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Ellen Kooijman

Researcher at Swedish Museum of Natural History

Publications -  62
Citations -  1715

Ellen Kooijman is an academic researcher from Swedish Museum of Natural History. The author has contributed to research in topics: Zircon & Geology. The author has an hindex of 21, co-authored 48 publications receiving 1273 citations. Previous affiliations of Ellen Kooijman include University of California, Santa Barbara & University of Münster.

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Constraints on the U-Pb systematics of metamorphic rutile from in situ LA-ICP-MS analysis

TL;DR: In this article, a new T c (x ) model was constructed based on the analyzed age profiles that are described by an error function, which is interpreted to be the extrapolated theoretical absolute temperature of insignificant Pb diffusion in rutile.
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Magmatic and metamorphic history of Paleoarchean tonalite–trondhjemite–granodiorite (TTG) suite from the Singhbhum craton, eastern India

TL;DR: In this paper, texturally controlled dating of zircon from Paleoarchean tonalite-trondhjemite-granodiorites of the Older Metamorphic Tonalitic Gneisses and the Singhbhum Granite batholith (Phases I, II, and III) reveals a polycyclic evolution of the Archean crust.
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Lithostructural and chronological constraints for tectonic restoration of Proterozoic accretion in the Eastern Indian Precambrian shield

TL;DR: In this article, the authors used laser ablation inductively coupled plasma mass spectrometry (LAMS) to estimate the ages of the Chottanagpur Gneiss Complex (CGC), the North Singhbhum Mobile Belt (NSMB) and the Singhbhem Craton (SC).
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Trace element systematics in granulite facies rutile: implications for Zr geothermometry and provenance studies

TL;DR: In this paper, electron probe micro-analysis of rutile grains from three metapelitic gneisses was performed using a spatial resolution of down to 2μm.
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Petrology and Geochronology of Rutile

TL;DR: Triebold et al. as mentioned in this paper reviewed rutile occurrences, trace element geochemistry, and U-Pb geochronology individually to illustrate the insights that can be gained from microstructures, chemistry and ages.