Seismically-induced soft-sediment deformation structures associated with the Magallanes?Fagnano Fault System (Isla Grande de Tierra del Fuego, Argentina)

MARÍA ROMINA ONORATO; LAURA PATRICIA PERUCCA; ANDREA CORONATO; JORGE RABASSA; RAMIRO LÓPEZ

SEDIMENTARY GEOLOGY

ELSEVIER SCIENCE BV

Lugar: Amsterdam; Año: 2016 p. 135 - 144

0037-0738

In this paper, evidence of paleoearthquake-induced soft-sediment deformation structures associated with the Magallanes?Fagnano Fault Systemin the Isla Grande de Tierra del Fuego, southern Argentina, has been identified.Well-preserved soft-sediment deformation structures were found in a Holocene sequence of the Udaeta pond.These structures were analyzed in terms of their geometrical characteristics, deformation mechanism, driving force system and possible trigger agent. They were also grouped in different morphological types: sand dykes,convolute lamination, load structures and faulted soft-sediment deformation features. Udaeta, a small pond in Argentina Tierra del Fuego, is considered a Quaternary pull-apart basin related to the Magallanes?FagnanoFault System. The recognition of these seismically-induced features is an essential tool for paleoseismic studies.Since the three main urban centers in the Tierra del Fuego province of Argentina (Ushuaia, Río Grande and Tolhuin) have undergone an explosive growth in recent years, the results of this study will hopefully contribute to future analyses of the seismic risk of the region.