TY - JOUR
T1 - Radiolarians of the Stylocapsa (?) spiralis Zone (uppermost Middle to lower Upper Jurassic) extracted from a borehole core sample in the Chichibu Composite Belt, Hamakita City, Shizuoka Prefecture, Southwest Japan
AU - Kashiwagi, Kenji
AU - Tsukada, Kazuhiro
AU - Niwa, Masakazu
AU - Niwa, Kohsuke
AU - Miyakoshi, Noriaki
PY - 2006/3
Y1 - 2006/3
N2 - Age-determinable radiolarian assemblage was extracted from a borehole core in Hamakita City, east of Lake Hamana-ko, Shizuoka Prefecture, Southwest Japan. Rocks of the borehole core are derived from a melange belonging to the accretionary complex of the Chichibu Composite Belt. The core consists of blocks of mafic volcanic rocks, limestone, chert, sandstone and so on in a scaly mudstone matrix. The radiolaria-bearing sample is the alternation of thin beds of sandstone and siltstone, which occurs as a block in a scaly mudstone matrix. Radiolarian assemblage from the sample belongs to the Stylocapsa (?) spiralis Zone, which indicates latest Middle to early Late Jurassic age (latest Callovian to Oxfordian) according to the radiolarian zonation in Japan and the western Pacific of Matsuoka (1995). On the basis of the radiolarian age of the alternation, we conclude that the formative age of the melange is the latest Middle to early Late Jurassic or later.
AB - Age-determinable radiolarian assemblage was extracted from a borehole core in Hamakita City, east of Lake Hamana-ko, Shizuoka Prefecture, Southwest Japan. Rocks of the borehole core are derived from a melange belonging to the accretionary complex of the Chichibu Composite Belt. The core consists of blocks of mafic volcanic rocks, limestone, chert, sandstone and so on in a scaly mudstone matrix. The radiolaria-bearing sample is the alternation of thin beds of sandstone and siltstone, which occurs as a block in a scaly mudstone matrix. Radiolarian assemblage from the sample belongs to the Stylocapsa (?) spiralis Zone, which indicates latest Middle to early Late Jurassic age (latest Callovian to Oxfordian) according to the radiolarian zonation in Japan and the western Pacific of Matsuoka (1995). On the basis of the radiolarian age of the alternation, we conclude that the formative age of the melange is the latest Middle to early Late Jurassic or later.
UR - http://www.scopus.com/inward/record.url?scp=33750279941&partnerID=8YFLogxK
M3 - 学術論文
AN - SCOPUS:33750279941
SN - 1347-5622
SP - 41
EP - 46
JO - Memoir of the Fukui Prefectural Dinosaur Museum
JF - Memoir of the Fukui Prefectural Dinosaur Museum
IS - 5
ER -