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Reiner Klemd

Researcher at University of Erlangen-Nuremberg

Publications -  150
Citations -  7793

Reiner Klemd is an academic researcher from University of Erlangen-Nuremberg. The author has contributed to research in topics: Zircon & Metamorphism. The author has an hindex of 42, co-authored 128 publications receiving 6655 citations. Previous affiliations of Reiner Klemd include Rand Afrikaans University & Freiberg University of Mining and Technology.

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MPI-DING reference glasses for in situ microanalysis: New reference values for element concentrations and isotope ratios

Klaus Peter Jochum, +60 more
TL;DR: In this paper, the authors present new analytical data of major and trace elements for the geological MPI-DING glasses KL2-G, ML3B-G and ATHO-G.
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Tectonic evolution of the South Tianshan orogen and adjacent regions, NW China: geochemical and age constraints of granitoid rocks

TL;DR: In this article, the authors obtained geochemical and geochronological evidence from granitoids of the South Tianshan orogen and adjacent regions, which consist of three individual tectonic domains, the Kazakhstan-Yili plate, the Central Tianhan Terrane and the Tarim plate from north to south.
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Formation of HP–LT rocks and their tectonic implications in the western Tianshan Orogen, NW China: geochemical and age constraints

TL;DR: In this article, a well-defined 40Ar/39Ar plateau age of 344±1 Ma was obtained for crossite from an omphacite-phengite-bearing blueschist and concordant with the Sm-Nd isochron age for the eclogite, suggesting that neither argon loss nor excess argon affected the crossite.
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Archaean to Proterozoic Crustal Evolution in the Central Zone of the Limpopo Belt (South Africa^Botswana): Constraints from Combined U^Pb and Lu^Hf Isotope Analyses of Zircon

TL;DR: In this paper, a combined set of U^Pb and Lu^Hf in situ laser ablation ICP-(MC)-MS zircon analyses were obtained from orthogneisses and granitoids in the Central Zone of the Limpopo Belt, which comprises the Beit Bridge and Mahalapye complexes.
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Volcanic arcs fed by rapid pulsed fluid flow through subducting slabs

TL;DR: In this article, the authors used the Li-Ca-Sr isotope system to quantitatively constrain the duration of subduction-zone fluid release at ∼ 70 km depth within subducting oceanic lithosphere, now exhumed in the Chinese Tianshan Mountains.