2 edition of study on the Cretaceous sedimentation in Hokkaido, Japan found in the catalog.
study on the Cretaceous sedimentation in Hokkaido, Japan
Bibliography: p. 114-119.
|Statement||by Keisaku Tanaka.|
|Series||Report / Geological Survey of Japan ;, no. 197, Report (Chishitsu Chōsajo (Japan)) ;, no. 197.|
|LC Classifications||QE304 .C54a no. 197, QE471 .C54a no. 197|
|The Physical Object|
|Pagination||119 p.,  leaves of plates (some folded) :|
|Number of Pages||119|
|LC Control Number||82103393|
3 Hokkaido Forestry Research Institute (Koshunai, Bibai, Hokkaido , Japan) 4 Graduate School of Agriculture, Hokkaido University (Kita 9, Nishi 9, Kita-ku, Sapporo-shi, Hokkaido , Japan) On August 9 , Typhoon (Etau) hit the Saru . The study area is on the southeastern end (the Nemuro Peninsula) of Hokkaido Island, the northernmost island of Japan, which is at the western end of the Kuril Arc (Fig. 1). The Kuril Arc is a subduction zone that extends from Hokkaido Island to the Kamchatka Peninsula in eastern Russia.
The Cretaceous System in the Japanese Islands [Cretaceceous Research Committee, Tatsuro Matsumoto] on *FREE* shipping on qualifying offers. The Cretaceous System in the Japanese IslandsAuthor: Cretaceceous Research Committee. Introduction. The Sorachi–Yezo Belt (Kiminami et al. ) in central Hokkaido, Japan, is composed of three geological units: the Sorachi Group, the Yezo Supergroup and the Kamuikotan Sorachi Group is a peculiar accretionary complex characterized by numerous occurrences of greenstones, which extend for approximately km from north to south in central Hokkaido ().
The breakup of Rodinia about million years ago formed the Panthalassa ocean, with rocks that eventually became Japan sitting on its eastern margin. In the Early Silurian ( million years ago), the subduction of the oceanic plates started, and this process continues to the present day, forming a roughly km wide orogeny at the convergent boundary. We here describe a new Early Cretaceous (early Albian) eutherian mammal, Sasayamamylos kawaii gen. et sp. nov., from the ‘Lower Formation’ of the Sasayama Group, Hyogo Prefecture, mamylos kawaii is characterized by a robust dentary, a distinct angle on the ventral margin of the dentary at the posterior end of the mandibular symphysis, a lower dental formula .
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Geology and stratigraphy of forearc basin sediments in Hokkaido, Japan: Cretaceous environmental events on the north-west Pacific margin Article (PDF Available) in Cretaceous Research 25(3) Upper Cretaceous foraminifera from the Rumoi Coal Field, Study on the Cretaceous sedimentation in Hokkaido, Japan (Report / Geological Survey of Japan) [Fukuta, Osamu] on *FREE* shipping on qualifying offers.
Upper Cretaceous foraminifera from the Rumoi Coal Field, Hokkaido, Japan (Report / Geological Survey of Japan)Author: Osamu Fukuta. “Dinosaur fossils from Japan are exceptionally rare and most material is extremely fragmentary.
The finding of this single tooth does indicate that during the latter stages of the Late Cretaceous, this part of the world was home to large Tyrannosaurs similar to those found in similar aged rocks in North America and elsewhere in Asia.”. The Cretaceous Yezo Group, exposed in central Hokkaido, northern Japan, was probably deposited at about 35–45°N (Hoshi and Takashima,Kodama et al., ) along a westward subduction margin in the north-eastern Asian continent during the group consists of a 10,m-thick forearc sedimentary sequence of sandstones and mudstones with subordinate by: Mid-Cretaceous strata in central Hokkaido exhibit east–west lithofacies changes that are the most remarkable within the Yezo Group.
The source of Cretaceous sediments was to the east (Tanaka, ), whereas western marginal facies such as coastal, shoreface and inner-shelf sediments are widely present in the Ikushumbetsu area ().The inshore, shallow-water facies comprises the Mikasa Cited by: The Japanese islands were part of the active continental margin of Asia until the opening of the Japan Sea in the Miocene.
Of the Japanese islands, Hokkaido Island and the northeastern part of. TY - CHAP. T1 - Cretaceou biostratigraphy and ammonites in Hokkaido, Japan. AU - Hirano, H. PY - Y1 - N2 - The Cretaceous sediments of Hokkaido are composed of miogeosynclinal and deltaic sediments from the Aptian to the Maastrichtian, distributed in two belts westward of the paired metamorphic belts.
New 40ArAr total fusion ages have been obtained on sanidine from tuffs in the zone of Mantelliceras saxbii (equivalent to the same subzone of the European ammonite zonation) and the zone of Graysonites wooldridgei (equivalent to the European subzone of Neostlingoceras carcitanense).
Ages of ?. Ma and ?. Ma, for these zones, respectively, place new constraints on the age of. Cretaceous, Strihe-SlipIzumi Basin, Japan 87 In this paper, I reconstruct the depositional systems ofthe Izumi Group as an exam ple of turbidite sedimentation in a tectonically constrained, elongated basin, and evaluate the tectonic controls on the evolution of the basin.
— and —. Structure and affinities of the petrified plants from the Cretaceous of Japan and Saghalien, II. Petrified plants from the Upper Cretaceous of Hokkaido (2).
The Cretaceous (/ k r ɪ ˈ t eɪ. ʃ ə s /, krih-TAY-shəs) is a geological period that lasted from about to 66 million years ago (mya). It is the third and final period of the Mesozoic Era, as well as the name is derived from the Latin creta, "chalk".It is usually abbreviated K, for its German translation Kreide.
The Cretaceous was a period with a relatively warm climate. Title Pollen Analysis of Carbonaceous Matter from the Hakobuchi Group in the Enbetsu District, Northern Hokkaido, Japan: Palynological Study on Cretaceous Sediment (I) Author(s) Sato, Seiji Citation Journal of the Faculty of Science, Hokkaido University.
Series 4, Geology and mineralogy, 11(1), Re-evaluation of the intra-Yezo disturbance and the Cretaceous tectonics in Hokkaido, Japan.
Reishi Takashima, Hiroshi Nishi. 1) Institute of Geology and Paleontology, Graduate School of Science, Tohoku University 2) Graduate School of Social and Cultural Studies, Kyushu University.
This banner text can have markup. web; books; video; audio; software; images; Toggle navigation. Upper Albian to Lower Cenomanian biostratigraphy in the Oyubari area, Hokkaido, Japan: toward a Cretaceous biochronology for the North Pacific FUMIHISA KAWABE1, REISHI TAKASHIMA2, RYOJI WANI3, HIROSHI NISHI4 & KAZUYOSHI MORIYA5 1 Department of Earth Sciences, School of Education, Waseda University, Nishiwaseda, Shinjuku-ku, Tokyo, Japan.
Title: Pre-Cretaceous Terranes of Japan: Contributors: Kōichirō Ichikawa, International Geological Correlation Programme. ProjectPre-Jurassic Geologic Evolution of Eastern Continental Margin of Asia, International Geological Correlation Programme.
most Cretaceous. Shigeta et al. () correlated upper lower Maastrichtian strata in Southwest Japan, Hokkaido and Alaska based on the common occurrence of G.
izumi-ense Matsumoto and Morozumi, Furthermore, the discovery of G. tombetsense Matsumoto, in the Sotoizumi Group of Southwest Japan demonstrated that.
Abstract. A fauna of provannid and provannid-like shells is described from Upper Cretaceous seep carbonates in Hokkaido, Japan. We describe two new provannid species, Provanna tappuensis sp. nov. and Desbruyeresia kanajirisawensis sp.
nov., with preserved protoconchs of unquestionable provannid type with decollate material confirms the occurrence of Provannidae as early as the Middle.
Yoshihiro Kase, Gentaro Kawakami and Osamu Takano, Depositional systems and petroleum geology of the Middle–Late Miocene foreland basin deposits in the Hidaka coast area, central Hokkaido, Japan 北海道日高海岸地域の中部～上部中新統前縁盆地埋積物の堆積システムと石油地質, The Journal of.
The (δ 18O values of nine Cretaceous granitic rocks from the low P/T type regional metamorphic zone of Japan are + to +‰ relative to SMOW, while ten Cretaceous granitic rocks from the non-metamorphic zone are + to +‰.
The 18O-enrichment in the former rocks is mainly attributed to oxygen isotopic exchange between the granitic magma and the surrounding metamorphic rocks during. The study estuary, on the Niigata Plain, central Honshu, Japan, is wave-dominated and microtidal, with a barrier island and bay-head delta.
We took two m-long cores, one from an area adjacent to major river discharge and another from the basin margin.Revised parameter to measure and compile the degree of organic metamorphism of the Tertiary and the upper Cretaceous systems based on vitrinite reflectance value (R 0) are introduced; i.
e. V-value, decupled R 0, ν-value along iso-rank direction in the traditional proximate rank classification diagram (Fig.
4).Numerous data of proximate analysis of the Tertiary and the Cretaceous coalfields.Kaim, A., Jenkins, R.G., and Hikida, Y. Gastropods from Late Cretaceous Omagari and Yasukawa hydrocarbon seep deposits in the Nakagawa area, Hokkaido, Japan.
Acta Palaeontologica Polonica 54 (3) – DOI: / app Sixteen gastropod species from two Campanian (Upper Cretaceous) hydrocarbon seep localities in Hokkaido.