Petroleum in shale reservoirs is hosted in organic matter and mineral pores as well as in natural fractures and voids. For thermally mature plays, e.g., the Marcellus Shale, methane and other light alkane gases are thought to be primarily contained in organic matter pores with radii <= 50 nm. Thus, in order to understand natural gas occurrence, transport, storage, and recoverability within unconventional reservoirs at the dry-gas stage of thermal maturity, it is critical to characterize the associated organic matter porosity across length scales from 50 nm down to the angstrom level. We utilized wide Q-range neutron total scattering to characterize perdeuterated methane (CD4) adsorption at 60 degrees C up to the zero average contrast (ZAC) pressure (similar to 60 MPa) within two mineralogically different samples collected from the same producing interval from the Middle Devonian Marcellus Shale. The neutron scattering approach used here provides structural information from the interatomic regime up to a nominal pore radius of similar to 12.5 nm and, by reaching the CD(4)ZAC pressure (similar to 60 MPa), it is possible to examine the distribution of open versus closed pores within this pore size range in the samples. Our results indicate that similar to 10% of the largest pores measured are closed to CD4 for a quartz-rich sample whereas up to 25% of pores with a nominal radius of similar to 12.5 nm are inaccessible within a sample with an equivalent proportion of quartz, carbonate, and clay. As pore size decreases, accessibility also decreases; all pores with radii similar to 0.5 nm are effectively closed to CD4 in both samples. Additionally, up to similar to 4.5x more CD4 is adsorbed within the quartz-rich sample at 60 MPa and we see no evidence for densification of CD4 within the shale pores. These findings suggest that for shale samples within the dry-gas window, (i) nanometer-scale porosity is primarily located within organic matter, (ii) the amount of available nanoporosity can vary widely over meter scales, and (iii) mineralogy plays a secondary role in dictating methane behavior within these systems.