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• W4313252488 abstract "The late Cenozoic tectonic evolution of the east-central Alborz Mountains in northern Iran has been well recorded in the Chashm Sub-basin. The depositional setting of this sub-basin has changed from a marine to a shallow marine-lagoon by the late Oligocene likely as a result of the far-field effects of the onset of the Arabia-Eurasia collision. Since the recent findings suggest that the collision might have initiated long later, the diachronous initiation of the collision are proposed. In the Miocene time, the sedimentary environment changed to a continental setting possibly due to less known stages of the Arabia-Eurasian collision, represented by the deposition of the red thick clastic sediments. The middle-upper Miocene deposits characterize the intermontane basins that generally developed in the Alborz Mountains at this time and continued in the Pliocene and Quaternary. The detrital materials were provided for the Chashm Sub-basin due to the uplift of nearby elevated areas that are the hanging wall blocks of the Chashm and Bashm faults. The Miocene and younger deposits have also undergone folding and faulting, and provide evidence for a significant change in the kinematic regime from a Miocene right-lateral to the present-day left-lateral transpressive regime in the east-central Alborz Mountains. We suggest that vertical-axis rotations of the Alborz Mountains arms can simply explain the late Cenozoic kinematic changes observed in this range without the shortening direction associated with the Arabia-Eurasia collision being necessarily changed." @default.
• W4313252488 created "2023-01-06" @default.
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• W4313252488 date "2023-03-01" @default.
• W4313252488 modified "2023-10-18" @default.
• W4313252488 title "Depositional and structural characteristics of the Chashm Sub-basin; implications for the late Cenozoic tectonic evolution of the east-central Alborz Mountains, northern Iran" @default.
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• W4313252488 doi "https://doi.org/10.1016/j.jseaes.2022.105519" @default.
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