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GeoRef Categories
Era and Period
Epoch and Age
Book Series
Date
Availability
Rise and Shine shear zone
Geochemical signatures of mesothermal Au-mineralized late-metamorphic deformation zones, Otago Schist, New Zealand Available to Purchase
Summary of Sb concentrations in the OSB. ( a ) Antimony concentrations in h... Available to Purchase
Geological map of the OSB, with principal structural/metamorphic domains (a... Available to Purchase
General location and regional tectonic map of the Otago Schist belt, South ... Available to Purchase
Map of the Otago region showing the different terranes, extent of regional ... Available to Purchase
Contrasting geochemistry of orogenic gold deposits in Yukon, Canada and Otago, New Zealand Available to Purchase
Age and Origin of Orogenic Gold Mineralization in the Otago Schist Belt, South Island, New Zealand: Constraints from Lead Isotope and 40 Ar/ 39 Ar Dating Studies Available to Purchase
Drilling- and coring-induced artefacts in poorly indurated clays Available to Purchase
Tectonic sequence diagrams and the structural evolution of schists and gneisses in multiply deformed terranes Available to Purchase
Step-Like Delta from Talchir Rocks Around Village Simlipal, Orissa Available to Purchase
Ubiquity of anomalous fading in K-feldspars and the measurement and correction for it in optical dating Available to Purchase
Interpreting structural controls on hydrate and free-gas accumulation using well and seismic information from the Gulf of Mexico Available to Purchase
Three-dimensional Distinct Element Method modelling of the growth of normal faults in layered sequences Available to Purchase
Abstract: The growth of normal faults in mechanically layered sequences is numerically modelled using three-dimensional Distinct Element Method (DEM) models, in which rock comprises an assemblage of bonded spherical particles. Faulting is induced by movement on a pre-defined normal fault at the model base whilst a constant confining pressure is maintained by applying forces to particles lying at the model top. The structure of the modelled fault zones and its dependency on confining pressure, sequence (net:gross) and fault obliquity are assessed using various new techniques that allow (a) visualization of faulted horizons, (b) quantification of throw partitioning and (c) determination of the fault zone throw beyond which theoretical juxtaposition sealing occurs along the entire zone length. The results indicate that fault zones become better localized with increasing throw and confinement. The mechanical stratigraphy has a profound impact on fault zone structure and localization: both low and high net:gross sequences lead to wide and relatively poorly localized faults. Fault strands developing above oblique-slip normal faults form, on average, normal to the greatest infinitesimal stretching direction in transtensional zones. The model results are consistent with field observations and results from physical experiments.