As shown on the map by Niida (1974) the rocks of the Horoman peridotite body are mainly plagioclase lherzolite, lherzolite, and dunite, as well as small amounts of gabbro and pyroxenite. Interlayered plagioclase lherzolite and dunite account for almost all of the bedrock surface in the northern three-quarters of the body, from south of Mt. Apoi to north of Mt. Pinneshiri, a distance of about seven kilometers. Thus, these two rock types dominate the lithology of the body. The remaining southern one-quarter of the surface is mainly interlayered lherzolite and dunite. You can download Prof. Niida's 1984 paper, including the dramatic geological map, from: http://eprints.lib.hokudai.ac.jp/dspace/handle/2115/36729 This will take you to the abstract of Dr. Niida's paper in HUSCAP, Hokkaido University Scholarly and Academic Papers. To download the entire PDF (11.4 mb), click the "View/Open" box. The map is on the fourth page (page 200).
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University students on a field trip in the Horoman peridotite complex. Layering is clearly visible in the fallen rock at right. Photo: geomantleh1 via lherzharz1.exblog.jp |
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REFERENCES
Niida, K., (1974), Structure of the Horoman Massif of the Hidaka Metamorphic Belt, Jour. Geol Soc. Japan; 80:1, p. 31-44. (In English)
Niida, K., (1984), Petrology of the Horoman Ultramafic Rocks in the Hidaka Metamorphic Belt, Hokkaido, Japan, Journal of the Faculty of Science, Hokkaido University. Series 4, Geology and mineralogy, 21(2):197-250. (In English)
Niida, K., and Takazawa, E. (2007), Origin of Layering observed in the Horoman Peridotite Complex, Japan, Jour. Geol Soc. Japan; 113:Supplement, p. 167-184. (In Japanese except for some of the figure labels)
Takahashi, N., (1991), Origin of three peridotite suites from the Horoman peridotite complex, Hokkaido, Japan; Melting, melt segregation, and solidification processes in the upper mantle; Jour. Min.Petr. Econ. Geol., 86: p. 199-215. (In English)
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