Magnetic properties of sedimentary greigite (Fe3S4): An update
Greigite (Fe3S4) is an authigenic ferrimagnetic mineral that grows as a precursor to pyrite
during early diagenetic sedimentary sulfate reduction. It can also grow at any time when …
during early diagenetic sedimentary sulfate reduction. It can also grow at any time when …
How deformed are weakly deformed mudrocks? Insights from magnetic anisotropy
JM Parés - Geological Society, London, Special Publications, 2004 - lyellcollection.org
For over thirty years the anisotropy of magnetic susceptibility (AMS) has been exploited in
rock fabric studies. Our knowledge of the mechanisms leading to magnetic fabric …
rock fabric studies. Our knowledge of the mechanisms leading to magnetic fabric …
Neogene and Quaternary rollback evolution of the Tyrrhenian Sea, the Apennines, and the Sicilian Maghrebides
G Rosenbaum, GS Lister - Tectonics, 2004 - Wiley Online Library
Reconstruction of the evolution of the Tyrrhenian Sea shows that the major stage of rifting
associated with the opening of this basin began at∼ 10 Ma. It involved two episodes of back …
associated with the opening of this basin began at∼ 10 Ma. It involved two episodes of back …
The southern Tyrrhenian subduction zone: deep geometry, magmatism and Plio-Pleistocene evolution
We report on a high-resolution Vp, Vp/Vs and Qp model of the southern Tyrrhenian
subduction zone, obtained by the inversion of P-and S-wave arrival times and t∗ values from …
subduction zone, obtained by the inversion of P-and S-wave arrival times and t∗ values from …
Evaluating magnetic lineations (AMS) in deformed rocks
JM Parés, BA Van Der Pluijm - Tectonophysics, 2002 - Elsevier
Magnetic lineation in rocks is given by a cluster of the principal axes of maximum
susceptibility (Kmax) of the Anisotropy of Magnetic Susceptibility (AMS) tensor. In deformed …
susceptibility (Kmax) of the Anisotropy of Magnetic Susceptibility (AMS) tensor. In deformed …
Neogene-Quaternary strike-slip tectonics in the central Calabrian Arc (southern Italy)
A Middle Miocene-Middle Pleistocene regional NW-SE left-lateral strike-slip fault system
profoundly conditioned the evolution of central Calabria, during the late tectonic phases …
profoundly conditioned the evolution of central Calabria, during the late tectonic phases …
Tectono-stratigraphic and kinematic evolution of the southern Apennines/Calabria–Peloritani Terrane system (Italy)
Temporal controls such as sedimentation ages, in foredeep and wedge-top basins,
combined with information about stratigraphic and metamorphic evolution, ages and …
combined with information about stratigraphic and metamorphic evolution, ages and …
Multi‐Phase Non‐Coaxial Orogenic Growth: Propagation of the Longmen Shan Thrust Belt on the Eastern Margin of the Tibetan Plateau
Reconstructing the deformation sequence and strain history of the Longmen Shan thrust belt
(LSTB) has significant implications for the growths of the SW Qinling orogenic belt and the …
(LSTB) has significant implications for the growths of the SW Qinling orogenic belt and the …
Subduction, convergence and the mode of backarc extension in the Mediterranean region
35 Ma ago a major change occurred in the Mediterranean region, from a regionally
compressional subduction coeval with the formation of Alpine mountain belts, to extensional …
compressional subduction coeval with the formation of Alpine mountain belts, to extensional …
Alpine structural and metamorphic signature of the Sila Piccola Massif nappe stack (Calabria, Italy): Insights for the tectonic evolution of the Calabrian Arc
Combined structural and petrographical investigations, coupled with 40Ar/39Ar
geochronology, were carried out in the Sila Piccola Massif of the Calabrian Arc in order to …
geochronology, were carried out in the Sila Piccola Massif of the Calabrian Arc in order to …