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Autor Le Pera, Emilia |
Documentos disponibles escritos por este autor (6)
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The Henares River, central Spain, flows westward from the Iberian Range (Mesozoic sedimentary rocks) under semiarid climatic conditions. In the middle and lower reaches, the Henares River receives sediment from three tributaries (Cañamares, Born[...]texto impreso
Caracciolo, Luca ; Tolosana Delgado, Raimon ; Le Pera, Emilia ; Eynatten, Hilmar von ; Arribas Mocoroa, José ; Tarquini, Simone | Elsevier | 2012The aim of this study is to determine and characterise the control exerted by parent rock texture on sand composition as a function of grain size. The sands investigated were generated from granitoid parent rocks by the Rhone, Damma and Sidelen [...]texto impreso
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Le Pera, Emilia ; Arribas Mocoroa, José ; Critelli, Salvatore ; Tortosa, A. | Blackwell Publishing Ltd | 2001Plutonic and gneissic rocks of the Sila Massif in the uppermost portion of the Neto drainage basin (Calabria, Southern Italy) weather and erode under a humid Mediterranean climate. During the development of weathering pro®les, a combination of c[...]texto impreso
The recycled orogenic sand provenance from an uplifted thrust belt, Betic Cordillera, Southern Spain
Critelli, Salvatore ; Arribas Mocoroa, José ; Le Pera, Emilia ; Tortosa, A. ; Marsaglia, Kathleen M. ; Latter, Kelly K. | SEPM (Society for Sedimentary Geology) | 2003The Betic Cordillera of southern Spain represents an uplifted foreland fold–thrust belt. Source rock types of the Betic Cordillera include metamorphic (mainly phyllite, schist, quartzite, and gneiss), sedimentary (siliciclastic and carbonate), v[...]