The Mesozoic Iberia-Eurasia diffuse plate boundary: A wide domain of distributed transtensional deformation progressively focusing along the North Pyrenean Zone
Plate kinematic reconstructions available for the Late Jurassic-Early Cretaceous eastward
drift and counterclockwise rotation of the Iberian plate imply a major left-lateral motion of …
drift and counterclockwise rotation of the Iberian plate imply a major left-lateral motion of …
The Iberia-Eurasia plate boundary east of the Pyrenees
In this work we provide a reappraisal of the mid-Cretaceous extensional basins located to
the east of the Pyrenean mountain ranges, from the easternmost portion of Iberia to the …
the east of the Pyrenean mountain ranges, from the easternmost portion of Iberia to the …
Inverse magnetic fabric of remagnetized limestones in the Zaduo area, Eastern Qiangtang Terrane: Implications for oroclinal bending in the Eastern Himalayan …
Magnetic fabric analysis is a common technique to assess the strain regime during mountain
building processes. Here, we use this approach to evaluate the tectonic evolution of the …
building processes. Here, we use this approach to evaluate the tectonic evolution of the …
Two-stage strike-slip faulting of the Altyn Tagh Fault revealed by magnetic fabrics in the Qaidam Basin
The timing and mechanism of the changes in the stress/strain field direction on the
northeastern Tibetan Plateau are controversial, which limits our understanding of the …
northeastern Tibetan Plateau are controversial, which limits our understanding of the …
Magnetic fabric constraints on the Cenozoic compressional strain changes in the northern Qaidam marginal thrust belt and their tectonic implications
Reconstructing the compressional strain history of the northern Qaidam marginal thrust belt
has significant implications for understanding the mountain building processes of the …
has significant implications for understanding the mountain building processes of the …
Inversion tectonics and magnetic fabrics in Mesozoic basins of the Western Tethys: A review
Positive tectonic inversion of sedimentary basins has been recognized as one of the primary
mechanisms of mountain building and intraplate deformation. Reconstructing the tectonic …
mechanisms of mountain building and intraplate deformation. Reconstructing the tectonic …
[HTML][HTML] Anisotropy of magnetic susceptibility study and its significance in the Late Cretaceous-Cenozoic Sanmenxia Basin in the southeastern Shanxi rift, Central …
K Jiang, W Liang, G Wu, C Liu, X Zou, X He, J Li… - Solid Earth …, 2022 - Elsevier
Abstract The Sanmenxia Basin, located on the southeastern margin of the Shanxi rift and
filled with Cretaceous-Paleogene fluvial and lacustrine sediments, is a faulted basin …
filled with Cretaceous-Paleogene fluvial and lacustrine sediments, is a faulted basin …
Evidence for the Permo-Triassic transtensional rifting in the Iberian Range (NE Spain) according to magnetic fabrics results
Anisotropy of magnetic susceptibility (AMS) techniques are applied to Permo-Triassic red
beds from the Castilian Branch (Iberian Range, NE Spain) that were deposited in an …
beds from the Castilian Branch (Iberian Range, NE Spain) that were deposited in an …
Improving the method of low‐temperature anisotropy of magnetic susceptibility (LT‐AMS) measurements in air
R Issachar, T Levi, V Lyakhovsky… - Geochemistry …, 2016 - Wiley Online Library
This study examines the limitations of the method of low‐temperature anisotropy of magnetic
susceptibility (LT‐AMS) measurements in air and presents technical improvements that …
susceptibility (LT‐AMS) measurements in air and presents technical improvements that …
Along‐strike evolution of folding, stretching and breaching of supra‐salt strata in the Plataforma Burgalesa extensional forced fold system (northern Spain)
The P lataforma B urgalesa is a partly exposed extensional forced fold system with an
intermediate salt layer, which has developed along the southern portion of the B asque‐C …
intermediate salt layer, which has developed along the southern portion of the B asque‐C …