about
Natural gas: Should fracking stop?Capillary tension and imbibition sequester frack fluid in Marcellus gas shale.Comment on "Predictors of Indoor Radon Concentrations in Pennsylvania, 1989-2013".Thickness trends and sequence stratigraphy of the Middle Devonian Marcellus Formation, Appalachian Basin: Implications for Acadian foreland basin evolutionFluid evolution history of brittle-ductile shear zones on the hanging wall of Yellow Spring thrust, Valley and Ridge Province, Pennsylvania, U.S.APancake joints in Utica gas shale: Mechanisms for lifting overburden during exhumationFormation of spaced cleavage and folds in brittle limestone by dissolutionClassification of solution cleavage in pelagic limestonesThe relationship between pencil cleavage and lateral shortening within the Devonian section of the Appalachian Plateau, New YorkThe fate of residual treatment water in gas shaleRole of pressure solution and dissolution in geologyA model describing flowback chemistry changes with time after Marcellus Shale hydraulic fracturingThe concept of joint saturation and its applicationSequence stratigraphy and depositional environments of the Shamokin (Union Springs) Member, Marcellus Formation, and associated strata in the middle Appalachian BasinCorrelation between abnormal pore pressure and tectonic jointing in the Devonian Catskill DeltaEarly jointing in coal and black shale: Evidence for an Appalachian-wide stress field as a prelude to the Alleghanian orogenyCharacterization of Appalachian faultsAnalysis of pinnate joints in the Mount Desert Island granite: Implications for postintrusion kinematics in the coastal volcanic belt, MaineFossil distortion and décollement tectonics of the Appalachian PlateauVeins in the Lockport dolostone: Evidence for an Acadian fluid circulation systemCurving cross joints and the lithospheric stress field in eastern North AmericaHeterogeneous hydrofracture development and accretionary fault dynamics: Comment and ReplyInfluence of poroelastic behavior on the magnitude of minimum horizontal stress, Sh in overpressured parts of sedimentary basinsTectonic implications drawn from differences in the surface morphology on two joint sets in the Appalachian Valley and Ridge, VirginiaKinematic implications of joint zones and isolated joints in the Navajo Sandstone at Zion National Park, Utah: Evidence for Cordilleran relaxationThe feedback between joint-zone development and downward erosion of regularly spaced canyons in the Navajo Sandstone, Zion National Park, UtahInfluence of tectonic exhumation on porosity of Wufeng–Longmaxi shale in the Fuling gas field of the eastern Sichuan Basin, ChinaDeformation associated with the movement of the Muddy Mountain overthrust in the Buffington window, southeastern NevadaDetecting and explaining why aquifers occasionally become degraded near hydraulically fractured shale gas wellsThe role of salt in fold-and-thrust beltsOn the use of regional joint sets as trajectories of paleostress fields during the development of the Appalachian Plateau, New YorkJoint sets that enhance production from Middle and Upper Devonian gas shales of the Appalachian BasinLoading paths to joint propagation during a tectonic cycle: an example from the Appalachian Plateau, U.S.AFactors controlling joint spacing in interbedded sedimentary rocks: integrating numerical models with field observations from the Monterey Formation, USAIs there a genetic relationship between selected regional joints and contemporary stress within the lithosphere of North America?Development of cleavage in limestones of a fold-thrust belt in eastern New York
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P50
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