The Mesozoic strata of the Osaka area, Oita Prefecture, Kyushu, are distributed in several narrow regions within Chichibu Terrain. On the basis of stratigraphic and paleontological studies, they are classified into the following formations: the Koshigoe {Hauterivian-Lower Barremian}, Haidate (emend.) {Barremian}, Osaka {Barremian} and Shiibaru {Cenomanian} Formations. Among them the Koshigoe and Haidate Formations are combined under the name Haidateyama Group. The Koshigoe Formation unconformably overlies the basement rocks with a conglomerate. On the other hand, the Osaka Formation belongs to one of the “Pre-Sotoizumi Group”. Therefore the “Pre-Sotoizumi Group” which was regarded as a member of the Ryoke Belt, is cropping out as the thrust sheets on the Hidateyama Group, in the Osaka and Takaya areas.
In this paper, the Stratigraphy is described in some detail, with remarks on correlation, and the features of the bivalve faunas are made clear. The faunal composition with other areas of Southwest Japan, together with the faunal change in time and space, are also discussed.
雑誌名
熊本大学教育学部紀要 自然科学
巻
61
ページ
29 - 38
発行年
2012-12-12
ISSN
04546148
書誌レコードID
AN10315071
フォーマット
application/pdf
形態
12201079 bytes
著者版フラグ
publisher
日本十進分類法
450
その他の言語のタイトル
Thrust Nappe of the Cretaceous in the Chichibu Terrane (Osaka Subbelt), Oita Prefecture
大分県秩父帯（小坂亜帯）白亜系の衝上ナップ
KN0061_029-038.pdf
(12.2MB)
