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Estimation of the tectonic slip-rate from Quaternary lacustrine facies within the intraplate Albacete province (SE of Spain)

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Rodríguez Pascua, Miguel Angel and Bischoff, James L. and Garduño Monroy, V.H. and Pérez López, Raúl and Giner-Robles, J.L. and Israde Alcántara, I. and Calvo Sorando, José Pedro and Williams, Ross W. (2009) Estimation of the tectonic slip-rate from Quaternary lacustrine facies within the intraplate Albacete province (SE of Spain). Sedimentary geology, 222 . pp. 89-97. ISSN 0037-0738

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Official URL: https://www.journals.elsevier.com/sedimentary-geology



Abstract

The Quaternary lacustrine basin of Cordovilla (CB) represents one of the most active tectonic areas of the Prebetic Zone (Albacete, SE of Spain). The Quaternary sedimentary deposits of this basin are mainly endoreic lacustrine carbonate and alluvial deposits, developed in a semi-arid climate (Pleistocene-present). The basin is a NW–SE-elongated graben bounded by a major right-lateral oblique-fault, the Pozohondo Fault. This fault trendsNW–SE, with an approximate trace of 55 km, and is composed of various segments which are identified by fault scarps. In order to establish the slip-rate of the most active segment of the Pozohondo Fault, called the Cordovilla segment, we carried out a detailed study of the affected Quaternary lacustrine deposits. We found that the lacustrine facies could be related to episodic moderate paleoearthquakes. The slip-rate is calculated to be 0.05 and 0.09 mm/yr, using radiometric dating for the vertical offsets of the lacustrine facies. A trenching study at the northern part of the Cordovilla segment revealed two events caused by paleoearthquakes, with the most recent expressed as an oblique-fault off-setting a poorly-developed soil. The magnitude of the last event was greater than 6, using various empirical relationships for the fault displacement and the surface-length rupture. We estimate episodic activity across the Cordovilla segment, to be characterized by moderate-sized paleoearthquakes (M6), which is in agreement with the tectonic context of an intraplate zone of the Iberian plate.


Item Type:Article
Uncontrolled Keywords:Lacustrine record; Quaternary fault; Slip rate; Intraplate; Paleoearthquake
Subjects:Sciences > Geology > Geodynamics
ID Code:58803
Deposited On:05 Feb 2020 12:11
Last Modified:05 Feb 2020 15:33

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