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• W2082297586 abstract "Structural geology is concerned with the history of movement in the Earth's crust and the processes by which displacements occur. In the upper one third to one half of deforming continental crust, displacement is accommodated largely by seismic slip increments on existing faults. It follows that earthquakes and related processes are an integral part of structural geology. Traditionally, structural geologists have been preoccupied with the complexity of the finite deformation within fault zones and with the stress states prevailing at the initiation of faults in intact crust. Future structural work should be directed more towards understanding the dynamic character of fault reactivation during incremental slip, and related effects. Questions of interest include rheological and geometrical controls on the initiation, perturbation and termination of ruptures; directivity effects associated with rupture propagation; the recognition of structures resulting from repeated stress cycling within seismogenic crust; and identification of structural features diagnostic of shear stress levels during faulting. Structures arising from the inter-relationships between slip episodes and induced fluid flow are of special importance, because these dynamic fault processes appear influential in the development of much fault-hosted mineralization. Mesothermal gold-quartz lodes hosted in high-angle reverse shear zones of mixed brittle-ductile character form illustrative examples of structures that, arguably, can only be interpreted by seismo-structural analysis embodying the concepts listed above." @default.
• W2082297586 created "2016-06-24" @default.
• W2082297586 creator A5043712271 @default.
• W2082297586 date "1989-01-01" @default.
• W2082297586 modified "2023-10-06" @default.
• W2082297586 title "Earthquake faulting as a structural process" @default.
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• W2082297586 doi "https://doi.org/10.1016/0191-8141(89)90032-1" @default.
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