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• W4384927467 abstract "Abstract The NNW Iranian Plateau and west Alborz within the Arabia‐Eurasia collision zone are characterized by three main tectono‐stratigraphic zones, crosscut by the Qezel‐Owzan River (QOR) Basin. The interplay between present‐day deformation and climate, which control the landscape evolution of the region, is still poorly constrained. We addressed this gap by measuring millennial‐scale erosion rates from 10 Be‐concentration in the QOR sands along with topographic/climatic metrics analyses. Results reveal low erosion rates in the Plateau and relatively high in the west Alborz. The regional consistency of topographic parameters with geomorphology suggests that they control sediment fluxes in the Plateau, while the surface uplift, active thrust‐faulting, and shallow crustal seismicity in the west Alborz are the main controlling factors. Climate has a secondary role on erosion rates. Furthermore, we calculated exhumation rates from published thermochronometric AFT/AHe ages to determine their relationship with 10 Be short‐term data. Results imply that the exhumation rates increased slightly in the Plateau and west Alborz from ∼26 to ∼10 Ma, simultaneous with hard collision processes between the Arabia‐Eurasia. This trend accelerated from ∼10 to ∼2.8 Ma due to the isolation of the Caspian Sea and extreme base‐level fall. From ∼2.8 to ∼2 Ma, base‐level rise occurred under climate influence, and erosion rates decreased. Millennial‐scale data show the erosion rate decreased from ∼2 Ma to the Present‐day, which is attributed to the change in deformation style and fault kinematics from fold/thrusting to mainly strike‐slip faulting. The significantly lower erosion rates in the Plateau compared to west Alborz suggest a relatively stable plateau surface." @default.
• W4384927467 created "2023-07-22" @default.
• W4384927467 creator A5015236502 @default.
• W4384927467 creator A5023255987 @default.
• W4384927467 creator A5034068742 @default.
• W4384927467 creator A5040408630 @default.
• W4384927467 creator A5051916488 @default.
• W4384927467 date "2023-07-29" @default.
• W4384927467 modified "2023-10-14" @default.
• W4384927467 title "Tectonics, Base‐Level Fluctuations, and Climate Impact on the Eocene to Present‐Day Erosional Pattern of the Arabia‐Eurasia Collision Zone (NNW Iranian Plateau and West Alborz Mountains)" @default.
• W4384927467 cites W1504827285 @default.
• W4384927467 cites W1518550229 @default.
• W4384927467 cites W1531354667 @default.
• W4384927467 cites W1602192732 @default.
• W4384927467 cites W1622026908 @default.
• W4384927467 cites W1641647539 @default.
• W4384927467 cites W1664416090 @default.
• W4384927467 cites W1730466325 @default.
• W4384927467 cites W1780510282 @default.
• W4384927467 cites W1799723375 @default.
• W4384927467 cites W1909972016 @default.
• W4384927467 cites W1911637049 @default.
• W4384927467 cites W1918485811 @default.
• W4384927467 cites W1930936663 @default.
• W4384927467 cites W1969157568 @default.
• W4384927467 cites W1973364186 @default.
• W4384927467 cites W1975350041 @default.
• W4384927467 cites W1977260961 @default.
• W4384927467 cites W1978776740 @default.
• W4384927467 cites W1979414112 @default.
• W4384927467 cites W1981035482 @default.
• W4384927467 cites W1984126050 @default.
• W4384927467 cites W1985374532 @default.
• W4384927467 cites W1986860125 @default.
• W4384927467 cites W1987169966 @default.
• W4384927467 cites W1990633455 @default.
• W4384927467 cites W1991220051 @default.
• W4384927467 cites W1991811150 @default.
• W4384927467 cites W1991913409 @default.
• W4384927467 cites W1993744042 @default.
• W4384927467 cites W1995543833 @default.
• W4384927467 cites W1997255700 @default.
• W4384927467 cites W2002532823 @default.
• W4384927467 cites W2003243667 @default.
• W4384927467 cites W2003599747 @default.
• W4384927467 cites W2005035365 @default.
• W4384927467 cites W2005596384 @default.
• W4384927467 cites W2007567695 @default.
• W4384927467 cites W2011948344 @default.
• W4384927467 cites W2018265973 @default.
• W4384927467 cites W2023091835 @default.
• W4384927467 cites W2026871562 @default.
• W4384927467 cites W2031192009 @default.
• W4384927467 cites W2031340793 @default.
• W4384927467 cites W2033345860 @default.
• W4384927467 cites W2035097336 @default.
• W4384927467 cites W203584942 @default.
• W4384927467 cites W2037781695 @default.
• W4384927467 cites W2038087606 @default.
• W4384927467 cites W2038519446 @default.
• W4384927467 cites W2038947148 @default.
• W4384927467 cites W2039550923 @default.
• W4384927467 cites W2039682763 @default.
• W4384927467 cites W2043119271 @default.
• W4384927467 cites W2044851583 @default.
• W4384927467 cites W2045175855 @default.
• W4384927467 cites W2051693561 @default.
• W4384927467 cites W2053151969 @default.
• W4384927467 cites W2053381713 @default.
• W4384927467 cites W2054340203 @default.
• W4384927467 cites W2054350901 @default.
• W4384927467 cites W2060140824 @default.
• W4384927467 cites W2062290164 @default.
• W4384927467 cites W2063522637 @default.
• W4384927467 cites W2064841659 @default.
• W4384927467 cites W2065123927 @default.
• W4384927467 cites W2075151941 @default.
• W4384927467 cites W2088171171 @default.
• W4384927467 cites W2089462565 @default.
• W4384927467 cites W2092352873 @default.
• W4384927467 cites W2093905602 @default.
• W4384927467 cites W2093931182 @default.
• W4384927467 cites W2093962246 @default.
• W4384927467 cites W2094546888 @default.
• W4384927467 cites W2094909528 @default.
• W4384927467 cites W2096773693 @default.
• W4384927467 cites W2100057200 @default.
• W4384927467 cites W2102250984 @default.
• W4384927467 cites W2104300819 @default.
• W4384927467 cites W2104837834 @default.
• W4384927467 cites W2106081716 @default.
• W4384927467 cites W2107567801 @default.
• W4384927467 cites W2108026051 @default.
• W4384927467 cites W2108399175 @default.
• W4384927467 cites W2109567422 @default.
• W4384927467 cites W2110209344 @default.
• W4384927467 cites W2112776483 @default.
• W4384927467 cites W2113162852 @default.
• W4384927467 cites W2114057995 @default.
• W4384927467 cites W2117031136 @default.

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