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Comparison of Foreland Basin Sequences: The Trenton Group in Southern Quebec and Central New York

Charlotte J. Mehrtens
Charlotte J. Mehrtens
University of Vermont Burlington, Vermont
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January 01, 1988


Numerous high-angle faults that were active during deposition are recognizable within the autochthonous, Upper Ordovician, Trenton Group ramp sequence in southern Quebec/The facies of the Trenton Group in southern Quebec can be compared to those in New York and can be shown to be controlled by proximity to, or position within, the Taconic foreland basin.

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AAPG Studies in Geology

The Trenton Group (Upper Ordovician Series) of Eastern North America: Deposition, Diagenesis, and Petroleum

Brain D. Keith
Brain D. Keith
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American Association of Petroleum Geologists
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Publication date:
January 01, 1988




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