The Horokanai ophiolite is a geological complex located in the Kamuikotan tectonic belt about 30 km northwest of Asahikawa city, Hokkaido, Japan.[1][2] The ophiolite complex is exposed along either side of a north-dipping anticline in several blocks.[1]
^ abASAHINA, TOSHIHIRO; KOMATSU, MASAYUKI (1979). "THE HOROKANAI OPHIOLITIC COMPLEX IN THE KAMUIKOTAN TECTONIC BELT, HOKKAIDO, JAPAN". The Journal of the Geological Society of Japan. 85 (6): 317–330_1. doi:10.5575/geosoc.85.317. ISSN 0016-7630.
^ISHIZUKA, HIDEO (1981). "Geochemistry of the Horokanai ophiolite in the Kamuikotan tectonic belt, Hokkaido, Japan". The Journal of the Geological Society of Japan. 87 (1): 17–34. doi:10.5575/geosoc.87.17. ISSN 0016-7630.
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