This book describes four different methods of paleotemperature
assessment on selected Paleozoic rock units and determines spatial
variations in maximum burial depths of these units and thicknesses
of lost overburden. Stratigraphic and tectonic history of the
northern Appalachian basin is described in details followed by a
critical review of fluid inclusion, clay diagenesis, organic
maturation, and stable isotope techniques of paleotemperature
measurements in sedimentary rocks.
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