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Showing 1 to 20 of 46 for “"slip faults"”.

  1. Structural analysis of brittle deformation features along Grenvillian shear zones in southeastern Ontario

    … highs in Paleozoic cover above the RLmz. Normal faults striking NW to WNW and ESE-striking dextral strike-slip faults in the RLmz and Paleozoic cover above both shear zones are compatible with Ordovician-Devonian Taconic and Acadian stresses. Prominent NNE- and NW-striking subvertical joint sets …

    queens Repository record for Structural analysis of brittle deformation features along Grenvillian shear zones in southeastern Ontario (opens in a new tab)

  2. Reevaluation of the southwestern end of the Salem synclinorium

    … between veins, fractures, slickensides, oblique-slip faults and thrusts in a riverbed exposure within the southwestern portion of the Salem synclinorium, offers a structural model for the Salem synclinorium. Thrusting induced extensional fractures and veins. Oblique-slip faults which cut the …

    vt Repository record for Reevaluation of the southwestern end of the Salem synclinorium (opens in a new tab)

  3. A PALAEOMAGNETIC STUDY OF CRUSTAL ROTATIONS AND THEIR RELATIONSHIP TO THE TECTONICS OF THE ATACAMA AND DOMEYKO FAULT SYSTEMS, NORTHERN CHILE

    … palaeomagnetic analysis from within two strike-slip fault systems in northern Chile (25.4°S - 26.4°S); the Atacama Fault System in the Coastal Cordillera, and the Domeyko Fault System in the Andean pre-Cordillera. In the Coastal Cordillera, analysis of Middle Jurassic lavas (La Negra Formation) …

    plymouth Repository record for A PALAEOMAGNETIC STUDY OF CRUSTAL ROTATIONS AND THEIR RELATIONSHIP TO THE TECTONICS OF THE ATACAMA AND DOMEYKO FAULT SYSTEMS, NORTHERN CHILE (opens in a new tab)

  4. Geologic mapping and zircon (U-Th)/He thermochronology of the Avawatz Mountains, California; Implications for the eastern terminus of the Garlock fault

    … are located at the eastern tip of the left-slip Garlock fault where the fault intersects the NW-striking right-slip Southern Death Valley fault (SDVF). The Avawatz Mountains were constructed via late Cenozoic contractional deformation involving active thrust and/or oblique-slip faults. …

    unr Repository record for Geologic mapping and zircon (U-Th)/He thermochronology of the Avawatz Mountains, California; Implications for the eastern terminus of the Garlock fault (opens in a new tab)

  5. Development and interaction of segmented fault systems

    Faults in contractional and extensional settings have been studied, both during fieldwork and from interpretation of 2D and 3D seismic sections. Detailed analysis of the geometries of faults, with displacements of a few mm to 100's m, has provided insights into the development of fault networks. …

    soton Repository record for Development and interaction of segmented fault systems (opens in a new tab)

  6. Partitioning of fluid flow along faults and fractures in the Bristol Channel Basin: implications for low carbon geoscience projects in SW England

    … slickenfibres within normal, thrust, and strike-slip faults in the East<br/>Quantoxhead and Kilve region of Somerset.<br/>Protracted N-S extension (ca. 150–120 Ma) formed normal faults, while subsequent NS shortening (ca. 50–20 Ma) involved (i) cross-cutting strike-slip faults, (ii) minor …

    plymouth Repository record for Partitioning of fluid flow along faults and fractures in the Bristol Channel Basin: implications for low carbon geoscience projects in SW England (opens in a new tab)

  7. Seismic tomography and surface deformation in Krýsuvík, SW Iceland

    … time, our relocation result delineates strike-slip and dip-slip faults above and around this low velocity zone. Brittle-ductile transition is delineated based on the distribution of the earthquakes in this area. In order to understand the relation between the subsurface structure and the …

    mit Repository record for Seismic tomography and surface deformation in Krýsuvík, SW Iceland (opens in a new tab)

  8. Structural analysis of the valley and ridge extension of the Parsons Lineament

    … joints and second—order, sinistral strike-slip faults. Two sets of regional joints occur : J1, a pervasive east—west— trending, near vertical joint set, and J2 which varies with structural position. Peaks in J1 intensity coincide with known strike-slip faults and pronounced photolineaments. …

    vt Repository record for Structural analysis of the valley and ridge extension of the Parsons Lineament (opens in a new tab)

  9. Evolution of tectonic and stratigraphic geometries in the Southern Outeniqua Basin

    … based on the geographical position of these faults. Sequence stratigraphic analysis of the basin lead to the identification of seven secondorder unconformities which have been further defined into five main seismo-stratigraphic units. The variation in major structural orientations suggest the …

    cape-town Repository record for Evolution of tectonic and stratigraphic geometries in the Southern Outeniqua Basin (opens in a new tab)

  10. Tectonic significance of the Atnarko complex, Coast Mountains, British Columbia

    … while to the southeast large dextral strike-slip faults dominate. Relative plate motions between ca. 70-60 Ma indicate that dextral transpression occurred between the Kula and North American plates. Strain during this transpressive deformation was partitioned into compressive and …

    ubc Repository record for Tectonic significance of the Atnarko complex, Coast Mountains, British Columbia (opens in a new tab)

  11. Structural Geology of the Caddo Gap Area, Ouachita Mountains, Arkansas

    … unmapped, northeast-trending strike-slip faults in the Arkansas Novaculite were discovered on the east-west “South Ridge” immediately south of and adjacent to the South Caddo Mountain fold. This style of faulting differs significantly from previous regional interpretations (Haley et …

    sfasu Repository record for Structural Geology of the Caddo Gap Area, Ouachita Mountains, Arkansas (opens in a new tab)

  12. Fault Behavior and Kinematic Evolution of the Eastern California Shear Zone

    … wide and complex network of right-lateral strike-slip faults, is not well understood, despite hosting three large (>Mw 7.0) earthquake ruptures in recent decades. The low-net slip faults of the ECSZ (each with <10 km) offer a unique opportunity to assess strain distribution in a developing, …

    vt Repository record for Fault Behavior and Kinematic Evolution of the Eastern California Shear Zone (opens in a new tab)

  13. Thermal and mechanical development of the East African Rift System

    … fault system. These basins are linked by oblique-slip and strike-slip faults cross-cutting the rift valley. Faults bounding the Kenya and Western rift valleys delineate two north-south-trending, 40-75 km wide zones of crustal extension, and little or no crustal thinning has occurred beneath the …

    woods-hole Repository record for Thermal and mechanical development of the East African Rift System (opens in a new tab)

  14. Thermal and mechanical development of the East African Rift System

    … fault system. These basins are linked by oblique-slip and strike-slip faults cross-cutting the rift valley. Faults bounding the Kenya and Western rift valleys delineate two north-south-trending, 40-75 km wide zones of crustal extension, and little or no crustal thinning has occurred beneath the …

    mit Repository record for Thermal and mechanical development of the East African Rift System (opens in a new tab)

  15. Geology of part of the Inchelium Quadrangle, Stevens County, Washington

    … Northwest- and northeast-trending strike-slip faults displace the normal faults and also the folds. The area is covered in part by glacial debris, alluvium and colluvium.</p>

    eastern-wash Repository record for Geology of part of the Inchelium Quadrangle, Stevens County, Washington (opens in a new tab)

  16. Structure of the Patagonian fold-thrust belt in the Magallanes region of Chile, 53° - 55° S Lat.

    … tectonic superposition of a left-lateral strike-slip plate margin defined by the Magallanes- Fagnano fault zone. In this dissertation, I present new geologic maps, cross sections and detailed macro- and microscopic structural analyses that describe the geometry and kinematic evolution of the …

    texas Repository record for Structure of the Patagonian fold-thrust belt in the Magallanes region of Chile, 53° - 55° S Lat. (opens in a new tab)

  17. Building Velocity Models for Steep-Dip Prestack Depth Migration through First Arrival Traveltime Tomography

    … of sedimentary basins, such as major strike-slip faults, seismic reflectivity is often sparse and little is known of detailed subsurface geology. Alternate methods of velocity model construction must be used. First arrival (refraction and turning ray) traveltime tomography is proposed to …

    vt Repository record for Building Velocity Models for Steep-Dip Prestack Depth Migration through First Arrival Traveltime Tomography (opens in a new tab)

  18. Different styles of deformation of the fore-arc wedge along the Chilean convergent margin : insights from 3D numerical experiments

    … starved trench. Two major margin parallel strike slip faults are observed in this area, the Atacama Fault Zone (AFZ) and the Precordilleran Fault System (PFS). Both strike-slip faults do not exhibit significant recent displacement. The southern study area (37° - 42°S), compared to the northern …

    potsdam-diss Repository record for Different styles of deformation of the fore-arc wedge along the Chilean convergent margin : insights from 3D numerical experiments (opens in a new tab)

  19. Present day plate boundary deformation in the Caribbean and crustal deformation on southern Haiti

    … marked by subduction and large intra-arc strike-slip faults, are a natural laboratory for the study of strain partitioning and interseismic plate coupling in relation to large earth- quakes. In this work, I use the available campaign and continuous GPS measurements in the Caribbean to derive a …

    purdue-thes Repository record for Present day plate boundary deformation in the Caribbean and crustal deformation on southern Haiti (opens in a new tab)

  20. Structural style of the San Francisco Mountains, Sevier fold-thrust belt, Utah

    … sheets that are overprinted by extensional faults, distorting correlations of geologic structures in the region. The Frisco thrust is exposed within the San Francisco Mountains in west-central Utah. Correlations with the better studied Canyon Range-Willard thrust to the north and the Wah Wah …

    missouri Repository record for Structural style of the San Francisco Mountains, Sevier fold-thrust belt, Utah (opens in a new tab)

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