Ostracode-based aminostratigraphy and aminochronology of a tufa system in central Spain [PDF]
, 2005 In the Priego area, central Spain, extensive tufa deposits are located in three small tributaries located at the head of the 1000 kmlong Tagus River. The deposits are originated after karst-origin running waters emerged from the confines of the canyons ...
Andrews +46 more
core +2 more sources
Journal of Maps, 2020 The High Plateaus Basin is an important region to understand landscape evolution and human occupation in North Africa during the Quaternary. We focused on the Gara Soultana area, applying Unmanned Aerial Vehicles, photogrammetry and a submeter Global ...
A. Benito-Calvo +5 more
doaj +1 more source
Frontiers in Earth Science, 2021 The height of a thrust-fault scarp on a fluvial terrace would be modified due to erosion and deposition, and these surface processes can also influence the dating of terraces.
Qingri Liu +11 more
doaj +1 more source
Geomorphic signal of active faulting at the northern edge of Lut Block. Insights on the kinematic scenario of Central Iran [PDF]
, 2016 Recent works documented Neogene to Quaternary dextral strike-slip tectonics along the Kuh-e-Sarhangi and Kuh-e-Faghan intraplate strike-slip faults at the northern edge of the Lut Block of Central Iran, previously thought to be dominated by sinistral ...
Claudio, Faccenna +6 more
core +1 more source
Kinematic analysis of the Pakuashan fault tip fold, west central Taiwan: Shortening rate and age of folding inception [PDF]
, 2007 The Pakuashan anticline is an active fault tip fold that constitutes the frontal most zone of deformation along the western piedmont of the Taiwan Range.
Avouac, Jean Philippe +7 more
core +4 more sources
Evidence of Quaternary tectonics along Río Grande valley, southern Malargüe fold and thrust belt, Mendoza, Argentina [PDF]
, 2019 The Malargüe fold and thrust belt is developed in the Argentinian Andes between 34° and 37° S, through the tectonic inversion of Upper Triassic and Lower Jurassic depocenters of the Neuquén Basin, with an uplift history since the Cretaceous.
Colavitto, Bruno +4 more
core +1 more source
SEDIMENTS AND AGE OF TERRACES AND FLOODPLAINS OF THE EZOUSAS RIVER IN SW CYPRUS [PDF]
Acta Geobalcanica, 2021 Since 2014 Jan Kochanowski University in Kielce participate in the research in Paphos region in SW Cyprus. The aim of geomorphologic study was the age and sediments of terraces and floodplains in Ezousas river valley.
Tomasz Kalicki +6 more
doaj +1 more source
Modeling the shortening history of a fault tip fold using structural and geomorphic records of deformation [PDF]
, 2007 We present a methodology to derive the growth history of a fault tip fold above a basal detachment. Our approach is based on modeling the stratigraphic and geomorphic records of deformation, as well as the finite structure of the fold constrained from ...
Avouac, Jean-Philippe +2 more
core +3 more sources
Pleistocene terraced fluvial succession, northern slope of Torino Hill [PDF]
Quaternary International, 2007 Abstract A Pleistocene terraced fluvial succession is found on the northern slope of the Torino Hill. This succession consists of many relics of flat surfaces, separated by scarps, often associated with sandy and silty deposits, perched from 30 to 400 m on the Po Plain. Terraced surfaces at high levels are more deformed, dissected and mostly deprived
Diego Barbero +3 more
openaire +1 more source
Sporepolinic morphology of fluvial terrace sediments in the Western Amazon [PDF]
Acta Botanica Brasilica, 2020 ABSTRACT Morphological descriptions were made for pollen grains and spores extracted from samples from three sedimentary sections - Chandless 1, Purus 10 and Purus 30 - from fluvial terraces on the Chandless and Purus rivers, Acre State, Brazil. Level CH1-12 at Chandless 1 was C14-dated to 4861 - 5050 cal yr BP, P10-3 of Purus 10 was dated through the ...
Mayra Nina Araujo Silva +3 more
openaire +5 more sources