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利用西宾夕法尼亚和东俄亥俄州22口气井、5个岩心的气体样品,采取稳定同位素地球化学方法解释了阿巴拉契亚中央高原区天然气体的成因及与其可能来源的相关性,并评价这一方法的可行性。
Using gas isotope geochemistry of five core gas samples from 22 gas wells in western Pennsylvania and eastern Ohio, the origin of natural gas in the Appalachian Central Highlands and its possible sources were explained and evaluated Feasibility of the method.