D
Daniel J. Schulze
Researcher at University of Toronto
Publications - 46
Citations - 2315
Daniel J. Schulze is an academic researcher from University of Toronto. The author has contributed to research in topics: Kimberlite & Xenolith. The author has an hindex of 23, co-authored 43 publications receiving 2030 citations.
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Zircon megacrysts from kimberlite: oxygen isotope variability among mantle melts
TL;DR: The oxygen isotope ratios of phanerozoic zircons from kimberlite pipes in the Kaapvaal Craton of southern Africa and the Siberian Platform vary from 4.7 to 5.9 as mentioned in this paper.
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Zircons from kimberlite: New insights from oxygen isotopes, trace elements, and Ti in zircon thermometry
F. Zeb Page,Bin Fu,Noriko T. Kita,John H. Fournelle,Michael J. Spicuzza,Daniel J. Schulze,Fanus Viljoen,Miguel Angelo Stipp Basei,John W. Valley +8 more
TL;DR: A suite of 88 zircons found in kimberlites from Africa, Siberia, Brazil, and the United States have been analyzed for their Ti concentration and selected zirons were analyzed for rare earth element (REE) concentrations by ion microprobe.
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Timing of Precambrian melt depletion and Phanerozoic refertilization events in the lithospheric mantle of the Wyoming Craton and adjacent Central Plains Orogen
TL;DR: Garnet peridotite xenoliths from the Sloan kimberlite (Colorado) are variably depleted in their major magmaphile (Ca, Al) element compositions with whole rock Re-depletion model ages generally consistent with this depletion occurring in the mid-Proterozoic as discussed by the authors.
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A classification scheme for mantle-derived garnets in kimberlite: a tool for investigating the mantle and exploring for diamonds
TL;DR: In this paper, a new empirical method has been devised for classification of mantle-derived garnets in kimberlite, based on Mg, Fe, Ca, Cr, Ti and Na values.
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Extreme crustal oxygen isotope signatures preserved in coesite in diamond
TL;DR: The oxygen isotope values of coesite (a polymorph of SiO2) inclusions are substantially higher than previously reported for xenoliths from the subcratonic mantle, but are typical of subduction-zone meta-basalts, and accordingly provide strong support for the link between altered ocean-floor basalts and mantle eclogite Xenoliths.