| Project/Area Number |
01302018
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| Research Category |
Grant-in-Aid for Co-operative Research (A)
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| Allocation Type | Single-year Grants |
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| Research Field |
地質学一般
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| Research Institution | Nagoya University |
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Principal Investigator |
SUWA Kanenori Nagoya University, School of Science, Professor, 理学部, 教授 (70022564)
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| Co-Investigator(Kenkyū-buntansha) |
AIHARA Atsuo Kyusyu University, Faculty of Science, Professor, 理学部, 教授 (80037291)
SHIMAZAKI Hidehiko University of Tokyo, Faculty of Science, Professor, 理学部, 教授 (50013751)
SAITO Tsunemasa Tohoku University, Faculty of Science, Professor, 理学部, 教授 (90111335)
KATO Makoto Hokkaido University. Faculty of Science, Professor, 理学部, 教授 (60000824)
MIZUTANI Shinjiro Nagoya University, School of Science, Professor, 理学部, 教授 (50022538)
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| Project Period (FY) |
1989 – 1991
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| Project Status |
Completed (Fiscal Year 1991)
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| Budget Amount *help |
¥16,500,000 (Direct Cost: ¥16,500,000)
Fiscal Year 1991: ¥5,200,000 (Direct Cost: ¥5,200,000)
Fiscal Year 1990: ¥5,200,000 (Direct Cost: ¥5,200,000)
Fiscal Year 1989: ¥6,100,000 (Direct Cost: ¥6,100,000)
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| Keywords | Geotraverse / the Japanese Islands / Metamorphic belt / Age determination / Island arc / Suture zone / Precambrian / Volcano / 変成岩 / 堆積岩 / 鉱床 |
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| Research Abstract |
Geotraverses of the Japanese Iiands
The Japanese Islands are divided into two principal geologic provinces, Northeast Japan and Southwest Japan. Both provinces are composed of many tectonostratigraphic terrenes. Without knowledge of these terrenes, the complex geological history of the Japanese Islands can not be properly understood.
The purpose of this study is to examine intra- and inter-terrene relations as well as stratigraphic, sedimentological, geochronological and metamorphic characteristics of these terrenes through geotraverses in many regions in the Japanese Islands, from Hokkaido to Okinawa, and to overview the Paleozoic to Cenozoic geologic evolution.
As a result of this study, the following lines of new evidence were obtained.
(1). In the central part of the Hida terrene the so-called Precambrian Gray Granite occurs as veins and dikes cutting the Hida gneiss. The detailed geochronological studies on the basis of CHIME ages of monazites and zircons from the Gray, franite have revealed that it intruded into the Hida gneiss in early Triassic time (ca. 240 Ma). not in Precambrian time.
(2). CHIME age data of monazite and zircon grains from the Carboniferous llikami granite in the Soutil Kitakami terrene have shown that the ca. 250 Ma thermal event is also recorded in tile rims of many zircon crystals in the granite. It seems probable that the latest Permian magnatism was much more extensive both in Northeast Japan and Southwest Japan than has been thought.
(3). The oldest radiometric date is a 2050 Ma Rb-Sr whole-rock isochron age (originally 1985 Ma, it was recalculated using the currently-accepted decay constant) for quartzo-feldspathic gneisses in the Kamiaso conglomerate. CHIME ages of monazites in quartzo-feldspathic gneiss clasts and sandstones in the Mino terrene also give ca. 1700-1400 Ma, showing that the middle Precambrian rocks were widespread in the provenance of the classic rocks.
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