Basins of extensional and strike|slip settings

Basins of extensional and strike-slip settings - IS MUNI

This account of extensional basin development will be given in terms of continental rifts and passive margins, which are the most common tectonic settings where.

Basins formed by strike-slip tectonics - Geological Digressions

Strike-slip basins form by extension-related subsidence at fault ... extensional, contractional, and strike-slip tectonic settings.

(PDF) Strike-slip basins, Part 1 - ResearchGate

Strike-slip basins are characteristically developing structures along strike-slip faults. They develop in extensional zones and are frequently inverted into ...

Strike-Slip Basins

The processes leading to crustal extension and subsidence in strike-slip settings are generally not as well understood as they are in other ...

Strike-Slip Basin – Its Configuration and Sedimentary Facies

Strike-slip faulting is one of the most important mechanisms of sedimentary basin formation at plate convergent margins, where localized extension can cause ...

The tectonic transition from rifting to strike-slip in the Liaodong Bay ...

Rifting typically forms basins by an extensional process, and it usually ... In contrast, extensional faults in transtensional or strike-slip settings ...

STRIKE-SLIP AND OBLIQUE-SLIP TECTONICS

Large- scale, extensional horsetail splays may host sedimentary basins at tips of major strike-slip faults. Conversely, compressional horsetail splays may ...

Strike-Slip Deformation, Basin Formation and Sedimentation

deform in strike slip settings Some of this work especially new studies ... EXTENSIONAL SETTINGS. Six papers are included in the section on basins in Ex.

Influence of extensional strike-slip fault systems on hydrocarbon ...

Extensional strike-slip basins have unique structural features that influence both sub-sags and traps. Despite previous investigations into ...

Pull-apart basin - Wikipedia

A pull-apart basin is a structural basin where two overlapping (en echelon) strike-slip faults or a fault bend create an area of crustal extension undergoing ...

Strike-slip-basins-Part-1.pdf - ResearchGate

The basins generally form in transtensional settings, local areas of extension along strike- slip faults, and commonly are subsequently inverted in.

Tectono-sequence Evolution of an Extensional Strike-slip ...

The significance of tectonics in shaping sequence stratigraphy within continental rift basins, especially those with extensional strike-slip ...

Extensional and transtensional continental arc basins - Cathy Busby

this is typical of strike-slip basins (see full discus- sion with references ... Busby, C.J., Schermer, E.R., and Mattinson, J.M. (2002). Extensional arc setting ...

Formation and Persistence of Extensional Internally Drained Basins ...

The slickenlines analysis reveals multiple families of slip-vectors and timing of activity, suggesting a change in extension slip-direction from ...

Plate tectonics and basin subsidence history - SERC - Carleton

regional extension or shortening. Different types of basins can form in strike-slip settings, from simple pull-apart basins developed along fault oversteps ...

EXTENSION SYSTEMS - The Web site cannot be found

- intra-continental regions (graben, rifts and extensional basins). Smaller-scale extensional settings ... oblique extensional ramps. Page 18. Tectonics ...

Editorial: Extensional basins associated with collisional tectonics

Nevertheless, understanding the evolution of extensional basins in collisional tectonics is paramount as tectonic inversion can reactivate the basin's dip-slip ...

4D analogue modelling of transtensional pull-apart basins

setting (Fodor, 2007) show that they are oblique-extensional or pure-extensional faults that strike oblique to the main en-echelon fault segments. One of ...

Flexural strike-slip basins | Geology - GeoScienceWorld

Strike-slip faults are classically associated with pull-apart basins where continental crust is thinned between two laterally offset fault ...

Drop-down formation of deep basins along the Dead Sea and other ...

The formation of these basins is usually explained by a pull-apart mechanism that predicts a rhomb-shaped basin geometry bounded by two longitudinal strike-slip ...