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Horse (geology)

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Diagram showing development of thrust-bounded horses within a thrust duplex
A horse sits between the walls of thisnormal faultlocated nearUpheaval Dome,Utah.Thefault planetraces from the upper right to the lower left of the image. The horse is the broad lens-shaped feature in the rock defined by the splitting and rejoining of the trace of the fault plane.

Ahorse,ingeology,is any block ofrockcompletely separated from the surrounding rock either bymineral veinsorfault planes.Inmining,a horse is a block ofcountry rockentirely encased within a minerallode.[1]Instructural geologythe term was first used to describe the thrust-bounded imbricates found within athrust duplex.[2]In later literature it has become a general term for any block entirely bounded by faults, whether the overall deformation type iscontractional,extensionalorstrike-slipin nature.[3][4]

References

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  1. ^Butler, F.H. 1911. The brecciation of mineral veins.
  2. ^Dennis, J.G. 1967. International tectonic dictionary. AAPG Memoir 7, 196pp.
  3. ^Root, K.G. 1990. Extensional duplex in the Purcell Mountains of southeastern British Columbia. Geology, 18, 419-421
  4. ^Laney, Stephen E; Gates, Alexander E (1996), "Three-dimensional shuffling of horses in a strike-slip duplex: an example from the Lambertville sill, New Jersey",Tectonophysics,258(1–4): 53–70,Bibcode:1996Tectp.258...53L,doi:10.1016/0040-1951(95)00173-5
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