STABLE-ISOTOPE GEOCHEMISTRY OF CLAY-MINERALS FROM FOSSIL AND ACTIVE HYDROTHERMAL SYSTEMS, SOUTHWESTERN HOKKAIDO, JAPAN

Miocene submarine to Quaternary terrestrial volcanism in southwestern Hokkaido, Japan, is associated with hydrothermal clay alteration and m ineralization, including Kuroko-type deposits at Kagenosawa (14.2 Ma, Cu > Zn, Pb > Au) and Minamishiraoi (12.5 Ma, Ba > Zn, Pb, Cu), vein-s tyle mineralization at Date (5.2 Ma, Au-Ag-Cu-Pb-Zn) and Chitose (3.6 Ma, Au-Ag), and geothermal activity at Noboribetsu (less than or equal to 1.8 Ma). The delta D and delta(18)O values of mica (sericite), mic a-smectite, chlorite, chlorite-smectite, nacrite, dickite, kaolinite, and smectite were used to deduce the type(s) of hydrothermal fluid at each locality. Calculated compositions for Minamishiraoi and Kagenosaw a fluids suggest that seawater was dominant, but some mixing with magm atic water is also indicated, particularly for the polymetallic Kageno sawa deposit. Hydrothermal fluids at Date, Chitose, and the Noboribets u geothermal area were dominated by meteoric water. Minor involvement of magmatic water during mineralization at Date cannot be ruled out, b ut evolution of local meteoric water along an evaporation trend and/or an O-18-shift due to hydrothermal rock-meteoric water interaction als o could have produced appropriate fluid compositions. The delta D and delta(18)O values of modern hot-spring waters at Noboribetsu closely p arallel fluid compositions calculated for the clay alteration at Date, Chitose, and Noboribetsu. Because relatively poor reproducibility was obtained for the delta S values of the swelling clays, additional tes ts were conducted. Stepwise heating showed that, for some smectitic cl ays, water evolved between 200 and 300 degrees C had anomalously high delta D values because of residual interlayer water. This error can be minimized by sufficiently long preheating (in vacuo) at less than or equal to 200 degrees C. In vacuo TG patterns of other smectitic clays suggested gradual loss of hydroxyl-groups beginning near 200 degrees C , rather than the more typical distinct separation between interlayer water at <200 degrees C and hydroxyl-groups at >400 degrees C. This be haviour constrains the maximum temperature that can be used for in vac uo preheating. Furthermore, shifts to lower delta D values (by as much as 19 parts per thousand) were obtained when this smectite was disper sed in low-D water for three weeks, perhaps indicating isotopic exchan ge. However, with appropriate care, delta D values obtained by convent ional procedures (including preheating to less than or equal to 200 de grees C) normally reproduced natural compositions of the smectitic cla ys with acceptable accuracy and precision.