Abstract
Scleractinian corals were discovered from the limestone conglomerate distributed along the Shimochizawa River, west of Fukushi in the Kuzumaki-Kamaishi Belt (Jurassic accretionary complexes), Northeast Japan. These corals give the first evidence for Mesozoic limestone body present in the belt. The limestone conglomerates are lenticular in distribution pattern and interbedded in the thick bedded chert slab. They can be traced from the Shimochizawa River, trending NNW, to the north of Kita-Kawame over a distance of about 6 km.
Sign-in/Register to access full text options 
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
