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Arne P. Willner

Researcher at Ruhr University Bochum

Publications -  74
Citations -  3051

Arne P. Willner is an academic researcher from Ruhr University Bochum. The author has contributed to research in topics: Metamorphic rock & Metamorphism. The author has an hindex of 31, co-authored 71 publications receiving 2732 citations. Previous affiliations of Arne P. Willner include University of Stuttgart & Shandong University of Science and Technology.

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Time of formation and peak of Variscan HP-HT metamorphism of quartz-feldspar rocks in the central Erzgebirge, Saxony, Germany

TL;DR: The Gneiss-Eclogite Unit (GEU) is a composite tectonometamorphic assemblage characterized by a HP-HT imprint and comprises migmatitic para-and orthogneisses, HT mylonites, HP granulites, eclogites and garnet peridotites as discussed by the authors.
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History of crustal growth and recycling at the Pacific convergent margin of South America at latitudes 29°–36° S revealed by a U–Pb and Lu–Hf isotope study of detrital zircon from late Paleozoic accretionary systems

TL;DR: In this paper, a combined laser ablation ICP-MS U-Pb and Lu-Hf analysis of homogeneous growth domains in detrital zircon from late Paleozoic coastal accretionary systems in central Chile and the collisional Guarguaraz Complex in W Argentina was conducted.
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Physical controls of magmatic productivity at Pacific-type convergent margins: Numerical modelling

TL;DR: In this article, a coupled petrological-thermomechanical model of subduction with spontaneous slab bending is used to investigate magmatic productivity at active continental margins, and the model is designed to simulate fossil Pacific-type margins that have a broad well-developed forearc accretionary wedge system.
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Arc–continent collision in the Southern Urals

TL;DR: The Southern Urals of Russia contain what is arguably one of the best-preserved examples of an arc-continent collision in any Paleozoic orogen as discussed by the authors, which led to the development of an accretionary complex that includes shallowly and deeply subducted continental margin rocks, ophiolite fragments and sediments that were deposited in a foreland-basin setting.
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Time markers for the evolution and exhumation history of a Late Palaeozoic paired metamorphic belt in North-Central Chile (34°-35°30′S)

TL;DR: In this paper, a multi-method geochronological approach is applied to unravel the dynamics of a paired metamorphic belt in the Coastal Cordillera of central Chile, represented by high-pressure -low-temperature rocks of an accretionary prism (Western Series), and a low-pressure-hightemperature overprint in the retro-wedge with less deformed metagreywackes (Eastern Series) intruded by magmas of the coeval arc.