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1 Acknowledgments 2 Factors that affect transformation of silica and their bearing on sample selection 2 Preliminary indications of temperature anomalies in siliceous shale caused by serpentinite 3 Geology and tectonics of the Cholame area 3 Degrees of diagenesis 3 General aspects 3 Regional diagenesis 5 Warmspot diagenesis. ^ 5 Intrusive serpentinite as a source of heat 6 References cited 7

Thermal effects of large bodies of intrusive serpentinite on overlying Monterey Shale, southern Diablo Range, Cholame area, California