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Bruno Turi
Researcher at Sapienza University of Rome
Publications - 45
Citations - 1234
Bruno Turi is an academic researcher from Sapienza University of Rome. The author has contributed to research in topics: Volcanic rock & Igneous rock. The author has an hindex of 18, co-authored 45 publications receiving 1198 citations.
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Oxygen isotope studies of potassic volcanic rocks of the Roman Province, Central Italy
Bruno Turi,Hugh P. Taylor +1 more
TL;DR: In this article, the authors measured the 18O/16O ratios of 93 samples of leucite-bearing lavas, pyroclastics, and related volcanic rocks from the Quaternary Roman Co-Magmatic Province, Italy.
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Isotopic study of the origin of sulfur and carbon in Solfatara fumaroles, Campi Flegrei caldera
TL;DR: In this paper, an isotopic study of the origin of sulfur and carbon in the hottest (Solfatara) fumaroles of Campi Flegrei caldera, Southern Italy, was carried out on gas samples collected between 1983 and 1988, i.e. during and after the 1982-1984 seismo-volcanic crisis.
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Late Pleistocene Paleoclimates and sea-level change in the Mediterranean as inferred from stable isotope and U-series studies of overgrowths on speleothems, Mallorca, Spain
TL;DR: In this article, a number of phreatic overgrowths on speleothems have been dated using the Th/U method in order to determine the position of the sea level during Late Quaternary.
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High-18O igneous rocks from the Tuscan Magmatic Province, Italy
Hugh P. Taylor,Bruno Turi +1 more
TL;DR: In this article, the authors measured the 18O/16O ratios of 60 rocks and coexisting minerals from the Plio-Pleistocene, calc-alkaline, Tuscan Magmatic Province, Italy.
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Oxygen isotope geochemistry of the potassic igneous rocks from the Roccamonfina volcano, Roman comagmatic region, Italy
TL;DR: In this article, the authors reported that assimilation of high-18O country rocks (pelitic schists, flysch, and some carbonates) was an important petrologic process during fractional crystallization of both the early, HKS and the later, LKS magmas (trachybasalts, trachyandesites, and trachytes).