Results 61 to 70 of about 7,074 (218)
Oxygen Isotopic Composition of Miocene Meteoric Water (δ18Ow) in Alpine Foreland Basins
Abstract The reconstructed stable oxygen isotopic composition of meteoric water (δ18Ow) is widely used for paleoclimate reconstructions. Understanding past environmental factors that drove changes in δ18Ow is essential for interpreting past climate conditions.
Armelle Ballian +6 more
wiley +1 more source
New Species of Bathysiphon (Foraminiferida: Textulariina) from Franciscan Flysch Deposits, Northernmost California [PDF]
New species of Bathysiphon (Foraminiferida: Textulariina) from Franciscan Flysch Deposits, northernmost ...
Miller, III, William
core
Nuovi dati sul Flysch di Nocara (Calabria settentrionale)
Two turbidite series were identified in the "Nocara Flysch". The uppermost sequence was named "Nocara Conglomerates" and the lowermost "Colle Cappella Sandstones".
Bartoli A. +3 more
core +1 more source
Active Tectonics of the Eastern and Southern Alps ‐ Crustal Response to Deep Processes? A Review
Abstract Owing to the low N‐S convergence rates between Adria and Europe, crustal deformation rates in the Alps and its forelands are low. Active tectonics are, therefore, difficult to study, especially as non‐tectonic landscape forming processes can erase or modify the tectonic surface imprint. Large‐scale and dense seismological data recently offered
Christoph Grützner +20 more
wiley +1 more source
Paesaggi dei flysch appenninici
I Flysch sono successioni di arenarie, calcari e peliti di origine torbiditica. I paesaggi dei Flysch, sono in funzione della litologia che li costituisce (alternanza di litotipi) e, soprattutto, dell’assetto strutturale. Nell'articolo vengono descritti,
CASTALDINI, Doriano
core
The Chablais Prealps (Haute-Savoie, France) represent a well-preserved accretionary wedge of the Western Alpine Tethys. They comprise a stack of sedimentary nappes related to palaeogeographic realms ranging from the Ultrahelvetic to the Southern Penninic.
Branimir Segvic +7 more
core +1 more source
Abstract The exhumation of Alpine Corsica is the result of Oligocene‐Miocene lithospheric back‐arc extension in the wake of the eastward migration of Apenninic subduction. Although the geometry, kinematics and timing of ductile detachments are well constrained, the brittle extension leading to final exhumation of Alpine Corsica is less documented.
Simone Masoch +7 more
wiley +1 more source
Influence of Anisotropy on the Swelling Properties of Alentejo Flysch Rocks (Portugal) [PDF]
This paper aims to contribute to the knowledge of the swelling properties for the rock materials belonging to the Baixo Alentejo Flysch Group (BAF) in the south of Portugal.
Duarte, Isabel M. R., Pinho, António B.
core +1 more source
Devonian-Carboniferous pre-flysch and flysch environments in the Circum Pannonian Region
The following Devonian-Carboniferous paleogeographic and Variscan orogenic domains were recognized in the Circum Pannonian Region: Oceanic and arc related environments – Noric Bosnian/Carnic-Dinaric Zone (carbonate dominated passive continental margins) – Inovo Zone (Devonian siliciclastic dominated stable continental margins) – Quartzphyllite ...
Jamičić, Domagoj +2 more
openaire +3 more sources
Las «areniscas del Aljibe» son materiales bimodales constituidos en su mayor parte por cuarzos eólicos con «coating» ferruginoso o arcilloso y cemento de cuarzo sintaxial. Tanto la composición mineralógica de la muestra total como la de la fracción < 2 μ
P. Rodríguez Jiménez, M. D. Ruiz Cruz
doaj +1 more source

