Sedimentology of Some
Flysch Deposits: A Graphic Approach to Facies Interpretation.
The study area is covered by the rocks ranging in age from Triassic to recent/subrecent, and can be divided structurally, into three domains, Tungi-Ahmadun Syncline Area, Khanozai-Torkhula Ophiolite Segment and Murgha Zikriazai
Flysch Segment.
A good example are the
Flysch Carpathians, where so far almost 58,000 landslides have been inventoried in the Polish part of the area, and their approximate number here may exceed even 100,000 (Wojcik and Wojciechowski, 2016).
K-bentonite, black-shale and
flysch successions at the Ordovician--Silurian transition, South China: Possible sedimentary responses to the accretion of Cathaysia to the Yangtze Block and its implications for the evolution of Gondwana.
* Tajillo del Moro (Casabermeja): se trata de un sepulcro megalitico de corredor ubicado en las laderas septentrionales de los Montes de Malaga, en el contacto con el
flysch de Colmenar, en las cercanias de los asentamientos de Cerro Garcia y Los Penones, de la estacion rupestre de Penas de Cabrera y las minas de cobre de Casacara.
En su geologia predomina el
flysch propio de la fase de sedimentos eocenicos destacando el paisaje karstico en el macizo de Larra y las profundas foces en las barras calizas del mediodia del valle.
Tazioli, "Characterizing the recharge of fractured aquifers: a case study in a
Flysch rock mass of the Northern Apennines (Italy)," Engineering Geology for Society and Territory, vol.
(iv) F: coastal rockstone
flysch bank of Cenozoic era (more precisely, Eocene period), with high compactness
These carbonate platforms tectonically overlay a pile of Mesozoic-Tertiary pelagic basin successions belonging to the Lagonegro unit, Neogene
flysch deposits, and shallow-water and slope facies carbonates of the Apulian Platform ([40-43] and references therein).
The most widespread lithotypes are limestones and dolomites (34%), alluvial sediments and clays (22%), volcanic rocks (18%), and
flysch deposits and arenaceous assemblages (17%) (Geoportale Nazionale, 2016).