By Sudipta Sengupta (auth.), S. Sengupta (eds.)
Structural geology has built at a really fast velocity lately. Evolution of Geological constructions in Micro- to Macro-Scales, overlaying a large spectrum of present study in structural geology from the grain scale to the size of orogenic belts and from the brittle to the ductile box, presents an outline of newly rising ideas in one quantity. The booklet covers a variety of advances in such wide fields as hydraulic factures, basic faults, overthrusts, ductile shear zones, rock materials, folds, superposed folds and basement structures.
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Extra info for Evolution of Geological Structures in Micro- to Macro-scales
12(b) and (c) and 1000 m in diameter. 10. 7(c), namely 21 Hydraulic fractures and their implications Strike of Palaeoslope \ Upper tier 1----1____ s Undeformed ············.. 10 A structural synopsis of a three-dimensional seismic survey of block 30119, located in the basin centre, showing a polygonal network of small extensional faults affecting the lower Tertiary. From Cartwright (1994). a uniform horizontal stress and the maximum principal compression vertical. 12) that analogue models involving the formation of desiccation fractures under a variety of different boundary conditions could provide a powerful tool to support theoretical studies into the organization of hydraulic fractures that might be expected to occur in different sites within a basin or in sedimentary successions in general.
Stage 4 is when the relay ramp is destroyed to produce a single fault which has an along-strike bend. 6). A branch line between normal faults or an alongstrike bend may represent a stage 4 relay, with Relay ramps and transfer zones eomm n U U2lOmm o timon ---- 3IOmm U'3Dmm a) 10m e) ,/' b) u ~ - == Skin u 95mm ......... 1 kin d) ... -----~m ===:J ~ g) U 1 m o -=t;:;J.. 3 Examples of fault segmentation at varying scales: (a) Beryl embayment, North Sea, UK; (b) active fault traces (Tobin and Pearce faults) in the Central Nevada (after Jackson and Leeder, 1994, fig.
1 Summary of the main features of the various models for fault displacement Model Rationale d-x profile r/dMAX ratio Single slip event in an ideal elastic material (Pollard and Segall, 1987) Displacement depends on the driving stress, the elastic properties of the rock, fault length and the distance from the fault centre Semi-circular Controlled by the driving stress and the elastic properties of the rock Cumulative slip model (Walsh and Watterson, 1987) Displacement builds up by a series of slip events, each obeying the ideal elastic model Approximately linear after about 100 slip events Post-yield fracture mechanics model (Cowie and Scholz, 1992a, 1992c) Inelastic deformation occurs at fault tips Approximately semicircular, but tapering at fault tips Cowie and Scholz (1992a, 1992c) suggest that r a dMAX Modelling of Biirgmann et al.