Paleogeographic and sedimentary evolution of the South Pyrenean foreland basin
Abstract During the Paleogene and Neogene the NE Iberian plate underwent significant
paleogeographic changes driven by the Iberian and European plate collision and the …
paleogeographic changes driven by the Iberian and European plate collision and the …
Microcodium: an extensive review and a proposed non-rhizogenic biologically induced origin for its formation
P Kabanov, P Anadón, WE Krumbein - Sedimentary geology, 2008 - Elsevier
Microcodium has been previously described as a mainly Cenozoic calcification pattern
ascribed to various organisms. A review of the available literature and our data reveal two …
ascribed to various organisms. A review of the available literature and our data reveal two …
Lacustrine carbonates: facies models, facies distributions and hydrocarbon aspects
Lacustrine carbonates are dominantly biogenic or bio‐induced precipitates. While lake
basinal carbonates may be modelled in terms of hydrological factors, marginal lacustrine …
basinal carbonates may be modelled in terms of hydrological factors, marginal lacustrine …
Global catalogue, classification and tectonic origins of restraining-and releasing bends on active and ancient strike-slip fault systems
P Mann - 2007 - pubs.geoscienceworld.org
Restraining-and releasing bends with similar morphology and structure have been
described by many previous studies of strike-slip faults in a variety of active and ancient …
described by many previous studies of strike-slip faults in a variety of active and ancient …
The Neogene structure of the eastern Iberian margin: structural constraints on the crustal evolution of the Valencia trough (western Mediterranean)
The presence of a thinned crust beneath the Valencia trough has been recognized for a long
time. However, to date no attempt to link this thinning, inferred from geophysical data, with …
time. However, to date no attempt to link this thinning, inferred from geophysical data, with …
Eastern Pyrenees and related foreland basins: pre-, syn-and post-collisional crustal-scale cross-sections
A new crustal-scale cross-section through the Eastern Pyrenees shows a minimum of 125
km of total shortening across the belt. Convergence rates of 6 mm/yr (during early and …
km of total shortening across the belt. Convergence rates of 6 mm/yr (during early and …
Oligocene to Middle Miocene evolution of the central Catalan margin (northwestern Mediterranean)
The Catalan margin belongs to the northern sector of the margin that separates the
extremely thinned continental crust of the Valencia trough from the undeformed or thickened …
extremely thinned continental crust of the Valencia trough from the undeformed or thickened …
[HTML][HTML] Mineralogical and thermal characterization of kaolinitic clays from Terra Alta (Catalonia, Spain)
This research characterizes the kaolinitic clays from Cretaceous–Paleocene lateritic
deposits of Terra Alta (south Catalonia) to evaluate their possible applications. The outcrops …
deposits of Terra Alta (south Catalonia) to evaluate their possible applications. The outcrops …
Evolution of the central Catalan margin of the Valencia trough (western Mediterranean)
The evolution of the central Catalan margin was conditioned by major fault activity and
thermal processes generated by crustal thinning. The continental margin structure is …
thermal processes generated by crustal thinning. The continental margin structure is …
Closing and continentalization of the South Pyrenean foreland basin (NE Spain): magnetochronological constraints
This paper presents new magnetostratigraphic results from a 1100‐m‐thick composite
section across the marine to continental sediments of the central part of the SE margin of the …
section across the marine to continental sediments of the central part of the SE margin of the …