Abstract
Reports the depositional environment of the Amanokawara Formation with limestone-breccia facies, one of the Permian oceanic-rock units of the Funabuseyama mass in the Mino terrane. The carbonates are interpreted as deposits of a shallow-marine carbonate buildup with a lagoonal flat, sand bars and shoals, marginal terrace, and foreslope on a basaltic mound in an open-ocean realm. -from Author
Original language | English |
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Pages (from-to) | 527-540 |
Number of pages | 14 |
Journal | Journal - Geological Society of Japan |
Volume | 95 |
Issue number | 7 |
DOIs | |
Publication status | Published - 1989 |
All Science Journal Classification (ASJC) codes
- Environmental Science(all)
- Engineering(all)
- Earth and Planetary Sciences(all)