Article
Geosciences, Multidisciplinary
Sofia Alves Fornero, John M. Millett, Evandro Fernandes de Lima, Candida Menezes de Jesus, Leandro Arrais Bevilaqua, Gabriel Medeiros Marins
Summary: Sill intrusions can have a significant impact on petroleum systems in sedimentary basins, affecting source rock maturity, fluid migration, and serving as reservoirs, traps, and seals for hydrocarbons. In this study, a new approach was used to interpret geophysical borehole data for a 174 m thick sill in the Parnaiba Basin, providing insights into its emplacement mechanisms and effects on hydrocarbon migration and trapping. Integration of ultrasonic and microresistivity borehole image logs with conventional log data, petrographic analysis, and gas data revealed different rock types, anomalies in log responses, diverse inclusions, and evidence of magma mingling and assimilation processes. This study has important implications for understanding thick parallel layer intrusions and their role in fluid flow in sedimentary basins worldwide.
MARINE AND PETROLEUM GEOLOGY
(2023)
Article
Geosciences, Multidisciplinary
Mark G. Rowan, Jeff Tilton, Hermann Lebit, J. Carl Fiduk
Summary: The characteristics of thin-skinned extension detached on salt include: intersecting of basinward or landward faults with the top salt or equivalent weld, polarity of faulting may switch over time, and the oldest suprasalt strata separate into rafts with intervening younger depocenters. The base salt dipped landward in the northern and central Santos Basin, leading to minimal Albian gravity gliding, while in the Campos Basin, extension was accommodated on basinward-dipping faults. The Albian Gap in the Santos Basin formed by post-Albian thin-skinned extension with little/no extension during the Albian.
MARINE AND PETROLEUM GEOLOGY
(2022)
Article
Geochemistry & Geophysics
Leonardo M. Pichel, Christopher A-L Jackson, Frank Peel, Oriol Ferrer
Summary: This study investigates the Merluza Graben in the Santos Basin, Brazil using seismic data and structural restorations to understand the timing of salt deposition and crustal extension. It reveals that local variations in relative timing have a significant impact on salt tectonics along the margin.
Article
Geosciences, Multidisciplinary
Laura-Jane C. Fyfe, Nick Schofield, Simon P. Holford, Dougal A. Jerram, Adrian Hartley
Summary: The Little Minch Sill Complex is composed of stacked, multi-leaved Paleocene dolerite sills that intrude mainly into Mesozoic sedimentary rocks and Paleocene tuffs/hyaloclastites within the Sea of Hebrides Basin. A new assessment of the offshore extent and character of the sill complex has been constructed using high-resolution multibeam bathymetry data, providing insights into the magma flow directions within the intrusive network. This study's findings suggest that major basin-bounding faults may not play as significant a role in channelling magma through sedimentary basins as previously believed.
JOURNAL OF THE GEOLOGICAL SOCIETY
(2021)
Article
Geosciences, Multidisciplinary
Lauren Hoyer, Warwick W. Hastie
Summary: This study focuses on the morphology, intrusive relationships, and inherent structures of dolerite sills in the Karoo Large Igneous Province, South Africa. The results show directional variation in magma flow within and between the sills, emphasizing the need for careful interpretation of regional flow in sill networks.
JOURNAL OF VOLCANOLOGY AND GEOTHERMAL 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
Geosciences, Multidisciplinary
Qing Bian, Shang Deng, Huixi Lin, Jun Han
Summary: The connection between source rock and reservoir separated by salt strata is a global problem. This paper focuses on the No. 5 strike-slip fault passing through salt layers in the Tarim Basin. The seismic data reveals different structural styles in the salt layer, including transpression, transtension, and pure strikeslip. The impact of deep strike-slip salt tectonics on petroleum exploration is discussed using data from seven wells, showing that thicker salt layers result in poorer production.
MARINE AND PETROLEUM GEOLOGY
(2022)
Article
Geosciences, Multidisciplinary
Frank Zwaan, Matthias Rosenau, Daniele Maestrelli
Summary: This study systematically tested the influence of salt basin geometry on salt tectonics through analogue experiments, showing that the initial salt depocenter location and mean salt thickness are dominant factors controlling deformation. The experiments were qualitatively analyzed using top view photography, and quantitatively through Particle Image Velocimetry (PIV) and 3D photogrammetry (Structure-from-Motion, SfM) to obtain surface displacement and topographic evolution.
MARINE AND PETROLEUM GEOLOGY
(2021)
Article
Geosciences, Multidisciplinary
Simon Blondel, Massimo Bellucci, Sian Evans, Anna Del Ben, Angelo Camerlenghi
Summary: Field analogues illustrating the early stage of deformation of shortening structures in salt-bearing orogenic fold-and-thrust belts are not yet well illustrated in literature. The relatively young Messinian salt of the Algerian basin could represent a good case example of such systems. In this study, new seismic data is used to identify, classify and map salt structures throughout the central Algerian Basin and re-assess its structural style. The study found that horizontal displacement loading has driven salt deformation within the basin since its deposition, and observed variations in the structural style of the basin along- and down-dip.
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
Geosciences, Multidisciplinary
Leonardo M. Pichel, Oriol Ferrer, Christopher A-L Jackson, Eduard Roca
Summary: This study used 3D physical modeling to investigate salt tectonics in the Santos Basin, offshore Brazil. The results showed similar evolutionary patterns and structural styles to those proposed in recent studies. Additionally, the study explained the origin of salt diapirs in the Albian Gap and provided a mechanism for the formation of normal faults. This research is important for enhancing our understanding of the distribution and origin of salt-related structural styles in salt basins worldwide.
Article
Geology
Nivea G. Carramal, Daniel M. Oliveira, Alessandra S. M. Cacela, Matheus A. A. Cuglieri, Natasha P. Rocha, Samuel M. Viana, Sergio L. V. Toledo, Saulo Pedrinha, Luiz F. de Ros
Summary: This study focuses on the petrological analysis of the Aptian Barra Velha Formation in the Santos Basin, Brazil, and highlights the formation and diagenetic alteration patterns of Mg-silicates in lacustrine carbonates, which have been previously overlooked in scientific research.
JOURNAL OF SEDIMENTARY RESEARCH
(2022)
Article
Geosciences, Multidisciplinary
A. G. Mousouliotis, S. Pechlivanidou, K. Albanakis, A. Georgakopoulos, B. Medvedev
Summary: Salt-bearing basins are commonly deformed due to gravity mechanisms and regional tectonics, with the study area in the eastern part of the Herodotus Basin showing deformation associated with the flow of Messinian salt deposited during the Messinian Salinity Crisis. The research reveals significant thickness variations of the salt sequence and overlying sediments, as well as distinct salt-tectonic structural provinces characterized by different deformation styles. The compressional thickening of the Messinian salt driven by gravity mechanisms results in the absence of a bathymetric step on the seafloor in the western side of the study area.
MARINE AND PETROLEUM GEOLOGY
(2021)
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
Geochemistry & Geophysics
M. F. Doring, J. Julia, M. Evain
Summary: The crustal structure of the Reconcavo-Tucano basin in NE Brazil was investigated, revealing that the crust is over 40 km thick beneath the basin and contains a layer of high velocity material. Comparisons with neighboring regions show that the crust in the basin is thicker and has higher lower crustal velocities. The results support models of basin formation involving pure shear extension in the lower crust.
GEOPHYSICAL JOURNAL INTERNATIONAL
(2022)
Article
Geochemistry & Geophysics
David Redpath, Christopher A-L Jackson, Rebecca E. Bell
Summary: Mechanical stratigraphy plays a crucial role in the growth of normal faults, controlling their geometry and kinematics. This study examines normal faults formed in a deep-water clastic succession offshore Angola, and finds that the presence of a mass-transport complex (MTC) influences the growth patterns of the faults. Faults that offset the MTC have greater throw and propagate downward, while faults that terminate at the MTC have smaller throw. These findings highlight the significant control of mechanical stratigraphy on fault development.
Article
Geosciences, Multidisciplinary
Leonardo M. Pichel, Oriol Ferrer, Christopher A-L Jackson, Eduard Roca
Summary: This study used 3D physical modeling to investigate salt tectonics in the Santos Basin, offshore Brazil. The results showed similar evolutionary patterns and structural styles to those proposed in recent studies. Additionally, the study explained the origin of salt diapirs in the Albian Gap and provided a mechanism for the formation of normal faults. This research is important for enhancing our understanding of the distribution and origin of salt-related structural styles in salt basins worldwide.
Article
Geochemistry & Geophysics
Aurio Erdi, Christopher A-L Jackson
Summary: This study examines the structure and growth of salt-detached strike-slip faults using a 3D seismic reflection dataset from the Outer Kwanza Basin offshore Angola. The findings suggest that these faults formed to accommodate variations in differential seaward translation and salt diapirism. The growth of the fault arrays occurred through tip propagation of isolated fault segments, with some segments linking during specific time periods. The results also highlight the scatter in the D-L scaling of strike-slip faults, reflecting the propagation, interaction, and linkage of individual fault segments.
Letter
Geosciences, Multidisciplinary
Craig Magee, Matthew T. Reeve, Christopher A. -L. Jackson, Rebecca E. Bell, Ian D. Bastow
Article
Geosciences, Multidisciplinary
Aurio Erdi, Christopher A. -L. Jackson, Juan I. Soto
Summary: This study investigates the temporal and spatial evolution of thin-skinned deformation on the Tarakan Basin in offshore eastern Indonesia using 3D seismic reflection data. The results reveal concave- and convex-into-the-basin normal faults on a basal mobile shale, with normal faulting and shale mobilization starting in the Middle Miocene. The growth faults and anticlines in the delta system are influenced by variations in sedimentary loading, mobile-shale flow, and the trend and dip of the base mobile-shale surface.
Article
Geosciences, Multidisciplinary
Amir Joffe, Christopher A. -L. Jackson, Leonardo M. M. Pichel
Summary: Salt tectonics is primarily driven by the movement of evaporites due to gravity gliding and differential loading. Understanding the complexities of salt basins is crucial, especially when carbonate and clastic rocks interbed with evaporitic strata. Using seismic reflection and borehole data, we analyze the formation and deformation of minibasins within the Zechstein Supergroup in the Devil's Hole Horst, UK. Our findings refine the depositional model for the Central North Sea and provide insights into syn-depositional salt flow in layered evaporitic sequences and its impact on petroleum plays.
Article
Geosciences, Multidisciplinary
Thilo Wrona, Alexander C. Whittaker, Rebecca E. Bell, Robert L. Gawthorpe, Haakon Fossen, Christopher A. -L. Jackson, Marit Stokke Bauck
Summary: This study utilizes new 3D seismic reflection data from the northern North Sea to reveal a continental rift landscape dating back to the Late Permian-Early Triassic. The landscape, preserved by a combination of tectonic faults and burial sediments, provides valuable insights into the tectono-stratigraphic evolution of ancient continental rifts.
Article
Geology
Nan Wu, Christopher A. L. Jackson, Michael A. Clare, David M. Hodgson, Harya D. Nugraha, Michael J. Steventon, Guangfa Zhong
Summary: In this study, we used seismic reflection, geochemical, and petrophysical data to investigate how the physical properties of oozes control slope failure and emplacement processes. We discovered potential slide surfaces within ooze successions, which is crucial for improved submarine geohazard assessment. Additionally, we found that tectonics, ocean current activity, and silica diagenesis can prime multiple slides on low-gradient slopes in tropical oceanic basins.
Article
Geology
Ander Martinez-Donate, Ian A. A. Kane, David M. M. Hodgson, Aurelia M. L. J. Privat, Christopher A. L. Jackson, Ernesto Schwarz, Stephen S. S. Flint
Summary: The Los Molles Formation in the Neuquen Basin of Argentina provides a rare opportunity to study syn-rift to post-rift stratigraphy. A field-based study in the Chachil Graben revealed the stratigraphic evolution of two deep-marine intraslope lobe complexes, which were built by different types of flows and exhibited differences in their characteristics. Petrographic analysis further showed that the lobe complexes are volcanic arc-sourced. The study also proposed a model for intraslope lobe complex development and highlighted the importance of flow behavior and transformation in understanding their hydrocarbon reservoir potential.
Article
Geosciences, Multidisciplinary
Lise Nakken, Domenico Chiarella, Christopher A-L. Jackson
Summary: In this study, a model of the Late Jurassic rift physiography of the Froan Basin and Froya High is presented based on seismic reflection, well data, and reverse subsidence modelling. The results show that major footwall uplift during the Late Jurassic to Early Cretaceous caused the Froya High and the western margin of the central Froan Basin to be subaerially exposed, forming an intra-rift footwall island. Shallow marine areas to the east accumulated sediment supplied from the uplifted and partially eroded footwall, while the Trondelag Platform remained submerged throughout the rift episode.
Article
Geosciences, Multidisciplinary
Liu Cao, Qiliang Sun, Craig Magee
Summary: Structures facilitating fluid migration above a late Cretaceous volcanic field in the Great South Basin, offshore New Zealand, have been documented. Three vertically stacked vents suggest episodic re-use of the same fluid pathway between approximately 75 and 56 million years ago (Ma). The presence of a ca. 49 Ma palaeo-pockmark and free gas in strata ca. 21 million years old directly above these stacked vents implies the re-utilization of fluid migration pathways over a period of over 54 million years. The findings have important implications for hydrocarbon/geothermal exploration and geohazard assessment.
Article
Geosciences, Multidisciplinary
Francyne Bochi do Amarante, Juliano Kuchle, Christopher Aiden-Lee Jackson, Claiton Marlon dos Santos Scherer, Leonardo Muniz Pichel
Summary: Rift basins typically go through three main tectono-stratigraphic stages: pre-, syn- and post-rift. The syn-rift stage is characterized by the deposition of asymmetric growth strata wedges due to active normal faulting, while the subsequent post-rift stage is defined by long-wavelength subsidence driven by lithospheric cooling.
Article
Geochemistry & Geophysics
Edoseghe E. Osagiede, Casey W. Nixon, Rob Gawthorpe, Atle Rotevatn, Haakon Fossen, Christopher A. -L. Jackson, Fabian Tillmans
Summary: The spatial variation of the topological characteristics of normal fault networks at the rift-scale is investigated using 3D seismic reflection data from the northern North Sea. It is found that fault orientation varies spatially along the rift margin, with different dominant strikes in fault blocks adjacent to the graben compared to those farther from the graben. Two broad topological domains are identified within the fault network, which correlate with the sub-division of the rift margin into different structural domains. There is also a positive correlation between fault orientations and intensity, highlighting the relationship between fault geometry and topology.
Article
Geology
Nan Wu, Christopher A. L. Jackson, Michael A. Clare, David M. Hodgson, Harya D. Nugraha, Michael J. Steventon, Guangfa Zhong
Summary: This study investigates the impact of changes in physical properties of oozes during burial on slope stability and geohazards. The researchers used various data, including seismic reflection, geochemical, and petrophysical data, to analyze submarine slides on the Exmouth Plateau. The findings highlight the importance of considering the diagenetic state of silica-rich sediments in future slope stability assessments.