Variation of rock facies in Yasu granitic pluton, southern part of Lake Biwa, Southwest Japan
The Cretaceous granitic complex in the southern part of Lake Biwa occurs as a ring-shape complex. The complex is composed mainly of Hira, Hiei, Tanakami, Suzuka, and Yasu granitic plutons. The Yasu granitic pluton, which has stock shape and 10 km (N-S) to 8 km (E-W) extension, is situated at the mos...
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| Veröffentlicht in: | Chishitsugaku zasshi 2002/01/15, Vol.108(1), pp.1-15 |
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| Hauptverfasser: | , |
| Format: | Artikel |
| Sprache: | eng ; jpn |
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