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Tetsumaru Itaya

Researcher at Okayama University of Science

Publications -  180
Citations -  4625

Tetsumaru Itaya is an academic researcher from Okayama University of Science. The author has contributed to research in topics: Volcanic rock & Metamorphic rock. The author has an hindex of 36, co-authored 178 publications receiving 4319 citations. Previous affiliations of Tetsumaru Itaya include Stanford University.

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Argon isotope analysis by a newly developed mass spectrometric system for K-Ar dating.

TL;DR: A new mass spectrometer and associated analytical systems, called HIRU, was designed and constructed for the argon isotope analysis of minerals from young volcanic rocks as well as metamorphics and granitoids as mentioned in this paper.
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Rapid rotation of southwest Japan—palaeomagnetism and K‐Ar ages of Miocene volcanic rocks of southwest Japan

TL;DR: In this article, the angular velocity of southwest Japan about a rotation pole at 129°E, 34°N reached 20° Myr−1 at about 15 Ma, whereas a northerly declination is observed in formations younger than 14.2 ± 0.6 Ma.
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Contemporaneous formation of adjacent porphyry and epithermal Cu-Au deposits over 300 ka in northern Luzon, Philippines

TL;DR: In this article, the Lepanto epithermal Cu-Au deposit overlays the Far Southeast porphyry copper-alunite mine, and the ages of alunite from Lepanto have the same range as those of hydrothermal biotite and illite from the FSE mine.
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Muscovite K-Ar ages of the Sanbagawa schists, Japan and argon depletion during cooling and deformation

TL;DR: In this article, the Sanbagawa schists in central Shikoku, Japan have been studied using the K-Ar method and the results show that the ages of the schists are consistently older with increasing metamorphic grade.
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A new Late Miocene great ape from Kenya and its implications for the origins of African great apes and humans.

TL;DR: A new genus of great ape recently discovered from the early Late Miocene of Nakali, Kenya, called N. nakayamai could be close to the last common ancestor of the extant African apes and humans, and the associated primate fauna shows that hominoids and other non-cercopithecoid catarrhines retained higher diversity into the early late Miocene in East Africa than previously recognized.