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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Egypt
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Sinai Egypt (2)
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Southern Africa
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Primary terms
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Africa
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Asia
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Korea
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Atlantic Ocean
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gouge
Fault rock structure-related stiffness contrast explains earthquakes in creeping faults
Integrated geologic and geophysical modeling across the Bartlett Springs fault zone, northern California (USA): Implications for fault creep and regional structure
Atomic-scale interlayer friction of gibbsite is lower than brucite due to interactions of hydroxyls
Structural evolution of the reactivated Møre–Trøndelag Fault Complex, Fosen Peninsula, Norway
Melting of fault gouge at shallow depth during the 2008 M W 7.9 Wenchuan earthquake, China
How clay delamination supports aseismic slip
Repeated brittle reactivations of a pre-existing plastic shear zone: combined K–Ar and 40 Ar– 39 Ar geochronology of the long-lived (>700 Ma) Himdalen–Ørje Deformation Zone, SE Norway
Fault surface morphology as an indicator for earthquake nucleation potential
Structural traps and seals for expanding CO 2 storage in the northern Horda platform, North Sea
Fault zone architecture and lithology-dependent deformation mechanisms of the Himalayan frontal fold-thrust belt: Insights from the Nahan Thrust, India
Time-constrained multiphase brittle tectonic evolution of the onshore mid-Norwegian passive margin
Gouge fabrics reset by thermal pressurization record stress on faults after earthquakes
Grain-size-reducing- and mass-gaining processes in different hydrothermal fault rocks
History of earthquakes along the creeping section of the San Andreas fault, California, USA
Eocene fault-controlled fluid flow and mineralization in the Paradox Basin, United States
Seismic fault weakening via CO 2 pressurization enhanced by mechanical deformation of dolomite fault gouges
Complete Strain Record of a Highly Asymmetric Shear Zone: From Fault Core Gouges to Surface Rupture of Historical Earthquakes in the Alhama de Murcia Fault (SE Iberian Peninsula)
Syncing fault rock clocks: Direct comparison of U-Pb carbonate and K-Ar illite fault dating methods
Discussion on ‘Fault seal modelling – the influence of fluid properties on fault sealing capacity in hydrocarbon and CO 2 systems’, Petroleum Geoscience , 2020, https://doi.org/10.1144/petgeo2019-126
Fault seal behaviour in Permian Rotliegend reservoir sequences: case studies from the Dutch Southern North Sea
Abstract Permian Rotliegend reservoir rocks are generally characterized by high net/gross (N/G) ratios, and faults in such sand-dominated lithologies are typically not considered likely to seal. Nevertheless, many examples of membrane sealing are present in Rotliegend gas fields in the Southern Permian Basin. This manuscript reviews examples of membrane sealing in the Dutch Rotliegend; it presents an extensive dataset of petrophysical properties of Rotliegend fault rocks and analyses two case studies using commonly used workflows. Fault (membrane) seal studies have been carried out on two Rotliegend fields to test the level of confidence and uncertainty of prediction of ‘across fault pressure differences’ (AFPD) based on existing SGR-based algorithms. From the field studies it is concluded that observable small AFPDs are present and that these are likely pre-production AFPDs due to exploration-time scale trapping and retention of hydrocarbons. Two shale gouge ratio (SGR)-based empirical algorithms have been used here to estimate AFPDs in lower N/G reservoir intervals with the aim of predicting membrane seal behaviour, and these results are compared to field data. It is concluded the selected SGR-based tools predict AFPD for Upper Rotliegend lower N/G reservoir rocks with reasonable results. Nonetheless, the core sample datasets show a much wider range of permeability and capillary entry pressure than predicted by the selected SGR transforms. This highlights the potential to modify existing workflows for application to faults in high N/G lithologies. Data sharing and collaboration between industry and academics is encouraged, so that in the long run workflows can be developed specifically for faults in high N/G lithologies.