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| | Mino Terrane (Gifu) (Site not responding. Last check: 2007-10-09) |
 | | Central part of the Japanese Islands is underlain by basement rock-formations, consisting of limestone, greenstone, chert, shale, sandstone and sporadically conglomerate, which have been believed to be mostly late Paleozoic in age up to the 1960's, and, after the finding of Triassic conodonts in chert, to be mostly late Paleozoic to Triassic in the 1970's. |
 | | The Mino terrane is a late Jurassic to early Cretaceous melange terrane composed chiefly of Permian limestone-greenstone complex, Triassic bedded chert and shale, Jurassic siliceous tuffaceous shale, shale, sandstone and conglomerate. |
 | | The geological investigations and biostratigraphic works along with the paleontological studies have been done by dealing with rocks collected in the Mino terrane mainly in Nagoya University; therefore, most of the materials contained in this database are the data obtained in the Mino terrane of Central Japan. |
| www.num.nagoya-u.ac.jp /database/palaeont/rad1/Rad_pt_3/T_m_gf.htm (133 words) |
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