| Project/Area Number |
04302021
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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 | SHIZUOKA UNIVERSITY |
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Principal Investigator |
MASUDA Toshiaki INSTITUTE OF GEOSCIENCES SHIZUOKA UNIVERSITY, ASSISTANT PROFESSOR, 理学部, 助教授 (30126164)
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| Co-Investigator(Kenkyū-buntansha) |
NOHDA Susumu FACULTY OF LIBERAL ART, KYOTO-SANGYO UNIVERSITY PROFESSOR, 教養部, 教授 (30065841)
OTOFUJI Yoichiro DEPARTMENT OF EARTH SCIENCES, KOBE UNIVERSITY, ASSISTANT PROFESSOR, 理学部, 助教授 (90160895)
ITAYA Tetsumaru HIRUZEN RESEARCH INSTITUTE, OKAYAMA SCIENCE UNIVERSITY, PROFESSOR, 蒜山研究所, 教授 (60148682)
MARUYAMA Shigenori DEPARTMENT OF EARTH AND PLANETARY SCIENCES, TOKYO INSTITUTE OF TECHNOLOGY PROFES, 理学部, 教授 (50111737)
WADA Hideki INSTITUTE OF GEOSCIENCES SHIZUOKA UNIVERSITY, ASSISTANT PROFESSOR, 理学部, 助教授 (20126791)
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| Project Period (FY) |
1992 – 1993
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| Project Status |
Completed (Fiscal Year 1993)
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| Budget Amount *help |
¥9,400,000 (Direct Cost: ¥9,400,000)
Fiscal Year 1993: ¥5,000,000 (Direct Cost: ¥5,000,000)
Fiscal Year 1992: ¥4,400,000 (Direct Cost: ¥4,400,000)
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| Keywords | Greenland / Isua / Oldest rocks of the Earth / Archaean / Metamorphism / Conglomerate / Pillow lave / Banded iron formation / メタチャート / 超塩基性岩 / マイクロブーディン構造 / イリジウム / イスア表成岩帯 / 地球史 / 太古代 / 38億年前 / 変成岩 / 地球外物質 |
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| Research Abstract |
Strain analysis of the conglomerate showed that axial ratios of the strain ellipsoid is 3.73 and 1.23 in the XZ and YZ planes, respectively. The conglomerate before the deformation was restored by the de-straining technique, and found to be a pebbly mudstone. The deposition of the conglomerate is presumed to have taken place in deeper water environment than that previously considered. Five different lithologies are discriminated in the banded cherts : green, white, black gray and brown layrs. Anomalously large amount of lr was detected in a black layr by the INAA technique. Such high lr content suggests that anomalously large amount of extraterrestrial materials were accumulated in the early Archaean ocean. The banded iron formations were divided into five different lithologies : black, red, white, green and gray layrs, They commonly consists of quartz, magnetite, amphibole and carbonate. Their component are different from layr to layr. The depositional rhythm has not yet found out from the banded iron formation. Metamorphic zonation in the lsua region was proposed ; the region is divided into three zones on the basis of metamorphic mineral assemblages : amphibolite, amphibolite/greenschist and greenschist facies in the ascending order of metamorphic grade. Pyroxenes in the peridotite is found to be linearly arranged and boudinaged. These structures strongly indicate that the mantle convection in the early Archaean was much faster that that in Phanerozoic. The pillow lave conformably overlain by cherts has been discovered by the Japanese group. The pillow lava-chert assemblage is the same as the top of the present-day oceanic crust. This discovery suggests that the tectonic processes in the early Archaean is very similar to the plate tectonics active in the phanerozoic.
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