A significant part of the hydrocarbons contained in source rocks remains confined within the organic matter -called kerogen -from where they are generated. Understanding the sorption and transport properties of confined hydrocarbons within the kerogens is, therefore, paramount to predict production. Specifically, knowing the impact of thermal maturation on the evolution of the organic porous network is key. Here, we propose an experimental procedure to study the interplay between the chemical evolution and the structural properties of the organic porous network at the nanometer scale. First, the organic porous networks of source rock samples, covering a significant range of natural thermal maturation experienced by the Vaca Muerta formation (Neuquén basin, Argentina), are physically reconstructed using bright field electron tomography. Their structural description allows us to measure crucial parameters such as the porosity, specific pore volume and surface area, aperture and cavity size distributions, and constriction. In addition, a model-free computation of the topological properties (effective porosity, connectivity, and tortuosity) is conducted. Overall, we document a general increase of the specific pore volume with thermal maturation. This controls the topological features depicting increasing accessibility to alkane molecules, sensed by the evolution of the effective porosity. Collectively, our results highlight the input of bright field electron tomography in the study of complex disordered amorphous porous media, especially to describe the interplay between structural features and transport properties of confined fluids. recently been proposed 8,9 as a means to simulate the nano-structural arrangement of the carbon skeletons and their atoms hybridization at different thermal maturation. The nanoporous networks hence modelized, were evidenced to be responsible for the significant adsorption of hydrocarbons 10,11 , the breakdown of continuum hydrodynamics 10 , the occurrence of selfdiffusion governed transport regimes [12][13][14] , and the presence of interfacial wetting effects. 15 These results contributed greatly to the physical understanding of the fast productivity decline of hydrocarbon production wells of source rocks formations. 2,4,5 Such studies, however, only accounted for nanoscale structural pores (diameter ∅ < 2 nm) of the carbon skeleton, which only constitute the lower bound of the pore size distributions described in the literature.Considering the different sizes of pores making up organic porous networks, as experimentally probed in scanning electron microscopy [16][17][18] , small-angle X-ray and neutron scattering [19][20][21][22] , and gas adsorption 21,23,24 , is paramount to cover the mechanisms affecting hydrocarbon production from source rocks.From an experimental perspective, the analysis of gas adsorption isotherms demonstrated that the thermal maturity of the organic matter affects the pore volume and specific surface area. 21,23,24 Analyses of gas adsorption measurements also...