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環日本海地域比較層序論(前編)
Comparative Stratigraphy around the Sea of Japan (I)
1984
Journal of Geography (Chigaku Zasshi)
Comparative Stratigraphy around the Sea of Japan (I)
Preserved Fulltext
The Mongolian and Chichibu geosynclines were confluent with each other at the Touman-Suifung area and the intrageosynclinal vulcanism was there repeated during the Palaeozoic era.
doi:10.5026/jgeography.93.191
fatcat:ymcwdv4b3jcsbi4szl5d7fdhh4