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• W144183078 abstract "We report new structural descriptions and measurements carried out across the onshore Makran Accretionary Wedge, in SE Iran. Complementary geological mapping led to the identification of four main tectono-stratigraphic units separated by major thrust zones. From the north to the south, i.e. from top to bottom, these major thrust sheets are called North-, Inner-, Outer- and Coastal-Makran. The Bashakerd Thrust that emplaced North on Inner Makran separates two geologically different domains. North Makran includes ophiolites obducted in Late Cretaceous to Paleogene times and a tectonic assemblage of Cretaceous to Paleogene? deep-sea sediments and volcanics, the so-called “Coloured Mélange”, whereas from Inner Makran to the South, a Miocene to Recent fold-and-thrust belt constitutes the upper part of the Makran Accretionary Wedge. Inner and Outer Makran began to form before the catastrophic emplacement of a Tortonian olistostrome. Folding accompanying thrusting pertains to a continuous history that, however, was not evenly distributed in terms of location and amplification rates of individual folds, yet developed altogether in Middle Miocene to Pliocene times. Most of the deformation was shifted after emplacement of the olistostrome to the present-day submarine wedge, and Coastal Makran evolved into a wedge-top basin with shallower water and continental sedimentation. The juxtaposition of two wedges of different age makes it difficult to average the surface slope and to conclude that Makran is a mature wedge with one of the lowest taper angles, worldwide. Owing to internal strain and syn-sedimentary tectonic processes, it is likely that the Makran maintained an equilibrium triangular cross-sectional shape to grow into a larger similar wedge." @default.
• W144183078 created "2016-06-24" @default.
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• W144183078 date "2012-09-14" @default.
• W144183078 modified "2023-10-07" @default.
• W144183078 title "structural style of the Makran Tertiary accretionary complex in SE-Iran" @default.
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• W144183078 doi "https://doi.org/10.1007/978-3-642-30609-9_12" @default.
• W144183078 hasPublicationYear "2012" @default.
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