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Paradox Basin
Hydraulic fracturing in the overpressured, isotropically stressed Cane Creek Unit, Paradox Basin
Hydrologic windows into the crystalline basement and their controls on groundwater flow patterns across the Paradox Basin, western USA
Hydrocarbon-induced bleaching and copper mineralization in the Wingate Sandstone, Paradox Valley, Colorado: Two episodes of fluid migration during the evolution of the Paradox Basin
Hydrogeochemical evolution of formation waters responsible for sandstone bleaching and ore mineralization in the Paradox Basin, Colorado Plateau, USA
Eocene fault-controlled fluid flow and mineralization in the Paradox Basin, United States
Detrital zircon geochronology and provenance of the Middle to Late Jurassic Paradox Basin and Central Colorado trough: Paleogeographic implications for southwestern Laurentia
Organic geochemistry at varying scales: from kilometres to ångstroms
Abstract Petroleum geochemistry has historically relied on the analysis of field samples – source rocks, oils and gases. Data collected for individual samples are considered characteristic of a specific geographical location and geological position that, when aggregated with data from other samples, can be extrapolated to larger scales. These scale-ups may be as small as a few metres, such as a detailed characterization of source rocks penetrated by a single well, to global, such as petroleum systems that now span continents due to plate tectonics. However, a single sample contains a wealth of information at smaller scales. In situ analytical techniques have improved significantly over the last decade, allowing us to examine sedimentary rocks at ever higher spatial (areal and temporal) resolution. Mass spectrometric imaging is an emerging, enabling technology that can be performed at c. 200 µm (matrix-assisted laser desorption) to 50 nm (nanoSIMS) resolution. X-ray microcomputed tomography (µ-CT) is being applied to examine the storage and transport of petroleum in low-permeability shales and carbonates at spatial resolutions as low as c. 8 µm. Pore architecture in shale, both organic and inorganic, can be modelled from small-angle neutron scattering (SANS) data and imaged directly with helium ion microscopy at c. 1 nm resolution. Atomic force microscopy (AFM) can now resolve the molecular structure of individual asphaltene molecules. Information obtained with these techniques is now revealing the fundamental nature of geological organic materials, opening the span of petroleum geochemistry from atoms to continents.
Fault zone architecture and its scaling laws: where does the damage zone start and stop?
Abstract Damage zones of different fault types are investigated in siliciclastics (Utah, USA), carbonates (Majella Mountain, Italy) and metamorphic rocks (western Norway). The study was conducted taking measurements of deformation features such as fractures and deformation bands on multiple 1D scanlines along fault walls. The resulting datasets are used to plot the frequency distribution of deformation features and to constrain the geometrical width of the damage zone for the studied faults. The damage-zone width of a single fault is constrained by identifying the changes in the slope of cumulative plots made on the frequency data. The cumulative plot further shows high deformation frequency by a steep slope (inner damage zone) and less deformation as a gentle slope (outer damage zone). Statistical distributions of displacement and damage-zone width and their relationship are improved, and show two-slope power-law distributions with a break point at c. 100 m displacement. Bleached sandstones in the studied siliciclastic rocks of Utah are associated with a higher frequency of deformation bands and a wider damage zone compared to the unbleached zone of similar lithology. Fault damage zones in the carbonate rocks of Majella are often host to open fractures (karst), demonstrating that they can also be conductive to fluid flow.
Provenance of Pennsylvanian–Permian sedimentary rocks associated with the Ancestral Rocky Mountains orogeny in southwestern Laurentia: Implications for continental-scale Laurentian sediment transport systems
Controls on the structural and stratigraphic evolution of the megaflap-bearing Sinbad Valley salt wall, NE Paradox Basin, SW Colorado
Effective stress constraints on vertical flow in fault zones: Learnings from natural CO 2 reservoirs
A comparison of the relationship between measured acoustic response and porosity in carbonates across different geologic periods, depositional basins, and with variable mineral composition
Megaflaps adjacent to salt diapirs
Provenance of a Permian erg on the western margin of Pangea: Depositional system of the Kungurian (late Leonardian) Castle Valley and White Rim sandstones and subjacent Cutler Group, Paradox Basin, Utah, USA
Rapid river incision across an inactive fault—Implications for patterns of erosion and deformation in the central Colorado Plateau
Man-made versus natural CO 2 leakage: A 400 k.y. history of an analogue for engineered geological storage of CO 2
Clustering revisited: A spectral analysis of microseismic events
Sequence Stratigraphic Evolution and Cyclicity of An Ancient Coastal Desert System: The Pennsylvanian–Permian Lower Cutler Beds, Paradox Basin, Utah, U.S.A
Load-induced subsidence of the Ancestral Rocky Mountains recorded by preservation of Permian landscapes
Abstract The Southwest Carbon Partnership (SWP), one of seven United States Department of Energy-funded Regional Carbon Sequestration Partnerships, has been tasked with assessing the CO 2 sequestration potential within the southwestern United States. Carbon dioxide is considered a ‘greenhouse’ gas and is emitted, in large volumes, by the burning of fossil fuels and other industrial processes. CO 2 capture from point source emitters and subsequent geological sequestration is being considered as a viable short- to intermediate-range mitigation option to combat the phenomena of global warming. Significant fossil fuel reserves and consumers exist within the seven member states of the SWP and, as such, the Partnership is dedicating a large amount of resources to the challenges posed by large-scale CO 2 sequestration. Three distinct phases of work have been or will be performed by the SWP: a Characterization Phase to identify carbon capture and sequestration potential; a Validation Phase to test small-scale field injection of CO 2 ; and a Deployment Phase to test commercial-scale field injection of CO 2 . Each phase presents challenges and opportunities to the refinement of the best approach to safe and efficient geological storage of CO 2 within the SW region of the United States.