Results 101 to 110 of about 831 (199)

L'INQUADRAMENTO SINTASSONOMICO DEI BOSCHI A QUERCUS CERRIS ED OSTRYA CARPINIFOLIA DEL FLYSCH NELL'APPENNINO MARCHIGIANO SETTENTRIONALE

, 1982
SYNTAXONOMY OF QUERCUS CERRIS AND OSTRYA CARPINIFOLIA WOODS IN THE NORTHERN APENNINES OF THE MARCHE REGION (ITALY). The AA. discuss the syntaxonomy of Quercus cerris and Ostrya carpinifolia woods in the northern Apennines of Marche region (Pesaro-Urbino ...
Speranza, Maria, Ubaldi, Davide
core  

New data on the late Famennian miospore assemblage of the Cercal Anticline (westernmost Iberian Pyrite Belt area), Portugal [PDF]

, 2014
The Cercal Anticline (CA) is located in the westernmost region of the Iberian Pyrite Belt (IPB). The exposed stratigraphic sequence includes, in ascending order, the Volcano-Sedimentary Complex (VSC) followed by the Xistos das Abertas Fm, which ...
Oliveira, José Tomás, Matos, João Xavier, Fernandes, Paulo, Pereira, Zélia   +3 more
core  

Cretaceous (Aptian/Albian-?Cenomanian) age of "black flysch" and adjacent deposits of the Grajcarek thrust-sheets in the Małe Pieniny Mts. (Pieniny Klippen Belt, Polish Outer Carpathians)

, 2012
Several sections record the relation between the "black flysch" and Upper Cretaceous red shales in the Grajcarek thrust-sheets. In all the sections studied the "black flysch" appears in the core of imbricated folds or thrust-sheets, whereas the limbs are
Oszczypko, Nestor, Oszczypko, N., Olszewska, B., Malata, Ewa, Malata, E., Olszewska, Barbara   +5 more
core   +1 more source

Weather induced post failure kinematics of a highway embankment founded on a marly sandstone slope. [PDF]

Sci Rep, 2023
Comegna L, Mandolini A, Manna D, Rianna G, Reder A.   +4 more
europepmc   +1 more source

Shallow Seismic Refraction Tomography Images from the Pieniny Klippen Belt (Southern Poland)

The Pieniny Klippen Belt (PKB) is located between the Central and the Outer (Flysch) Carpathians and forms a narrow zone with a complex structure, often described as a mélange.
Jerzy Dec, Jan Golonka, Kamil Cichostępski, Anna Waśkowska   +3 more
core   +1 more source

Kinematic effect of the Andaman Sea opening on the Tanintharyi coastal strip bending with the formation of the Mergui Archipelago, Myanmar

Evolving Earth
The structural, bathymetric, and temporal complexities of the Mergui-Andaman Basin cannot be explained by a single, steady-state post-middle Miocene spreading phase.
Aung Moe, Kyi Khin, Kyi Pyar Aung
doaj   +1 more source

Early to Late Bajocian age of the "black flysch" (Szlachtowa Fm.) deposits: implications for the history and geological structure of the Pieniny Klippen Belt, Carpathians

, 2012
The "black flysch" deposits (Szlachtowa Formation at Podubocze near Czorsztyn in Poland), attributed so far to the Pieniny Klippen Basin successions, and at Hałuszowa in Poland as well as at Kamienka in Eastern Slovakia, attributed to the Grajcarek ...
Barski, M., Matyja, B. A., Segit, T., Wierzbowski, A.   +3 more
core  

Pre-Cretaceous Paleocurrents of the Northeastern Hidaka Belt, Hokkaido, Japan [PDF]

, 1979
Typical Pre-Cretaceous flysch type sediments, called the Yubetsu Group, are exposed on the northeastern part of the Hidaka Belt. The authors have done a three dimensional analysis of internal sedimentary structures utilizing the soft X-ray technique for ...
Kiminami, Kazuo, Kontani, Yoshihiro
core  

Constraints on upper crustal fluid circulation and seismogenesis from in-situ outcrop quantification of complex fault zone permeability. [PDF]

Sci Rep, 2023
Curzi M, Giuntoli F, Vignaroli G, Viola G.   +3 more
europepmc   +1 more source

Tectonic relationship between the Druja (Gavrovo) and the Ionian zones of the Albania thrust belt

, 2001
The Kruja zone and the Ionian one are integral parts of the Albanian Thrust Belt, which lie directly in the northern continuation of the Western Hellenic Nappes up to their interruption against the thrust front.
AVDULAJ, F., SULAJ, Y., PRENJASI, E., SINA, M.   +3 more
core