Pull-apart basin

Pull-apatr in transform faults

Нормальный Разлом

Реверсный Разлом (надвиг)

Strik-slip -сдвиг

Strik-slip -сдвиг

Толчковые Разломы Натяжения

Thrust -Толчковые Разломы Натяжения, шарьяж,покров

Torbay thrust

Strik-slipe transform fault (San Andreas)

Array of extensional faults cutting Triassic to Lower Jurassic Blomidon Formation rocks, near Clarke Head, Nova Scotia.Экстенсиональный разлом (extensional fault) – разлом, который вертикально сужает и горизонтально расширяет части земной коры и большинстве случаев такой разлом является нормальным разломом, но может быть и обратным имея более мелкую геометрию, обычно связанную с разломами, происходящими при трастовом разломе. Экстенсиональные разломы имеют вид плоскости и пока область напряжения ( http://en.wikipedia.org/wiki/Stress_field) ортогональна к поверхности Земли, разлом имеет падение 60 °, типично продолжаясь вниз как сейсмогеничный слой.

Detachment fault

Detachment faulting - Wheeler Peak, Snake Range, Nevada, is one of the tallest peaks within the Great Basin

Example of listric faults known as slumps. Hanging wall blocks rotate and slide along the entire fault plane.

The evolution of a listric fault

Listric fault

Nappes: These folds are part of the Musconetcong Nappe within the Reading Prong nappe megasystem in Lehigh County. The light-colored dolomite deformed mainly by flexural slip, while the dark-colored limestone beds deformed by flow.

Prerif-Nappe, Morokko.Section through the thrust of the "Prerifain Rides".

http://www.earthsci.unibe.ch/tectonics/nrp20.htm

http://tierra.rediris.es/TASYO/area.html - Morokko:The Betic-Rifian accretionary prismThe "Off-shore" Betic-Rifian accretionary prism: A step from passive to active margin The "Off-shore" Betic-Rifian accretionary prism: A step from passive to active margin -

Collisionas tecktonics: Triassic strata in Svalbard folded during Tertiary deformation

Cross section showing thin-skinned character of thrust stack associated with the Appalachian mountains. The blue layer has been repeated several times by cutting and stacking the pieces. In a thin-skinned style sub-horizontal detachments dominate, and the rocks at different levels are deforming in very differeent ways. In other words one level is detached from the other. The authochthonous basement rocks referred to here are basically undeformed, while a stack of thrust sheets exists above. Interestingly, here the rocks involved are crystalline basement rocks, whereas in many other localities stratified platform cover rocks tend to show this structural style

nappe

Nappe: Himalaya

Nappe of mo-clay formation, Hanklit, island of Fur, Denmark

Ductile thrust faulting and large-scale fold nappes producedwhen the Archean Wyoming and Superior provinces collided during the Paleoproterozoic Trans-Hudson orogeny. Theseoutcrops along the Laramie River of southeastern Wyoming contains layers of granitic gneiss and amphibolite

Vergence

strike-slip

Detachment

Normal fault

Reverse fault -http://www.uwsp.edu/geo/faculty/hefferan/geol320/reversefaults.html

strik-slip

Sudan collision suture

Keystone detachment reverse thrust, B&R

http://en.wikipedia.org/wiki/Thrust_tectonics

Keystone thrust

Strike-sleep fault

King''s Bowl lava field and the Great Rift zone of extension. The King’s Bowl (the giant hole) is a phreatic explosion pit, where magma erupting at the surface, Idaho, U.S.A

thrust

Detachment: Savahia Peak in the Whipple Mountains, CA.

Accretion bulldozer

Duplex, Japan

Extension fracture, Pamun Dome, CA

Thrust

Pull Apart

Ramp Fold British Columbia

Extensional fault