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- W2606553552 abstract "The Bukhara-Khiva region forms the northern margin of the Mesozoic Amu-DaryaBasin. We reconstructed several cross-sections across this margin from subsurface data. The objectivesincluded examining the structure of the Bukhara and Chardzhou steps and determining thetectonic–sedimentary evolution of the basin during the Jurassic. Subsequent to the Cimmerian collisionin the Middle Triassic, an extensional event controlled the deposition of the Early–MiddleJurassic siliciclastic succession in the Bukhara-Khiva region. The main Late Palaeozoic inheritedstructures were reactivated as normal faults during this period. Continental coarse-grained siliciclasticsediments are mainly confined to the basal Lower Jurassic section, probably Pliensbachian–Toarcian in age, whereas marine siliciclastic sediments occur in the early Late Bajocian.In the Early–Middle Jurassic the Bukhara and Chardzhou steps were predominantly sourced byareas of relief, the remains of Late Palaeozoic orogens located to the north. The rate of extensionsignificantly declined during the Middle Callovian–Kimmeridgian period. Deposition of the overlyingLower Cretaceous continental red-coloured clastic sediments was related to the interactionof basin subsidence, a fall in eustatic sea-level and sediment supply. Subsequent marine transgressionin the Late Barremian, partially related to broad thermal subsidence in the Amu-DaryaBasin, resulted in the deposition of an extensive Late Cretaceous clay–marl succession." @default.
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- W2606553552 date "2017-01-01" @default.
- W2606553552 modified "2023-09-26" @default.
- W2606553552 title "Structure and evolution of the Bukhara-Khiva region during the Mesozoic: the northern margin of the Amu-Darya Basin (southern Uzbekistan)" @default.
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- W2606553552 doi "https://doi.org/10.1144/sp427.16" @default.
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