Article
Geochemistry & Geophysics
Jafar Hassanpour, Josep Anton Munoz, Ali Yassaghi, Oriol Ferrer, Salman Jahani, Pablo Santolaria, Seyed Mohsen SeyedAli
Summary: The study uses interpretation of reflection seismic profiles, sequential restoration, and physical modelling to understand the kinematics of salt flow and diapirism in the Eastern Persian Gulf offshore Southern Iran. Salt tectonics in the area are caused by overlapping Ediacaran-Early Cambrian Hormuz Salt and Oligocene-Early Miocene Fars Salt. The flow of Fars Salt is mainly triggered by differential sedimentary loading and its lateral flow kinematics is controlled by the behavior of underlying Hormuz-Salt sheets.
Article
Geosciences, Multidisciplinary
Md Nahidul Hasan, Paul Mann
Summary: Based on marine geological research milestones, the late Jurassic Campeche salt basin in the southern Gulf of Mexico is related to the late Middle Miocene to Recent geological structures. The study reconstructed the geometry of the top of the Paleozoic basement and base-salt topography using shipborne magnetic data and 28,612 km of pre-stack, depth-migrated, 2D seismic data. The Campeche segment of the Gulf of Mexico outer marginal trough, which is 40-55 km wide, marks the limit of the northwest-directed passive margin foldbelt.
MARINE AND PETROLEUM GEOLOGY
(2021)
Article
Geosciences, Multidisciplinary
Michael R. Hudec, Frank J. Peel, Juan I. Soto, Gillian M. Apps
Summary: The East Breaks foldbelt is formed by slope-parallel folds and thrusts detached on a salt canopy on the northern Gulf of Mexico slope. Structures in the foldbelt are attributed to convergent gravity gliding caused by the bend in topography in the northwest Gulf of Mexico. Convergent deformation was localized in the East Breaks foldbelt because it was a shale-dominated slope between sand-prone slope aprons during the Oligocene.
MARINE AND PETROLEUM GEOLOGY
(2023)
Article
Geochemistry & Geophysics
Dan M. Tamas, Alexandra Tamas, Jessica Barabasch, Mark G. Rowan, Zsolt Schleder, Csaba Krezsek, Janos L. Urai
Summary: This study focuses on an intrasalt, sub-horizontal shear zone in the Romanian Eastern Carpathians, shedding light on the formation and evolution of salt structures and providing a detailed description of the unique geological features of salt-cored anticlines.
Article
Environmental Sciences
Mohammad Mohammadhasani, Fateme Kamali, Ahmad Rashidi, Mobin Bahrampour, Shahram Shafieibafti, Razieh Abbaspour, Reza Derakhshani
Summary: Geohazards, including earthquakes, pose a significant threat to human life and infrastructure globally, and Iran is particularly vulnerable due to its unique structural characteristics. Therefore, monitoring geohazards to mitigate their impacts is crucial. Radar interferometry has emerged as an accurate and cost-effective method, capable of operating under all weather conditions 24/7. This study utilized Sentinel 1A images and radar interferometry to investigate surface changes following earthquakes in the Persian Gulf region, revealing significant uplift and subsidence near Bandar Khamir and Bandar Charak.
Article
Geochemistry & Geophysics
Giulio Casini, Jaume Verges, Peter Drzewiecki, Mary Ford, David Cruset, Wayne Wright, David Hunt
Summary: The reinterpretation of the Organya Basin highlights the importance of Upper Triassic evaporites in the tectono-sedimentary evolution of the South-Central Pyrenees. The study integrates new field observations and subsurface data to create a restored cross-section that shows the template of the northern Iberian salt-rich rifted margin. The diapiric activity along this margin is divided into three stages: early salt mobilization in the Jurassic, main diapiric evolution from the late Jurassic to the middle Albian, and diapiric reactivation during basin inversion from the Campanian to the Miocene.
Article
Geochemistry & Geophysics
Giulio Casini, Jaume Verges, Peter Drzewiecki, Mary Ford, David Cruset, Wayne Wright, David Hunt
Summary: The reinterpretation of the Organya Basin highlights the importance of Upper Triassic evaporites in the tectono-sedimentary evolution of the South-Central Pyrenees. Detailed field observations and subsurface data are incorporated to reconstruct a cross-section through the Serres Marginals, Montsec, and eastern Organya salt-related depocenters. This study reveals three stages of diapiric activity along the northern Iberian margin, contributing to the understanding of the salt-rich rifted margin.
Article
Geosciences, Multidisciplinary
Jean Joseph Hooghvorst, Maria A. Nikolinakou, Toby W. D. Harrold, Oscar Fernandez, Peter B. Flemings, Alejandro Marcuello
Summary: This study systematically incorporates various parameters into a model to simulate the formation of the Sandia salt diapir on the NW African Coast, and finds that changes in sedimentation rates are a key control on the kinematic evolution of the salt system.
Article
Geosciences, Multidisciplinary
Zahra Tajmir Riahi, Khalil Sarkarinejad, Ali Faghih, Bahman Soleimany, Gholam Reza Payrovian
Summary: The study revealed that the Nourooz-Hendijan-Izeh Fault is a segmented pre-existing basement fault that underwent reactivation in at least seven tectonic phases. Inversion tectonics affected hydrocarbon trap development in the Late Cretaceous and controlled their current conditions in the NW Persian Gulf and the southern Dezful Embayment. Mild to moderate inversion structures are considered preferred petroleum exploration targets in the region.
MARINE AND PETROLEUM GEOLOGY
(2021)
Article
Geosciences, Multidisciplinary
Maditha Kurz, Oscar Fernandez, Lino Eggerth, Bernhard Grasemann, Philipp Strauss
Summary: This article describes a fossil salt sheet emplaced in submarine conditions in the Eastern Alps of Austria during the Jurassic period, providing valuable insights into the emplacement of similar structures and their impact on depositional systems. The salt sheet, formed from the squeezing of a salt diapir under compression, exhibits a mylonitic shear fabric indicating its radial emplacement towards the south. The study also documents the tectono-sedimentary relationships of the salt structure, including its initial growth, extrusion, and subsequent collapse, with syn-extrusion sediments indicating the variable bathymetry associated with the extruding salt sheet.
Article
Geosciences, Multidisciplinary
Blessing Adeoti, A. Alexander G. Webb
Summary: The Kuqa fold-thrust belt in China is known for its diverse surface salt structures. By studying the geomorphological features of lateral ridge propagation along the belt, researchers have found evidence supporting the formation of the belt through a combination of detachment folding and source-fed thrust faults.
JOURNAL OF STRUCTURAL GEOLOGY
(2022)
Article
Geochemistry & Geophysics
Stefan Back, Sebastian Amberg, Victoria Sachse, Ralf Littke
Summary: This article discusses the application of Archimedes' principle in the study of salt mine reconstruction. By using a three-dimensional sequential removal method, the surface of the salt mine is reconstructed, and the flow and redistribution of underground salt are analyzed. This research is of great significance for understanding the movement of underground salt and the impact of external forces.
Article
Geochemistry & Geophysics
Zachary F. M. Burton, Laura N. Dafov
Summary: This study proposes and demonstrates salt movement, particularly diapirism, as a new mechanism for the recycling of marine gas hydrates (GH). The research shows that salt diapir movement can significantly increase GH volumes and saturations. The results suggest that GH systems associated with salt diapir crests are attractive targets for hydrocarbon resource exploration and scientific drilling expeditions.
GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS
(2023)
Article
Geosciences, Multidisciplinary
Debora Duarte, Cristina Roque, Zhi Lin Ng, F. Javier Hernandez-Molina, Vitor Hugo Magalhaes, Sonia Silva, Estefania Llave
Summary: The Gulf of Cadiz Contourite Depositional System (GCCS) formation and evolution are controlled by tectonic activity, with structural features and tectonic events having a significant impact on seafloor relief and local oceanic circulation processes.
Article
Geosciences, Multidisciplinary
J. Obradors-Prats, E. E. Calderon Medina, S. J. Jones, M. Rouainia, A. C. Aplin, A. J. L. Crook
Summary: The multi-well pressure data from the Magnolia Field in the Gulf of Mexico reveal high and varying overpressures between sand bodies, which is mainly caused by rapid deposition of mud-rich sediments and tectonic loading. A 2D forward hydro-mechanical evolutionary model shows that disequilibrium compaction accounts for most of the observed overpressure, while tectonic loading contributes to a smaller extent. The model also demonstrates that small variations in permeability and connectivity of mud-rich sections result in compartmentalised pressure distributions in adjacent sand bodies.
MARINE AND PETROLEUM GEOLOGY
(2023)
Article
Geosciences, Multidisciplinary
Philipp Strauss, Pablo Granado, Josep Anton Munoz
Summary: The study found that salt expulsion led to the rapid growth of Triassic carbonate platforms in the eastern Northern Calcareous Alps, with salt expulsion being proportional to the growth potential of the carbonate producers. The results help explain the development of isolated carbonates platforms in the region and differentiate between mechanisms controlling accommodation space.
Article
Geosciences, Multidisciplinary
Mansoure Montahaei, Pilar Queralt, Juanjo Ledo, Behrooz Oskooi, Josep A. Munoz, Alex Marcuello
Summary: The study reveals distinct conductive structures within the crust in the central Zagros collision zone, influenced by local and regional stresses and rheological contrasts. The joint interpretation of magnetotelluric inverse modeling and seismicity data sheds light on fluid generation influencing rock deformation and seismicity in the region.
GEOSCIENCES JOURNAL
(2021)
Article
Geochemistry & Geophysics
Sebastian G. Wolf, Ritske S. Huismans, Josep-Anton Munoz, Magdalena Ellis Curry, Peter van der Beek
Summary: The interaction between crustal thickening and surface processes plays a key role in the growth of continent-continent collision orogens. Internal crustal loading and lithospheric pull are the main factors controlling large scale evolution, while surface process efficiency influences foreland-basin filling and orogen core exhumation. Inherited structures, surface processes, and decoupling between thin-and thick-skinned deformation affect structural style during orogenic growth.
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH
(2021)
Article
Geosciences, Multidisciplinary
Stefano Tavani, Pablo Granado, Amerigo Corradetti, Giovanni Camanni, Gianluca Vignaroli, Gianreto Manatschal, Stefano Mazzoli, Josep A. Munoz, Mariano Parente
Summary: In accretionary convergent margins, the re-localization of decollements is influenced by inherited rift-related structures, with deep decollements forming in the proximity of pre-orogenic rift systems. The ductile middle crust's preservation during rifting and reactivation as a decollement in the thrust system lead to underplating, metamorphism, and final emplacement of tectonic units.
GEOLOGICAL SOCIETY OF AMERICA BULLETIN
(2021)
Article
Geology
Magdalena Ellis Curry, Peter van der Beek, Ritske S. Huismans, Sebastian G. Wolf, Charlotte Fillon, Josep-Anton Munoz
Summary: By studying large-scale thermokinematic modeling of the Pyrenees mountains, it was found that the pattern of exhumation is primarily controlled by structural inheritance, with ancillary patterns reflecting growth and erosion of the antiformal stack as well as post-orogenic surface processes.
Article
Geochemistry & Geophysics
R. Lescoutre, G. Manatschal, J. A. Munoz
Summary: This study reveals that the orogenic architecture at the Pyrenean-Cantabrian junction results from the decoupling between thick-skinned and thin-skinned modes of deformation. It identifies two phases of rifting and related basins and emphasizes the role of inheritance during rifting and reactivation. The results suggest a NNE-SSW direction of extension during the mid-Cretaceous, discarding the existence of a major Pamplona transfer fault.
Article
Geosciences, Multidisciplinary
Pablo Granado, Jonas B. Ruh, Pablo Santolaria, Philipp Strauss, Josep Anton Munoz
Summary: This study presents a series of 2D thermo-mechanical numerical experiments on thick-skinned crustal extension, including a pre-rift salt horizon and different styles of convergence. The results show that extension along steep basement faults can produce half-graben structures and lead to changes in the distribution of pre-rift salt. The rate of thick-skinned extension and the rheology of salt control the accommodation space and timing of minibasin grounding.
FRONTIERS IN EARTH SCIENCE
(2021)
Editorial Material
Geosciences, Multidisciplinary
Philipp Strauss, Pablo Granado, Josep Anton Munoz
Summary: The study demonstrates that salt expulsion facilitated the rapid growth of isolated deep depocenters in Triassic carbonate platforms in the eastern Northern Calcareous Alps. With excellent biostratigraphic control and precise knowledge of paleo-bathymetry, a well-defined subsidence model was established.
Article
Geochemistry & Geophysics
Jafar Hassanpour, Josep Anton Munoz, Ali Yassaghi, Oriol Ferrer, Salman Jahani, Pablo Santolaria, Seyed Mohsen SeyedAli
Summary: The study uses interpretation of reflection seismic profiles, sequential restoration, and physical modelling to understand the kinematics of salt flow and diapirism in the Eastern Persian Gulf offshore Southern Iran. Salt tectonics in the area are caused by overlapping Ediacaran-Early Cambrian Hormuz Salt and Oligocene-Early Miocene Fars Salt. The flow of Fars Salt is mainly triggered by differential sedimentary loading and its lateral flow kinematics is controlled by the behavior of underlying Hormuz-Salt sheets.
Article
Geosciences, Multidisciplinary
Mark G. Rowan, Josep Anton Munoz, Eduard Roca, Oriol Ferrer, Pablo Santolaria, Pablo Granado, Marco Snidero
Summary: In this study, seismic data from the Sureste Basin in offshore SE Mexico is used to map and analyze two different structures. The results show that while analog models can reproduce some seismic geometries, there are also mismatches. Additionally, the dip angles of faults in the study area are steeper than those predicted by the models. Observations from other salt basins are brought in to discuss these discrepancies and suggest improvements for the applicability of models to real-world scenarios.
JOURNAL OF STRUCTURAL GEOLOGY
(2022)
Article
Geology
C. Evelyn Gannaway Dalton, Katherine A. Giles, Josep Anton Munoz, Mark G. Rowan
Summary: This study investigates the depositional facies and stratal architecture of the Aulet and Adons diapirs in the Ribagorca Basin in the Pyrenees. The research provides insights into the origin and evolution of these diapirs and their associated minibasins. The findings suggest that the depositional systems in the minibasins evolved in response to extension, salt evacuation, and passive diapirism during the Pyrenean rift and postrift phases. The study also highlights the importance of integrating sedimentological and stratigraphic evidence into structural interpretations.
JOURNAL OF SEDIMENTARY RESEARCH
(2022)
Article
Geosciences, Multidisciplinary
Rodolfo M. Uranga, Oriol Ferrer, Gonzalo Zamora, Josep A. Munoz, Mark G. Rowan
Summary: Salt tectonics plays a critical role in the evolution of passive margins, and this study highlights key events in the evolution of the Tarfaya Basin in Morocco through interpretation of seismic data.
MARINE AND PETROLEUM GEOLOGY
(2022)
Article
Environmental Sciences
Laura Blanco, David Garcia-Selles, Marta Guinau, Thanasis Zoumpekas, Anna Puig, Maria Salamo, Oscar Gratacos, Josep Anton Munoz, Marc Janeras, Oriol Pedraza
Summary: Rock slope monitoring using 3D point cloud data enables the creation of rockfall inventories, and a new methodology with machine learning techniques is proposed to identify rockfalls from compared temporary 3D point clouds.
Article
Geosciences, Multidisciplinary
Amir Kalifi, Charlotte Ribes, Pierre Dietrich, Emmanuel Dujoncquoy, Josep-Anton Munoz, Jean -Paul Callot, Jean-Claude Ringenbach
Summary: This paper provides a tectonostratigraphic framework of the Cotiella minibasins in the Pyrenees, Spain, to assess the influence of salt structures on facies distribution, stratal pattern, and thickness trends. The results show that the influence of halokinesis on sedimentation patterns, thickness trends, and depocenter localization is significant.
MARINE AND PETROLEUM GEOLOGY
(2023)