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Magallanes-Fagnano Fault

From Wikipedia, the free encyclopedia
Continental transform fault between the Scotia plate and the South American plate

TheMagallanes–Fagnano Fault (Spanish:Falla Fagnano–Magallanes) is a continentaltransform fault.[1] The fault marks atransform boundary between theScotia plate and theSouth American plate, cutting acrosscontinental crust.[2] It runs under theStrait of Magellan's western arm,Almirantazgo Sound andFagnano Lake.

It has been suggested that the Magallanes-Fagnano Fault is a reactivatedsuture of pre-Jurassic age separating thebasement of twoterranes.[2]

References

[edit]
  1. ^Lodolo, Emanuele; Menichetti, Marco; Bartole, Roberto;Ben-Avraham, Zvi; Tassone, Alejandro; Lippai, Horacio (2003)."Magallanes-Fagnano continental transform fault (Tierra del Fuego, southernmost South America)".Tectonics.22 (6): 1076.Bibcode:2003Tecto..22.1076L.doi:10.1029/2003TC001500.
  2. ^abHervé, F.; Fanning, C.M.;Pankhurst, R.J.;Mpodozis, C.; Klepeis, K.; Calderón, M.; Thomson, S.N. (2010)."Detrital zircon SHRIMP U–Pb age study of the Cordillera Darwin Metamorphic Complex of Tierra del Fuego: sedimentary sources and implications for the evolution of the Pacific margin of Gondwana"(PDF).Journal of the Geological Society, London.167 (3):555–568.Bibcode:2010JGSoc.167..555H.doi:10.1144/0016-76492009-124.

Sedimentary
basins
Faults
Batholiths
Metamorphic
complexes
Terranes


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