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Styles of positive inversion tectonics in the Central Apennines and in the Adriatic foreland: Implications for the evolution of the Apennine chain (Italy)
V Scisciani - Journal of Structural Geology, 2009 - Elsevier
Integration of new field structural and geophysical data with existing information from the
Apennines chain in Italy and its adjacent Adriatic foreland indicates that the styles of positive …
Apennines chain in Italy and its adjacent Adriatic foreland indicates that the styles of positive …
Structural and sedimentary origin of the Gargano-Pelagosa gateway and impact on sedimentary evolution during the Messinian Salinity Crisis
Circulation of water masses, sediment, and biotope between the sub-basins of the
Mediterranean Sea strongly depends on morphological oceanic gateways. These …
Mediterranean Sea strongly depends on morphological oceanic gateways. These …
Slab retreat and active shortening along the central-northern Apennines
The Quaternary geodynamic evolution and the tectonic processes active along the Central
and Northern Apennines thrust fronts and in the adjacent Padane-Adriatic foredeep domains …
and Northern Apennines thrust fronts and in the adjacent Padane-Adriatic foredeep domains …
Contrasting tectonic and sedimentary history of the central and eastern parts of the Polish Carpathian foredeep basin—results of seismic data interpretation
P Krzywiec - Marine and Petroleum Geology, 2001 - Elsevier
Polish Carpathian foredeep basin (PCFB) is located at the junction between Western and
Eastern European Platforms. Such location caused different evolution of various parts of this …
Eastern European Platforms. Such location caused different evolution of various parts of this …
Pomeranian Caledonides, NW Poland–A collisional suture or thin-skinned fold-and-thrust belt?
A main goal of this study was to understand the character of the Caledonian Deformation
Front in Pomerania, NW Poland and its relationship to the adjoining Teisseyre-Tornquist …
Front in Pomerania, NW Poland and its relationship to the adjoining Teisseyre-Tornquist …
Depositional wedge tops: interaction between low basal friction external orogenic wedges and flexural foreland basins
M Ford - Basin Research, 2004 - earthdoc.org
Growth structures develop mainly across depositional wedge tops where the top of the distal
orogenic wedge lies below local base level within the flexural foreland basin. Documented …
orogenic wedge lies below local base level within the flexural foreland basin. Documented …
[PDF][PDF] Sedimentology and physical stratigraphy of the Messinian turbidite deposits of the Laga Basin (central Apennines, Italy)
This work investigates the physical stratigraphy and the sedimentological characters of the
Messinian turbidites of the Laga Formation, central Apennines. In particular, the study …
Messinian turbidites of the Laga Formation, central Apennines. In particular, the study …
The Pliocene-Pleistocene stratigraphic and tectonic evolution of the central sector of the Western Periadriatic Basin of Italy
A Artoni - Marine and Petroleum Geology, 2013 - Elsevier
The Central portion of the Western Periadriatic Basin is a foreland basins systems
associated to the Central Apennine Outer Orogenic Wedge that stretches along the Marche …
associated to the Central Apennine Outer Orogenic Wedge that stretches along the Marche …
Geological model of the central Periadriatic basin (Apennines, Italy)
3D geological models from multi-source data (cross-sections, geological maps, borehole
logs and outcrops) are a critical tool to improve the interpretation of the spatial organization …
logs and outcrops) are a critical tool to improve the interpretation of the spatial organization …
[КНИГА][B] Thrust belts and foreland basins: From fold kinematics to hydrocarbon systems
What is the important geologic information recorded in Thrust Belts and Foreland Basins
(TBFB) on the evolution of orogens? How do they transcript the coupled influence of deep …
(TBFB) on the evolution of orogens? How do they transcript the coupled influence of deep …