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The dating of shallow faults in the earth crust

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Hidden earthquake faults revealed at Mount Hood, Oregon

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Hidden earthquake faults revealed at Mount Hood, Oregon -

Faults range in length from a few centimetres to many hundreds of kilometres, and displacement likewise may range from less than a centimetre to several hundred kilometres along the fracture surface the fault plane. In some instances, the movement is distributed over a fault zone composed of many individual faults that occupy a belt hundreds of metres wide. The geographic distribution of faults varies; some large areas have almost none, others are cut by innumerable faults. Faults may be vertical, horizontal, or inclined at any angle.
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Difference between Shallow Focus and Deep Focus Earthquakes

Thank you for visiting nature. You are using a browser version with limited support for CSS. To obtain the best experience, we recommend you use a more up to date browser or turn off compatibility mode in Internet Explorer. In the meantime, to ensure continued support, we are displaying the site without styles and JavaScript. But radiometric dating of shallow crustal faulting, which occurs in the crust's brittle regime, has remained difficult 1 , 2 , 3 , 4 because the low temperatures typical of shallow crusted faults prevent the complete syntectonic mineral recrystallization that occurs in deeper faults.
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When stress causes a material to change shape, it has undergone strain or deformation. Deformed rocks are common in geologically active areas. The rocks then have three possible responses to increasing stress: elastic deformation, plastic deformation, or fracturing.
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