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Whole‐rock Geochemistry of Basic Schists from the Besshi Area, Central Shikoku: Implications for the Tectonic Setting of the Besshi Sulfide Deposit
Author(s) -
Nozaki Tatsuo,
Nakamura Kentaro,
Awaji Shunsaku,
Kato Yasuhiro
Publication year - 2006
Publication title -
resource geology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.597
H-Index - 43
eISSN - 1751-3928
pISSN - 1344-1698
DOI - 10.1111/j.1751-3928.2006.tb00295.x
Subject(s) - schist , geology , geochemistry , protolith , metamorphic rock , volcanogenic massive sulfide ore deposit , sulfide , mineralogy , pyrite , sphalerite , chemistry , organic chemistry
Abstract. Whole‐rock chemical compositions of the Besshi basic schist closely associated with the Besshi massive sulfide deposit from the Sanbagawa Belt are reported. Studied samples were collected from four outcrops around the Dozan‐goe, central Shikoku. Common metamorphic mineral assemblage of the basic schist is albite + epidote + actinolite + chlorite ± muscovite ± quartz. Major element contents are similar to those of typical tholeiitic basalts. Trace element patterns of the basic schist normalized to normal mid‐ocean ridge basalt (N‐MORB) are generally flat, although concentrations of highly mobile large‐ion lithophile elements are quite variable. Chondrite‐normalized rare earth element (REE) patterns are flat to slightly light REE‐depleted patterns. In the Hf‐Th‐Ta and Nb‐Zr‐Y discrimination diagrams, basic schist samples closely associated with the sulfide deposit are plotted within the N‐MORB field. The Th/Nb ratios of the basic schist are also comparable to those of N‐MORB. These geo‐chemical lines of evidence indicate that the protolith of the Besshi basic schist is N‐MORB and the Besshi sulfide deposit was formed by hydrothermal activity in conjunction with MOR volcanism.