1979
DOI: 10.2343/geochemj.13.113
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Rb-Sr whole-rock and K-Ar mineral ages of granitic rocks in Japan.

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Cited by 126 publications
(42 citation statements)
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“…Considering the ages reported for the host rock [7][8][9], the dike swarm was emplaced in the final stage of the Late Cretaceous extensive igneous activity, as Kinoshita [26] interpreted as resulting from subduction of oceanic plates' divergent margin. Oikawa et al [24] stated that their K-Ar age for the andesitic dike provides the upper limit of the intrusion event.…”
Section: Time Sequence Of Igneous Activitymentioning
confidence: 99%
See 1 more Smart Citation
“…Considering the ages reported for the host rock [7][8][9], the dike swarm was emplaced in the final stage of the Late Cretaceous extensive igneous activity, as Kinoshita [26] interpreted as resulting from subduction of oceanic plates' divergent margin. Oikawa et al [24] stated that their K-Ar age for the andesitic dike provides the upper limit of the intrusion event.…”
Section: Time Sequence Of Igneous Activitymentioning
confidence: 99%
“…The pluton has yielded a CHIME monazite age of 68.3 ± 1.8 Ma [7] and whole-rock Rb-Sr ages of 72.3 ± 3.9 Ma [8] and 68.2 ± 1.1 Ma [9]. It is a stock, 14 km × 12 km in areal extent [10], having a vertical thickness of at least 1.5 km based on borehole investigations by JAEA.…”
Section: Geological Settingsmentioning
confidence: 99%
“…The Tono uranium mine is located in the Tono district, Gifu, in the central part of Japan ( Fig. 1 The length of boreholes: 500 m (DH-1, DH-2 and DH-4), 840 m (DH 20 Ma) and the Seto Group (0.7-5 Ma), with a combined total thickness of less than 200 m (Itoigawa, 1974), unconformably overlying the Toki granite (72.3± Ma; Shibata and Ishihara, 1979). The Toki granite consists of medium to coarse-grained biotite granite and medium-grained homblende-biotite porphyry, and is partly intruded by quartz porphyry and aplite dikes.…”
Section: Introductionmentioning
confidence: 99%
“…Location 1: Magarisawa tonalite (Shibata et al, 1984;Kemp et al, 2007); locations 2 and 3: Pankenushi gabbro (2: Maeda et al, 1990 andKemp et al, 2007;3: Maeda et al, this study, underlined ages); and location 4: Memurodake diorite . Ages reported for the Nissho Toge granite are shown on this map (Shibata and Ishihara, 1979;Ishihara and Terashima, 1985;Kuramoto et al, in press). Simplified geological boundaries are also shown.…”
mentioning
confidence: 99%
“…16.6 0.7 Ma K-Ar Terashima, 1985 17.3 Ma Shibata andIshihara, 1979 Rb Table 1 30 kg Komatsu et al, , 1994. Abbreviations: Chl = chlorite, Ms = muscovite, Bt = biotite, Grt = garnet, Crd = cordierite, Opx = orthopyroxene.…”
mentioning
confidence: 99%