Results 61 to 70 of about 7,074 (218)

Oxygen Isotopic Composition of Miocene Meteoric Water (δ18Ow) in Alpine Foreland Basins

open access: yesGeochemistry, Geophysics, Geosystems, Volume 27, Issue 8, August 2026.
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]

open access: yes, 2017
New species of Bathysiphon (Foraminiferida: Textulariina) from Franciscan Flysch Deposits, northernmost ...
Miller, III, William
core  

Nuovi dati sul Flysch di Nocara (Calabria settentrionale)

open access: yes, 1984
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

open access: yesTectonics, Volume 45, Issue 8, August 2026.
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

open access: yes, 2004
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  

Provenance analysis of the Voirons Flysch (Gurnigel nappe, Haute-Savoie, France): stratigraphic and palaeogeographic implications

open access: yes, 2017
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

Architecture of the Patrimonio Fault System and the Miocene Post‐Orogenic Extension in Alpine Corsica (France)

open access: yesTectonics, Volume 45, Issue 8, August 2026.
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]

open access: yes, 2019
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

open access: yesGeologica Carpathica, 2008
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

Mineralogía y génesis de las arcillas de las unidades del Campo de Gibraltar. I. Areniscas del Aljibe

open access: yesEstudios Geologicos, 1988
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

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