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• W2048442541 abstract "Mesozoic deep-water sedimentary and basic volcanogenic rocks, defined as the Karamba Complex, are exposed within the Indus suture zone of Western Ladakh (N India). The Karamba Complex originated as part of the North-Indian passive margin in its entirety, and does not include exotic melange or accreted oceanic units, as recently suggested. The complex preserves younger, more distal equivalents relative to more proximal deep-water slope (Lamayuru Complex) and shelf (Zanskar) successions of the North-Indian passive margin. The Karamba Complex is mainly inverted, youngs to the NNW, and includes many outcrop-scale folds that face NNW. The Complex was initially emplaced onto the Zanskar Shelf as three main thrust slices probably in the latest Cretaceous, and later inverted, faulted and sheared during mid–late Tertiary NW backthrusting that accompanied uplift of the High Himalaya. Sedimentation in the Karamba Complex began in the Mid–Late Triassic, with mainly siliciclastic turbidites derived from the Indian basement, together with redeposited limestones and minor basic volcanics. Mixed radiolarian sediments, siliciclastic turbidites and redeposited shelf-derived calciturbidites accumulated in Early–Mid Jurassic, accompanied by eruption of alkaline volcanic rocks, mainly in the Mid Jurassic. The probable cause of the Jurassic volcanism was a pulse of crustal extension along the continent–ocean transition zone, triggered by late-stage rifting of India from Gondwana, as a precursor to its northward drift. Quartzose sandstone turbidites accumulated on the upper slope in the Early Cretaceous, whereas sedimentation on the lower slope/rise was pelagic, marked by depositional hiatuses and sediment redeposition. During the Late Cretaceous a switch to mainly calcareous pelagic deposition took place, interspersed with radiolarian accumulation on the lower slope/rise. Initial thrust emplacement onto the Zanskar Shelf in the latest Cretaceous is suggested by the absence of post-Upper Cretaceous sediments within the Karamba Complex." @default.
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• W2048442541 title "Mesozoic deep-water slope/rise sedimentation and volcanism along the North-Indian passive margin: evidence from the Karamba Complex, Indus suture zone (Western Ladakh Himalaya)" @default.
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• W2048442541 doi "https://doi.org/10.1016/s0743-9547(98)00010-5" @default.
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