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Masafumi Sudo

Researcher at University of Potsdam

Publications -  74
Citations -  3064

Masafumi Sudo is an academic researcher from University of Potsdam. The author has contributed to research in topics: Metamorphism & Metamorphic rock. The author has an hindex of 27, co-authored 71 publications receiving 2545 citations. Previous affiliations of Masafumi Sudo include Kyoto University & Kobe University.

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The characteristics and chronology of the earliest Acheulean at Konso, Ethiopia

TL;DR: A newly established chronometric calibration is provided for the Acheulean assemblages of the Konso Formation, southern Ethiopia, which span the time period ∼1.75 to <1.0 Ma, paralleling the emergence of Homo erectus-like hominid morphology.
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Arabia-Eurasia continental collision: Insights from late Tertiary foreland-basin evolution in the Alborz Mountains, northern Iran

TL;DR: A poorly understood lag time between the initial Arabia-Eurasia continental collision in late Eocene to early Oligocene time and the acceleration of tectonic and sedimentary processes across the collision zone in the early to late Miocene is described in this article.

Arabia-Eurasia continental collision: insights from late Tertiary foreland-basin evolution in the Alborz mountains, northern Iran.

TL;DR: A poorly understood lag time between the initial Arabia-Eurasia continental collision in late Eocene to early Oligocene time and the acceleration of tectonic and sedimentary processes across the collision zone in the early to late Miocene is described in this article.
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Late Miocene-Pliocene deceleration of dextral slip between Pamir and Tarim: Implications for Pamir orogenesis

TL;DR: In this paper, the authors used thermochronologic data collected along the eastward-flowing, deeply incised, antecedent Tashkorgan-Yarkand River, which crosses the fault system on the eastern flank of the orogen.
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Oceanic-style subduction controls late Cenozoic deformation of the Northern Pamir orogen

TL;DR: In this paper, the authors demonstrate that the observed deformation of the upper and lower plates within the Pamir-Alai convergence zone resembles highly arcuate oceanic subduction systems characterized by slab rollback, subduction erosion, subduct accretion, and marginal slab-tear faults.