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Lothar Ratschbacher

Researcher at Freiberg University of Mining and Technology

Publications -  192
Citations -  13831

Lothar Ratschbacher is an academic researcher from Freiberg University of Mining and Technology. The author has contributed to research in topics: Foreland basin & Nappe. The author has an hindex of 57, co-authored 181 publications receiving 12198 citations. Previous affiliations of Lothar Ratschbacher include Stanford University & University of California, Berkeley.

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U/Pb zircon ages constrain the architecture of the ultrahigh-pressure Qinling–Dabie Orogen, China

TL;DR: In this article, new SHRIMP and TIMS zircon ages, 40Ar/39Ar ages, and eclogite locations contribute significantly to our understanding of the ultrahigh-pressure Dabie Shan.
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Tectonics of the Qinling (Central China): tectonostratigraphy, geochronology, and deformation history

TL;DR: The Qinling orogen preserves a record of late mid-Proterozoic to Cenozoic tectonism in central China as mentioned in this paper, where high pressure metamorphism and ophiolite emplacement assembled the Yangtze craton, including the lower Qinling unit, into Rodinia during the ∼1.0 Ga Grenvillian orogeny.
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Lateral extrusion in the eastern Alps, PArt 2: Structural analysis

TL;DR: In this article, a model for lateral extrusion in the Eastern Alps has been proposed and the kinematics of this process are approximated by an extrusion-spreading model proposed for nappe tectonics.
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Exhumation of ultrahigh-pressure continental crust in east central China: Late Triassic-Early Jurassic tectonic unroofing

TL;DR: The largest tract of ultrahigh pressure rocks, the Dabie-Hong'an area of China, was exhumed from 125 km depth by a combination of normal-sense shear from beneath the hanging wall Sino-Korean craton, southeastward thrusting onto the footwall Yangtze craton and orogen-parallel eastward extrusion as discussed by the authors.
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Distributed deformation in southern and western Tibet during and after the India-Asia collision

TL;DR: In this paper, the authors used field and radiometric data to describe and date strain and stress states in southern (longitude 88 o to 91oE, latitude 28 o to 30oN) and western Tibet (longitudes 79 o to 82oE and latitude 30 o to 34oN).