The spatial distribution of 961 debris flows in the Upper Aragón and Gállego valleys (Central Spanish Pyrenees) was analyzed. Most were located in the Flysch Sector (with a colluvium mantle derived ...
Un flysch est une formation géologique retrouvée dans les séries anciennes, constituée par une alternance monotone de bancs d'épaisseurs métriques à décamétriques. Typiquement, la nature de ces bancs ...
We present new stratigraphic and petrographic data on the easterly-derived medial Ordovician flysch sequence of western New England and eastern New York State. A conformable relationship exists ...
Sedimentary Features of Flysch and Greywackes By S. Dzulyński and E. K. Walton. (Developments in Sedimentology, Vol. 7.) Pp. viii + 274. (Amsterdam, London and New York: Elsevier Publishing Company, ...