短報
岐阜県丹生川村, 飛騨外縁帯森部層より産出した中期ペルム紀紡錘虫化石
2004 年 110 巻 6 号 p. 384-387
詳細
2004 年 110 巻 6 号 p. 384-387
This paper reports the following Middle Permian fusulinoideans from the Moribu Formation in the Hida-gaien Tectonic Zone, central Japan: Monodiexodina matsubaishi (Fujimoto), Monodiexodina sp. and Codonofusiella sp. These fusulinoideans clearly show that the lower part of the Moribu Formation is of Middle Permian age. It further suggests that a significant hiatus exists between the Moribu Formation and the underlying Arakigawa Formation.
