B. Schulte
Darmstadt University of Applied Sciences
9 Papers
82 Citations
B. Schulte is an academic researcher from Darmstadt University of Applied Sciences. The author has contributed to research in topics: Metamorphism & Shear zone. The author has an hindex of 6, co-authored 8 publications.
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Papers
Subduction- and exhumation-related fabrics in the Paleozoic high-pressure–low-temperature Maksyutov Complex, Antingan area, southern Urals, Russia
TL;DR: In this paper, structural and petrologic data from a cross section through the high-pressure-low-temperature Maksyutov Complex was used to develop a new model for its tectonometamorphic evolution.
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From passive margin to volcano-sedimentary forearc: the Tonian to Cryogenian evolution of the Anosyen Domain of southeastern Madagascar
TL;DR: In this paper, the Iakora and Horombe groups of the Anosyen Domain of southeastern Madagascar have been investigated and it was shown that the sedimentary and volcanic rocks of the IAKORA and HOROMBE groups contain predominantly 2400-1600-Ma aged detrital zircon with a modal age peak at approximately 1850-Ma.
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Proterozoic magmatic and tectonometamorphic evolution of the Taratash complex, Central Urals, Russia
TL;DR: The Taratash Complex (TC) as mentioned in this paper is a pre-Uralian polymetamorphic complex along the eastern margin of the East European Craton, which experienced granulite facies peak metamorphic conditions (850-900°C/10kbar).
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Monazite stability, composition and geochronology as tracers of Paleoproterozoic events at the eastern margin of the East European Craton (Taratash complex, Middle Urals)
TL;DR: In this paper, the ages of monazite from intensively deformed rocks within a major amphibolite-facies shear zone in the Taratash complex has been investigated by means of electron-probe microanalysis and laser-ablation SF-ICP-MS.
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The tectonic domains of southern and western Madagascar
S. D. Boger,Roland Maas,M. Pastuhov,P H Macey,W. Hirdes,B. Schulte,Christopher Fanning,C.A.M. Ferreira,T. Jenett,R. Dallwig +9 more
TL;DR: In this paper, the Androyen and Anosyen domains are linked to the western side of the Mozambique Ocean by the Beraketa high-strain zone.
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