“…The Eimer and Amend SrC0 3 isotope standard was analysed eight times and has an 87Sr/8 6S r ratio of 0'70805 ±O·00020 (I (7). This value is in excellent agreement with results published by other investigators (Brookins et al 1975;Burwell 1975). The concentrations of quartz, feldspar, illite, and kaolinite-chlorite were estimated from X-ray diffraction patterns (Cu K-alpha X-radiation, Diano Corp., Model XRD-6) based on calibrations described by Boger & Faure (1976).…”