Skip to Main Content
Skip Nav Destination
GEOREF RECORD

Calcrete features and age estimates from U/Th dating; implications for the analysis of Quaternary erosion rates in the northern limb of the Sierra Nevada range (Betic Cordillera, southeast Spain)

J. M. Azanon, P. Tuccimei, A. Azor, I. M. Sanchez-Almazo, Ana Maria Alonso-Zarza, M. Soligo and J. V. Perez-Pena
Calcrete features and age estimates from U/Th dating; implications for the analysis of Quaternary erosion rates in the northern limb of the Sierra Nevada range (Betic Cordillera, southeast Spain) (in Paleoenvironmental record and applications of calcretes and palustrine carbonates, Ana Maria Alonso-Zarza (editor) and Lawrence H. Tanner (editor))
Special Paper - Geological Society of America (2006) 416: 223-239

Abstract

The Guadix topographic depression is a Neogene-Quaternary basin located in the central sector of the Betic Cordillera at the boundary between the South Iberian margin and the Alboran domain. This topographic depression is a plateau with an average elevation of 1000 m in the northern limb of the Sierra Nevada range. The continental deposits infilling the Guadix basin span time from the late Tortonian to the Pleistocene, when a laminar calcrete developed on fine-to coarse-grained fluvial and lacustrine deposits. The drainage pattern is strongly incised (up to 200 m) below the calcrete layer. Four coeval subsamples from the top laminae of the calcrete were collected and dated by the U/Th method. The resulting date is 42.6+ or -5.6 ka, which indicates the minimum age for the cessation of active sedimentation in the Guadix basin. Using this age, we have calculated the incision and erosion rates for the late Pleistocene to present-day time span in the Arroyo de Gor, a highly incised canyon in the eastern border of the Guadix basin. The minimum incision rates in this canyon are around 4 mm/yr. We envisage the capture of the Pliocene-Pleistocene endorheic Guadix basin by the Guadalquivir River after 42 ka as the main factor triggering the formation of the present-day eroded landscape. After the capture, the combination of climatic (wet periods), lithological (soft and loose sediments), and topographic (high average altitude) features allowed the development of the present-day entrenched drainage pattern.


ISSN: 0072-1077
EISSN: 2331-219X
Coden: GSAPAZ
Serial Title: Special Paper - Geological Society of America
Serial Volume: 416
Title: Calcrete features and age estimates from U/Th dating; implications for the analysis of Quaternary erosion rates in the northern limb of the Sierra Nevada range (Betic Cordillera, southeast Spain)
Title: Paleoenvironmental record and applications of calcretes and palustrine carbonates
Author(s): Azanon, J. M.Tuccimei, P.Azor, A.Sanchez-Almazo, I. M.Alonso-Zarza, Ana MariaSoligo, M.Perez-Pena, J. V.
Author(s): Alonso-Zarza, Ana Mariaeditor
Author(s): Tanner, Lawrence H.editor
Affiliation: Universidad de Granada, Departamento de Geodinamica, Granada, Spain
Affiliation: Universidad Complutense de Madrid, Departamento Petrologia y Geoquimica, Madrid, Spain
Pages: 223-239
Published: 2006
Text Language: English
Summary Language: Spanish
Publisher: Geological Society of America (GSA), Boulder, CO, United States
ISBN: 08137241630
ISBN: 9780813724164
References: 54
Accession Number: 2007-113673
Categories: Quaternary geologyGeochronology
Document Type: Serial
Bibliographic Level: Analytic
Illustration Description: illus. incl. sects., strat. col., 1 table, sketch maps
N37°00'00" - N37°45'00", W04°30'00" - W02°30'00"
Secondary Affiliation: Le Moyne College, USA, United StatesUniversita Roma Tre, ITA, ItalyUniversidad Complutense, ESP, Spain
Country of Publication: United States
Secondary Affiliation: GeoRef, Copyright 2017, American Geosciences Institute.
Update Code: 200747
Close Modal

or Create an Account

Close Modal
Close Modal