1955•The Journal of the Japanese Association of Mineralogists Petrologists and Economic GeologistsOpen access
The preliminary study on the basic and the ultrabasic igneous rocks in the vicinities of Mt. Uhu. Aichi Prefecture
Hiroshi Asai
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Abstract
The basic and the ultrabasic igneous rocks intrude between the phyllite of the outer metamorphic zone of the median tectonic line and the non-metamorphic sedimentary rocks. The succesions of the igneous activities are following, metadiabase and metamicrogabbro, metagabbro, metagabbropegmatite, albitite, schistose-gabbro, relict olivine pyroxene serpentinite, serpentinite, diabase. These rocks are formed at the stage of the tectonic movement in this districts.
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