east, on the northern slopes of the main Himalayan range, this deformation is expressed by extensional shear movements of the upper tectonic levels finally leading to the late‐ to postmetamorphic normal fault system of the Zanskar shear zone. Towards the south‐west, deformation is expressed by compressional movements, e.g. at the Main Central Thrust (MCT) in the Kishtwar window area. The observed compression and extension is inferred to relate to an increased uplift of the domal bulges of the tectonic Kishtwar window and of the whole main Himalayan range.