Partitioning of Sr between coexisting minerals of the hollandite- and piemontite-groups in a quartz-rich schist from the Sanbagawa metamorphic belt, Japan

Coexisting minerals of the hollandite-cryptomelane series, piemontite-group , and abswurmbachite-braunite series occur as a small nodule in a quartzose schist (metachert) from the epidote-amphibolite facies area of the Sanbaga wa metamorphic belt, central Shikoku, Japan. Strontium, Ba, K, and Pb conte nts of the hollandite-cryptomelane minerals are 0.00-0.42, 0.07-0.99, 0.00- 0.75 and 0.00-0.05 apfu (atoms per formula unit: O = 16), respectively. The piemontite-group minerals can be divided into common piemontite (Ca > Sr i n the ten-coordinated A2-site) and strontiopiemontite (Sr > Ca). Strontium, Ba and Pb contents of the strontiopiemontite reach 0.71, 0.26 and 0.20 apf u (O = 12.5), respectively, suggesting the existence of two possible new en d-members for epidote-group minerals: "Ba-piemontite [BaCa(Mn3+, Fe3+, Al)( 3)Si3O12(OH)]" and "Pb-piemontite [PbCa(Mn3+, Fe3+, Al)(3)SiO12(OH)]." The abswurmbachite-braunite series minerals (Cu = 0.30-0.53 apfu: O = 12) conta in up to 0.34 apfu Mg, indicating the exchange Mg(Mn2+, Cu)(-1). Distributi on coefficients for Sr between the hollandite-cryptomelane series and the p iemontite-group minerals are up to 20, implying that the hollandite-type st ructure with its large open tunnel is more suitable for incorporation of Sr than the A2-site of the piemontite-group minerals. A synthetic aluminosili cate analogue of the hollandite-cryptomelane compound is stable under P > 8 -10 GPa, and suggests the hollandite-type aluminosilicate may be a reservoi r of Sr and other large-ion-lithophile elements in the upper mantle.