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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
bleaching
Genetic association between carbonates and gold precipitation mechanisms in the Jinshan deposit, eastern Jiangnan orogen Available to Purchase
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 Available to Purchase
Geometry optimization of an electrochemical reactor for bleaching kaolin Available to Purchase
Complex Rupture of the 2015 M w 8.3 Illapel Earthquake and Prehistoric Events in the Central Chile Tsunami Gap Available to Purchase
Hydrogeochemical evolution of formation waters responsible for sandstone bleaching and ore mineralization in the Paradox Basin, Colorado Plateau, USA Available to Purchase
Eocene fault-controlled fluid flow and mineralization in the Paradox Basin, United States Available to Purchase
Photosymbiosis in planktonic foraminifera across the Paleocene–Eocene thermal maximum Available to Purchase
Optimization of bleaching power by sulfuric acid activation of bentonite Open Access
Fault zone architecture and its scaling laws: where does the damage zone start and stop? Open Access
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.