[HTML][HTML] Timing, sequence, duration and rate of deformation in fold-and-thrust belts: A review of traditional approaches and recent advances from absolute dating (K …
O Lacombe, NE Beaudoin - Comptes …, 2024 - comptes-rendus.academie-sciences …
Résumé Based on a review of literature and a few case studies, this paper summarizes the
state of the art on the dating of folds and thrusts, then presents and discusses how recent …
state of the art on the dating of folds and thrusts, then presents and discusses how recent …
[HTML][HTML] Fluid-rock interaction, skarn genesis, and hydrothermal alteration within an upper crustal fault zone (Island of Elba, Italy)
The Terranera magnetite-hematite-pyrite deposit of the Island of Elba (Italy) is an historical
skarn deposit hosted by a fault zone of regional importance (Zuccale Fault) and by its …
skarn deposit hosted by a fault zone of regional importance (Zuccale Fault) and by its …
Architecture and permeability structure of the Sibillini Mts. Thrust and influence upon recent, extension-related seismicity in the central Apennines (Italy) through fault …
The central Apennines are a fold-thrust belt currently affected by post-orogenic extensional
seismicity. To constrain the influence that the inherited thrust-related structures exert on the …
seismicity. To constrain the influence that the inherited thrust-related structures exert on the …
Constraints on upper crustal fluid circulation and seismogenesis from in-situ outcrop quantification of complex fault zone permeability
The permeability of fault zones plays a significant role on the distribution of georesources
and on seismogenesis in the brittle upper crust, where both natural and induced seismicity …
and on seismogenesis in the brittle upper crust, where both natural and induced seismicity …
Repeated brittle reactivations of a pre-existing plastic shear zone: combined K–Ar and 40Ar–39Ar geochronology of the long-lived (> 700 Ma) Himdalen–Ørje …
E Torgersen, RH Gabrielsen, M Ganerød… - Geological …, 2022 - cambridge.org
Brittle reactivation of plastic shear zones is frequently observed in geologically old terranes.
To better understand such deformation zones, we have studied the> 700 Ma long structural …
To better understand such deformation zones, we have studied the> 700 Ma long structural …
[HTML][HTML] Tectonic-Sedimentary evolution of the Tuscan shelf (Italy): Seismic-stratigraphic/structural analysis of Neogenic succession in the Tyrrhenian Sea between …
A reinterpretation of the vectorized version of public vintage seismic profiles in the
Tyrrhenian Sea (Italy), between Elba Island and Monte Argentario promontory, was …
Tyrrhenian Sea (Italy), between Elba Island and Monte Argentario promontory, was …
Tectonic evolution of the Eastern Southern Alps (Italy): A reappraisal from new structural data and geochronological constraints
Abstract The Eastern Southern Alps fold‐and‐thrust belt (ESA) is part of the seismically
active S‐verging retro‐wedge of the European Alps. Its temporal tectonic evolution during …
active S‐verging retro‐wedge of the European Alps. Its temporal tectonic evolution during …
Relative dating of fault activity using the principle of cross-cutting relationships: An automated approach
Fault dating plays an essential role in understanding deformation histories and modeling the
tectonic evolution of orogenic belts. However, direct fault dating methods via different …
tectonic evolution of orogenic belts. However, direct fault dating methods via different …
[HTML][HTML] How brittle detachments form and evolve through space and time
We report the first absolute deformation ages for the Mykonos Detachment that juxtaposes,
in the context of the current Aegean rifting, Miocene siliciclastic deposits in the hanging wall …
in the context of the current Aegean rifting, Miocene siliciclastic deposits in the hanging wall …
[HTML][HTML] The complex continental margin of NE Oman: Fault-gouge dating of the Wadi Kabir Fault at the northern margin of the Saih Hatat window, Sultanate of Oman …
The complex structural geometry along the northern continental margin of Oman formed
during polyphase deformation from the late Cretaceous to the Miocene. We focus on the …
during polyphase deformation from the late Cretaceous to the Miocene. We focus on the …