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</html><description>Considering geological time scales, the occurrence of biogenic shale gas in Sweden&#xB4;s crust is relatively young. Geoscientists found that biogenic methane in the Alum Shale in South Sweden formed due to deglaciation around 12 years ago. Moreover, the formation processes were due to complex interactions between neotectonic activity and the occurrence of a deep biosphere.&hellip; Continue reading Untitled</description></oembed>
