[HTML][HTML] Fluid evolution from extension to compression in the Pyrenean Fold Belt and Basque-Cantabrian Basin: A review
We propose a review to discuss the large number of studies dealing with the fluid history in
extensional and compressional sedimentary basins that evolved along the Iberian-Eurasian …
extensional and compressional sedimentary basins that evolved along the Iberian-Eurasian …
[HTML][HTML] Spatio-temporal variation of fluid flow behavior along a fold: the Bóixols-Sant Corneli anticline (Southern Pyrenees) from U–Pb dating and structural …
This study integrates field structural data, petrographic and geochemical (δ 18 O, δ 13 C, Δ
47, 87 Sr/86 Sr, and elemental composition) analyses and U–Pb dating of calcite veins …
47, 87 Sr/86 Sr, and elemental composition) analyses and U–Pb dating of calcite veins …
[HTML][HTML] Petrological, petrophysical and petrothermal study of a folded sedimentary succession: the Oliana anticline (Southern Pyrenees), outcrop analogue of a …
P Ramirez-Perez, I Cantarero, G Cofrade… - Global and Planetary …, 2023 - Elsevier
Abstract The Oliana anticline (Southern Pyrenees) has been characterized as an outcrop
analogue of a geothermal reservoir using field data (stratigraphy and fracturing) and …
analogue of a geothermal reservoir using field data (stratigraphy and fracturing) and …
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 …
Reconstructing the Iberian salt‐bearing rifted margin of the Southern Pyrenees: Insights from the Organyà Basin
Reinterpretation of the Organyà Basin, based on new detailed field observations and
subsurface data, emphasizes the key contribution of Upper Triassic evaporites in the tectono …
subsurface data, emphasizes the key contribution of Upper Triassic evaporites in the tectono …
Multiple fluid flow events from salt‐related rifting to basin inversion (Upper Pedraforca thrust sheet, SE Pyrenees)
Fluid systems in inverted rifted margins are challenging to interpret because fractures
formed before compression were often reactivated acting as fluid pathways as new ones …
formed before compression were often reactivated acting as fluid pathways as new ones …
Passive structural control on skarn mineralization localization: A case study from the Variscan Rosas Shear Zone (SW Sardinia, Italy)
F Cocco, A Attardi, ML Deidda, D Fancello, A Funedda… - Minerals, 2022 - mdpi.com
The case study presented here deals with the Pb-Zn-Cu skarn ores hosted in the Rosas
Shear Zone (RSZ), a highly strained domain located in the external zone of the Sardinian …
Shear Zone (RSZ), a highly strained domain located in the external zone of the Sardinian …
Origin and distribution of calcite cements in a folded fluvial succession: The Puig‐reig anticline (south‐eastern Pyrenees)
As one of the predominant diagenetic products in clastic rocks, calcite cements are typical
fingerprints of cement‐forming fluids and are key controls on reservoir quality. The Puig‐reig …
fingerprints of cement‐forming fluids and are key controls on reservoir quality. The Puig‐reig …
[HTML][HTML] Fracture distribution in a folded fluvial succession: the Puig-reig anticline (South-eastern Pyrenees)
X Sun, E Gomez-Rivas, J Alcalde… - Marine and Petroleum …, 2021 - Elsevier
Sedimentary rocks of foreland fold-and-thrust belts typically undergo intensive fracturing as
folds grow. The resulting fracture networks can present significant variations depending on …
folds grow. The resulting fracture networks can present significant variations depending on …
Episodic reactivation of carbonate fault zones with implications for permeability–An example from Provence, Southeast France
Exposed in large, continuous outcrops in Provence, southern France, the Castellas fault
formed as a normal fault in the Upper Cretaceous and was reactivated as a left-lateral fault …
formed as a normal fault in the Upper Cretaceous and was reactivated as a left-lateral fault …