Implications for Investigations of Stray Gas Migration: Geochemistry of Natural Gases in Quaternary through Devonian Age Strata in the Northern Appalachian Basin
More than 2,000 gas samples were analyzed and evaluated for molecular and isotope geochemistry to determine gas origin, mixing, and thermal maturity. Samples were collected throughout the stratigraphic section from Quaternary to Middle Devonian deposits in northeastern Pennsylvania from mud gas samples during drilling of Marcellus formation gas wells, and during background groundwater water quality testing programs. Evaluation of our geochemical database reveals microbial, mixed microbial/thermogenic and thermogenic gases occur in some shallow aquifer systems that pre-date drilling activity in the Marcellus Formation. The data reveal a complex thermal history with distinct thermogenic gases, gas mixtures, and isotope reversals (ä13C1>ä13C2>ä13C3) throughout the stratigraphic section. Defining a specific source of stray natural gas migration requires the investigation and synthesis of different data types at a site specific level. Molecular and isotope geochemistry provides evidence of gas origin, and focus for investigations where pre-existing and multiple potential stray gas sources occur.
Echelon Applied Geoscience Consulting, Murrysville, PA