Magnetic mineral diagenesis
AP Roberts - Earth-Science Reviews, 2015 - Elsevier
Reduction–oxidation (redox) reactions occur during burial because sediments contain
reactive mixtures of oxidised and reduced components. Diagenetic chemical reactions …
reactive mixtures of oxidised and reduced components. Diagenetic chemical reactions …
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 …
Age of the Corsica–Sardinia rotation and Liguro–Provençal Basin spreading: new paleomagnetic and Ar/Ar evidence
The age of spreading of the Liguro–Provençal Basin is still poorly constrained due to the
lack of boreholes penetrating the whole sedimentary sequence above the oceanic crust and …
lack of boreholes penetrating the whole sedimentary sequence above the oceanic crust and …
Anisotropy of magnetic susceptibility (AMS) analysis of the Gonjo Basin as an independent constraint to date Tibetan shortening pulses
S Li, DJJ van Hinsbergen, Z Shen… - Geophysical …, 2020 - Wiley Online Library
Abstract The Tibetan Plateau accommodated major upper crustal shortening during Indian
Plate oceanic and continental lithosphere subduction. Deciphering whether shortening was …
Plate oceanic and continental lithosphere subduction. Deciphering whether shortening was …
Magnetostratigraphy and anisotropy of magnetic susceptibility of the Lulehe Formation in the northeastern Qaidam Basin
K Xue, J Junliang, Z Kexin, KOU Xiaohu… - Acta Geologica …, 2013 - Wiley Online Library
The timing of onset of deposition of the Lulehe Formation is a significant factor in
understanding the genesis of the Qaidam basin and the evolution of the Tibetan Plateau …
understanding the genesis of the Qaidam basin and the evolution of the Tibetan Plateau …
Late Cretaceous to Paleocene oroclinal bending in the central Pontides (Turkey)
The Turkish Pontide fold‐and‐thrust belt formed since the Paleozoic and is an important
element in the Africa‐Eurasia convergence and the resulting closure of the Neo‐Tethys …
element in the Africa‐Eurasia convergence and the resulting closure of the Neo‐Tethys …
Kinematics of a former oceanic plate of the Neotethys revealed by deformation in the Ulukışla basin (Turkey)
Kinematic reconstruction of modern ocean basins shows that since Pangea breakup a vast
area in the Neotethyan realm was lost to subduction. Here we develop a first‐order …
area in the Neotethyan realm was lost to subduction. Here we develop a first‐order …
Rock magnetism and palaeomagnetism of greigite-bearing mudstones in the Italian peninsula
L Sagnotti, A Winkler - Earth and Planetary Science Letters, 1999 - Elsevier
Magnetic measurements were carried out on a collection of samples from different
geological settings throughout the Italian peninsula. The samples display magnetic …
geological settings throughout the Italian peninsula. The samples display magnetic …
Magnetic fabric and petrographic investigation of hematite-bearing sandstones within ramp-related folds: examples from the South Atlas Front (Morocco)
An investigation of the anisotropy of magnetic susceptibility (AMS) of hematite-bearing
sandstones has been carried out along two fault-propagation folds located at the front of the …
sandstones has been carried out along two fault-propagation folds located at the front of the …
Reliability of magnetic fabric of weakly deformed mudrocks as a palaeostress indicator in compressive settings
In this work we compare the results of anisotropy of magnetic susceptibility (AMS) with
palaeostress analysis at local scale. The AMS data refer to 14 sites from weakly deformed …
palaeostress analysis at local scale. The AMS data refer to 14 sites from weakly deformed …