@article{10272/7457,
year = {2010},
url = {http://hdl.handle.net/10272/7457},
abstract = {The Arroyofrio bed (Oxfordian-Callovian) from NE Iberian Chain represents a sedimentary shallow
marine deposit with iron oolites. The paleogeographic model shows two possible paleocurrent directions:
i) normal to the Ejulve-Maestrazgo emerged area or ii) parallel to the shore line. Different techniques have
been applied to analyze paleocurrents in different environments. AMS analysis together with thin section
image analysis is developed to test the application of AMS to unravel the sedimentary imprint linked to
tractive currents. The obtained results show a general parallelism between magnetic lineation and oolite
arrangement analyzed from thin sections. The obtained results show an imbricated oolite pattern compatible
with a paleocurrent direction N020-040ºE},
publisher = {Universidad de Huelva},
title = {Análisis de paleocorrientes en la unidad de Arroyofrío (Calloviense-Oxfordiense; Cordillera Ibérica) por medio de análisis de imágenes de lámina delgada y Anisotropía de Susceptibilidad Magnética (ASM). Datos preliminares},
title = {Paleocurrent analysis in Arroyofrio beds (Callovian-Oxfordian; Iberian Range) by means of thin section image
analysis and Anisotropy of Magnetic Susceptibility (AMS). Preliminary data},
author = {Pueyo Anchuela, Óscar and Gil Imaz, Andrés and Ramajo Cordero, Javier and Meléndez Hevia, Guillermo},
}