Late Mesozoic coral-bearing limestone in the Murotsu area, Toyoura Town, western Yamaguchi Prefecture, Southwest Japan

Corals, nerineid gastropods, bivalves and cidarid echinoids were discovered from limestones in western Yamaguchi Prefecture. The fauna is comparable to the Torinosu Fauna widely distributed in the Chichibu Belt, Outer Zone of SW Japan.These limestones have been regarded as lacustrine facies belongin...

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Bibliographic Details
Published inChishitsugaku zasshi Vol. 107; no. 12; pp. 794 - 797
Main Authors Yoshidomi, Ken-ichi, Inoue, Yasuko
Format Journal Article
LanguageJapanese
English
Published Tokyo The Geological Society of Japan 01.12.2001
Japan Science and Technology Agency
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Summary:Corals, nerineid gastropods, bivalves and cidarid echinoids were discovered from limestones in western Yamaguchi Prefecture. The fauna is comparable to the Torinosu Fauna widely distributed in the Chichibu Belt, Outer Zone of SW Japan.These limestones have been regarded as lacustrine facies belonging to the Lower Cretaceous Wakino Subgroup (Kanmon Group). The formation containing limestones is divided into four members in ascending order ; Lower Mudstone Member, Middle Sandstone and Mudstone Member, Upper Limestone Member and Uppermost Sandstone and Mudstone Member. Uppermost Sandstone and Mudstone Member is correlated with the Yoshimo formation (Toyonishi Group) with brackish fauna, accordingly, it is concluded that conformably underlies Upper Limestone Member also belongs to the Toyonishi Group. Coral-limestone indicates that the Tethys Sea expanded to studied area in Early Cretaceous.
ISSN:0016-7630
1349-9963
DOI:10.5575/geosoc.107.794