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Shibikawa Formation

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FIGURE 5—Regression of outer borehole diameter (OBD) (=predator size) for complete boreholes on shell length (=prey size) at five localities where more than 30 bored specimens were obtained. (A) Early late Miocene Kubota Formation (Locality 1). (B) Pliocene Tentokuji Formation (Locality 2). (C) Early Pleistocene Sawane Formation (Locality 6). (D) Middle Pleistocene Shibikawa Formation (Locality 11). (E) Middle Pleistocene Shibikawa Formation (Locality 12)
Published: 01 August 2006
) Early Pleistocene Sawane Formation (Locality 6). (D) Middle Pleistocene Shibikawa Formation (Locality 11). (E) Middle Pleistocene Shibikawa Formation (Locality 12)
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Published: 01 July 2000
Table 1 Sedimentary facies classification of depositional succession covering the basal part of the Shibikawa Formation to the middle part of the Katanishi Formation. Facies code, lithologic features, and depositional environments with depositional depth are summarized.
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FIGURE 2—Drilled specimens. (A) Edge-drilled specimen, length=13.5 mm, Locality 12, middle Pleistocene Shibikawa Formation. (B) Completely bored specimen at the umbonal part, length=28.1 mm, Locality 3, Pliocene Nadachi Formation. (C) Completely drilled specimen at the central part of disc, length=40.2 mm, Locality 2, Pliocene Tentokuji Formation. (D) Incompletely bored specimen, length=35.1 mm, Locality 2, Pliocene Tentokuji Formation
Published: 01 August 2006
FIGURE 2 —Drilled specimens. (A) Edge-drilled specimen, length=13.5 mm, Locality 12, middle Pleistocene Shibikawa Formation. (B) Completely bored specimen at the umbonal part, length=28.1 mm, Locality 3, Pliocene Nadachi Formation. (C) Completely drilled specimen at the central part of disc, length
Journal Article
Published: 01 July 2000
Journal of Sedimentary Research (2000) 70 (4): 839–849.
...Table 1 Sedimentary facies classification of depositional succession covering the basal part of the Shibikawa Formation to the middle part of the Katanishi Formation. Facies code, lithologic features, and depositional environments with depositional depth are summarized. ...
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Journal Article
Journal: PALAIOS
Published: 01 August 2006
PALAIOS (2006) 21 (4): 369–375.
...) Early Pleistocene Sawane Formation (Locality 6). (D) Middle Pleistocene Shibikawa Formation (Locality 11). (E) Middle Pleistocene Shibikawa Formation (Locality 12) ...
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Journal Article
Published: 01 May 2002
Journal of Sedimentary Research (2002) 72 (3): 386–392.
... exposed along the coast of the Oga Peninsula, where they generally dip eastward and become younger to the east, from Miocene to Holocene. The Quaternary sediments are divided, in ascending order, into the Kitaura, Wakimoto, Shibikawa, Katanishi, and Iriai formations ( Fig. 1B ; e.g., Shiraishi 2000...
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Journal Article
Published: 01 September 2003
Journal of Paleontology (2003) 77 (5): 863–872.
... constricta Dall , 1918 , p. 228–229; Kosuge , 1972 , pl. 9, fig. 5. Searlesia shimosensis Oinomikado , 1935 , p. 598–599, pl. 1, figs. 5–6. Pliocene to Recent. Pliocene: Kuwae and Nadachi Formations, Niigata Prefecture. Pleistocene: Tomikawa Formation, Hokkaido; Shibikawa and Katanishi...
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Journal Article
Journal: Paleobiology
Published: 09 February 2016
Paleobiology (2016) 42 (2): 257–268.
... on fossil shells of the bivalve Glycymeris yessoensis . This bivalve species is most abundant among the fossil molluscan assemblages and has durable shells, making it relatively easy to examine the predatory drillholes quantitatively. The middle Pleistocene Shibikawa Formation...
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Journal Article
Published: 01 June 1983
Journal of the Geological Society (1983) 140 (3): 475–487.
... in Japan, 1969). W = Wakimoto F., S = Shibikawa F., K = Katanishi F. (Akitaj, H = Haizume F., 0 = Oguni F. (Niigataj. Geochemical features of the existence of the 'principal phase of oil formation' oil-producing formations obtained from the above presumed source beds seems to support the hypothesis...
Journal Article
Journal: AAPG Bulletin
Published: 01 July 1934
AAPG Bulletin (1934) 18 (7): 908–924.
... are found exclusively in marine Neogene formations. The chief oil fields in Hokkaidō are those of Masuhoro, Ishikari, and Yufutsu, of which Yufutsu is the most important. In the Prefecture of Akita, the oil fields of Kurokawa, Toyokawa, Michikawa-Asahigawa, and Oguni are noteworthy, though at present...
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