The Kimmeridge Clay Formation is regarded as a model of the formation of hydrocarbon source rocks. In Lake Bouchet, organic matter appears to be a good indicator of palaeoenvironmental changes occurring for over 350,000 years. This book should be of interest to geologists and geochemists interested in organic matter accumulation.
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I don't know how you got a book printed 26 years ago in the conditions that I received it (like new) but you do it! ABSOLUTELY AWESOME!
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