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Learn about different types of faults, their characteristics, and terminology in geology. This article explores normal faults, fault zones, offset stratigraphy, scarp patterns, and tectonic environments of faulting.
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Faults, especially Normal January 18, 2005
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Know These Terms • Footwall vs. Hanging wall • Fault plane vs. Fault zone vs. Shear zone • Offset: • Normal vs. thrust/reverse vs. strike-slip vs. oblique • Heave and throw • True vs. apparent
Normal Fault Terms • Scarp • Offset stratigraphy on maps and in drill cores • Triangular Facets • Offset streams • Two models - Horsts and Grabins • Termination
Normal fault scarp with indurated brecciaBreccia on normal fault. Quaternary Klamath Lake Ore. Note colluvial deposit against fault scarp. Smoother areas of fault show finer gouge that has not been weathered out from between breccia-size fragments.
Slickenlines on hanging wall. Note brecciated textures above and below slickenlined gouge face.
Indurated breccia on detachment surface. Note coarse lineation parallel to pen.
Tectonic Environments of Normal Faulting • Continental Rifting • Oceanic Spreading Ridges - Mid Ocean Basins • Sedimentary Basins - Compaction and gravitational collapse • Pull-apart basins - TRANSTENSION
Detachment surface in Whipple Mtns. Gneissic basement complex below. Young volcanic rocks and scraps of basement above.