Building the Zagros collisional orogen: timing, strain distribution and the dynamics of Arabia/Eurasia plate convergence

F Mouthereau, O Lacombe, J Vergés - Tectonophysics, 2012 - Elsevier
The Zagros Mountains are the result of the Arabia/Eurasia collision initiated at~ 35Ma as the
rifted Arabian lithosphere was underthrusted beneath the Iranian plate due to its negative …

A review of deformation pattern templates in foreland basin systems and fold-and-thrust belts: Implications for the state of stress in the frontal regions of thrust wedges

S Tavani, F Storti, O Lacombe, A Corradetti… - Earth-Science …, 2015 - Elsevier
Aesthetically appealing thrust systems and related large-scale anticlines, in both active and
fossil foreland fold-and-thrust belts, and the economic potential associated with them, have …

Evolution of the Zagros sector of Neo-Tethys: Tectonic and magmatic events that shaped its rifting, seafloor spreading and subduction history

A Jafari, S Ao, S Jamei, H Ghasemi - Earth-Science Reviews, 2023 - Elsevier
The evolution of the Neo-Tethys realm had a significant impact on the Phanerozoic
paleogeography of the Iran Plateau. However, there remains significant debate regarding …

Salt tectonics along the High Zagros Fault in Iran, faulting through welded salt walls

H Taghikhani, A Yassaghi, S Madanipour… - Journal of Asian Earth …, 2024 - Elsevier
In salt-bearing foreland fold-thrust belts, precursor salt structures affect deformation and
accommodate fault zones during orogenic shortening. The complex structure and the …

[HTML][HTML] Origin of oblique structures controlled by pre-tectonic thickness variations in frictional and salt-bearing fold-and-thrust belts: Insights from analogue modelling

P Santolaria, E Izquierdo-Llavall, R Soto… - Journal of Structural …, 2024 - Elsevier
This work includes, first, a synthesis of experimental analogue modelling programs
assessing the influence of along-strike thickness variations in the development of oblique …

[HTML][HTML] Do fault slip data inversions actually yield “paleostresses” that can be compared with contemporary stresses? A critical discussion

O Lacombe - Comptes Rendus Geoscience, 2012 - Elsevier
Based on a review of published literature and on the report of a few case studies, this paper
summarizes the state of the art on paleostress determinations by fault slip data inversions …

Distribution and arrest of vertical through-going joints in a seismic-scale carbonate platform exposure (Sorrento peninsula, Italy): insights from integrating field survey …

A Corradetti, S Tavani, M Parente, A Iannace… - Journal of Structural …, 2018 - Elsevier
Through-going joints cutting across beds are often invoked to match large-scale
permeability patterns in tight carbonate reservoirs. However, despite the importance of these …

Karst dissolution along fracture corridors in an anticline hinge, Jandaíra Formation, Brazil: Implications for reservoir quality

FL Bagni, FH Bezerra, F Balsamo, RP Maia… - Marine and Petroleum …, 2020 - Elsevier
Folded, fractured, and karstified structures have been recognized in several carbonate
reservoirs. However, they are rarely fully identified from seismic or well data and have been …

Formation of multi-stage and clustered fractures at 3.6–4.9 km in the Shizigou structure, SW Qaidam basin

J Wu, Q Wang, X Cheng, F Cheng, X Yu… - Journal of Structural …, 2023 - Elsevier
Abstract In the Eocene Upper **aganchaigou Formation from depths of about 3.6–4.9 km in
the Shizigou (SZG) Structure in the SW Qaidam basin, core and image logs reveal three …

On the distribution of fluids in folds: A review of controlling factors and processes

MA Evans, MP Fischer - Journal of Structural Geology, 2012 - Elsevier
Growing macroscale fold structures are one of the most dynamic and complex systems in
geology, where during fold growth pore fluid pressure, fluid temperature, and fluid …