Basin Research

Papers
(The TQCC of Basin Research is 7. The table below lists those papers that are above that threshold based on CrossRef citation counts [max. 250 papers]. The publications cover those that have been published in the past four years, i.e., from 2020-04-01 to 2024-04-01.)
ArticleCitations
Clinoforms and clinothems: Fundamental elements of basin infill45
Reconstruction of the Cenozoic deformation of the Bohai Bay Basin, North China36
Regional correlation and seismic stratigraphy of Triassic Strata in the Greater Barents Sea: Implications for sediment transport in Arctic basins23
Subsidence analysis of salt tectonics‐driven carbonate minibasins (Northern Calcareous Alps, Austria)22
Salt–magma interactions influence intrusion distribution and salt tectonics in the Santos Basin, offshore Brazil22
Tectonic inversion assessed by integration of geological and geophysical data: The intracontinental Rio do Peixe Basin, NE Brazil22
Early Cenozoic activated deformation in the Qilian Shan, northeastern Tibetan Plateau: Insights from detrital apatite fission‐track analysis21
Low‐temperature thermochronology as a control on vertical movements for semi‐quantitative source‐to‐sink analysis: A case study for the Permian to Neogene of Morocco and surroundings21
Burial dolomitization driven by modified seawater and basal aquifer‐sourced brines: Insights from the Middle and Upper Devonian of the Western Canadian Sedimentary Basin20
Salt tectonics in a double salt‐source layer setting (Eastern Persian Gulf, Iran): Insights from interpretation of seismic profiles and sequential cross‐section restoration20
Using Mesoproterozoic sedimentary geochemistry to reconstruct basin tectonic geography and link organic carbon productivity to nutrient flux from a Northern Australian large igneous Province19
Fault‐controlled base‐of‐scarp deposits19
Tectono‐sedimentary evolution of Jurassic–Cretaceous diapiric structures: Miravete anticline, Maestrat Basin, Spain19
Review of Iberia–Eurasia plate‐boundary basins: Role of sedimentary burial and salt tectonics during rifting and continental breakup18
Leaky salt: Pipe trails record the history of cross‐evaporite fluid escape in the northern Levant Basin, Eastern Mediterranean18
Turbidites, topography and tectonics: Evolution of submarine channel‐lobe systems in the salt‐influenced Kwanza Basin, offshore Angola18
Unravelling the widening of the earliest Andean northern orogen: Maastrichtian to early Eocene intra‐basinal deformation in the northern Eastern Cordillera of Colombia17
Extensional tectonics during the Tyrrhenian back‐arc basin formation and a new morpho‐tectonic map17
The Svalbard Eocene‐Oligocene (?) Central Basin succession: Sedimentation patterns and controls17
LA‐ICP‐MS dating of detrital zircon grains from the Cretaceous allochthonous bauxites of Languedoc (south of France): Provenance and geodynamic consequences17
From widespread faulting to localised rifting: Evidence from K‐Ar fault gouge dates from the Norwegian North Sea rift shoulder17
Rift interaction zones and the stages of rift linkage in active segmented continental rift systems17
Basement geology and its controls on the nucleation and growth of rift faults in the northern Campos Basin, offshore Brazil17
Long‐distance fluid migration defines the diagenetic history of unique Ediacaran sediments in the East European Craton16
Pre‐salt rift morphology controls salt tectonics in the Campos Basin, offshore SE Brazil16
Supradetachment to rift basin transition recorded in continental to marine deposition; Paleogene Bandar Jissah Basin, NE Oman16
Detrital zircons record the evolution of the Cathaysian Coastal Mountains along the South China margin15
Evolution of normal fault displacement and length as continental lithosphere stretches15
Strain migration during multiphase extension, Stord Basin, northern North Sea rift15
The Rosebank Field, NE Atlantic: Volcanic characterisation of an inter‐lava hydrocarbon discovery15
Signatures of tectonic‐climatic interaction during the Late Cenozoic orogenesis along the northern Chinese Tian Shan14
Development of an incipient Paleogene topography between the present‐day Eastern Andean Plateau (Puna) and the Eastern Cordillera, southern Central Andes, NW Argentina14
Reutilisation of hydrothermal vent complexes for focused fluid flow on continental margins (Modgunn Arch, Norwegian Sea)14
The structural evolution of pull‐apart basins in response to changes in plate motion14
Constraining recycled detritus in quartz‐rich sandstones: Insights from a multi‐proxy provenance study of the Mid‐Carboniferous, Clare Basin, western Ireland13
Pliocene–Pleistocene glacimarine shelf to slope processes in the south‐western Barents Sea13
Transcontinental retroarc sediment routing controlled by subduction geometry and climate change (Central and Southern Andes, Argentina)13
Assessing first‐order BQART estimates for ancient source‐to‐sink mass budget calculations13
Testing normal fault growth models by seismic stratigraphic architecture: The case of the Pliocene‐Quaternary Fucino Basin (Central Apennines, Italy)13
Evolution of a mixed siliciclastic‐carbonate deep‐marine system on an unstable margin: The Cretaceous of the Eastern Greater Caucasus, Azerbaijan13
Reconstructing the level of the central Red Sea evaporites at the end of the Miocene13
Reactivation of a hyperextended rift system: The Basque–Cantabrian Pyrenees case12
Straight from the source's mouth: Controls on field‐constrained sediment export across the entire active Corinth Rift, central Greece12
Mixed axial and transverse deep‐water systems: The Cretaceous post‐rift Lysing Formation, offshore Norway12
From rifting to hyperextension: Upper Jurassic–Lower Cretaceous tectono‐stratigraphy of the Porcupine Basin, Irish Atlantic Margin12
Cretaceous continental margin evolution revealed using quantitative seismic geomorphology, offshore northwest Africa12
Sedimentary response to a collision orogeny recorded in detrital zircon provenance of Greater Caucasus foreland basin sediments12
The formation of the Sichuan Basin, South China, during the Late Ediacaran to Early Cambrian12
Forebulge migration in the foreland basin system of the central‐southern Apennine fold‐thrust belt (Italy): New high‐resolution Sr‐isotope dating constraints12
Multiple fluid flow events from salt‐related rifting to basin inversion (Upper Pedraforca thrust sheet, SE Pyrenees)12
A regional CO2 containment assessment of the northern Utsira Formation seal and overburden, northern North Sea11
The formation and implications of giant blocks and fluid escape structures in submarine lateral spreads11
Syn‐rift sediment gravity flow deposition on a Late Jurassic fault‐terraced slope, northern North Sea11
Evaluating sediment recycling through combining inherited petrogenic and acquired sedimentary features of multiple detrital minerals11
Volcanic facies architecture of early bimodal volcanism of the NW Deccan Traps: Volcanic reservoirs of the Raageshwari Deep Gas Field, Barmer Basin, India11
Competition between 3D structural inheritance and kinematics during rifting: Insights from analogue models11
Quantifying the relationship between structural deformation and the morphology of submarine channels on the Niger Delta continental slope11
Chlorite coating patterns and reservoir quality in deep marine depositional systems – Example from the Cretaceous Agat Formation, Northern North Sea, Norway11
Quartz overgrowth textures and fluid inclusion thermometry evidence for basin‐scale sedimentary recycling: An example from the Mesozoic Barents Sea Basin11
Evaluating alluvial stratigraphic response to cyclic and non‐cyclic upstream forcing through process‐based alluvial architecture modelling11
The syn‐rift tectono‐stratigraphic record of rifted margins (Part I): Insights from the Alpine Tethys10
The Messinian Salinity Crisis as a trigger for high pore pressure development in the Western Mediterranean10
Characterization of Late Cretaceous to Miocene source rocks in the Eastern Mediterranean Sea: An integrated numerical approach of stratigraphic forward modelling and petroleum system modelling10
Volcanic events‐related hydrothermal dolomitisation and silicification controlled by intra‐cratonic strike‐slip fault systems: Insights from the northern slope of the Tazhong Uplift, Tarim Basin, Chin10
The syn‐rift tectono‐stratigraphic record of rifted margins (Part II): A new model to break through the proximal/distal interpretation frontier10
Integrated on‐land‐offshore stratigraphy of the Campi Flegrei caldera: New insights into the volcano‐tectonic evolution in the last 15 kyr10
Determining the tempo of exhumation in the eastern Himalaya: Part 1. Geometry, kinematics and predicted cooling ages10
Tidal amplification and along‐strike process variability in a mixed‐energy paralic system prograding onto a low accommodation shelf, Edgeøya, Svalbard10
Principles of shortening in salt basins containing isolated minibasins10
Quantitative analysis of a footwall‐scarp degradation complex and syn‐rift stratigraphic architecture, Exmouth Plateau, NW Shelf, offshore Australia10
Topographic growth of the northeastern Tibetan Plateau during the middle‐late Miocene: Insights from integrated provenance analysis in the NE Qaidam Basin10
Intelligent identification of sequence stratigraphy constrained by multipopulation genetic algorithm and dynamic time warping technique: A case study of Lower Cretaceous Qingshuihe Formation in hinter10
The transition from salt diapir to weld and thrust: Examples from the Northern Flinders Ranges in South Australia10
Influence of orographic precipitation on the topographic and erosional evolution of mountain ranges9
Impact of growth faults on mixed siliciclastic‐carbonate‐evaporite deposits during rift climax and reorganisation—Billefjorden Trough, Svalbard, Norway9
The Middle Jurassic to lowermost Cretaceous in the SW Barents Sea: Interplay between tectonics, coarse‐grained sediment supply and organic matter preservation9
Geomorphological characterization of basal flow markers during recurrent mass movement: A case study from the Taranaki Basin, offshore New Zealand9
The interactions of volcanism and clastic sedimentation in rift basins: Insights from the Palaeogene‐Neogene Shaleitian uplift and surrounding sub‐basins, Bohai Bay Basin, China9
Effects of basement structures and Carboniferous basin configuration on evaporite distribution and the development of salt structures in Nordkapp Basin, Barents Sea—Part I9
Tracing erosion patterns in South Tibet: Balancing sediment supply to the Yarlung Tsangpo from the Himalaya versus Lhasa Block9
Impact of Late Cretaceous inversion and Cenozoic extension on salt structure growth in the Baltic sector of the North German Basin9
Sediment dispersal pathways in the Po coastal plain since the Last Glacial Maximum: Provenance signals of autogenic and eustatic forcing9
10 Myr evolution of sedimentation rates in a deep marine to non‐marine foreland basin system: Tectonic and sedimentary controls (Eocene, Tremp–Jaca Basin, Southern Pyrenees, NE Spain)9
Low‐accommodation and backwater effects on sequence stratigraphic surfaces and depositional architecture of fluvio‐deltaic settings (Cretaceous Mesa Rica Sandstone, Dakota Group, USA)9
Middle to late Miocene growth of the North Pamir8
Interplay of tectonics and magmatism during post‐rift inversion on the central West Iberian Margin (Estremadura Spur)8
Flexural‐isostatic reconstruction of the Western Mediterranean during the Messinian Salinity Crisis: Implications for water level and basin connectivity8
A late Permian–Triassic trench‐slope basin in the Central Qiangtang metamorphic belt, Northern Tibet: Stratigraphy, sedimentology, syndepositional deformation and tectonic implications8
Sedimentology and provenance of newly identified Upper Cretaceous trench basin strata, Dênggar, southern Tibet: Implications for development of the Eurasian margin prior to India–Asia collision8
Correlating deformation events onshore and offshore in superimposed rift basins: The Lossiemouth Fault Zone, Inner Moray Firth Basin, Scotland8
Mass transport deposits in reflection seismic data offshore Oregon, USA8
Supradetachment basins in necking domains of rifted margins: Insights from the Norwegian Sea8
The Hidden Giant: How a rift pulse triggered a cascade of sector collapses and voluminous secondary mass‐transport events in the early evolution of Santorini8
Multiple drivers and controls of pockmark formation across the Canterbury Margin, New Zealand8
Piercement mechanisms for mobile shales7
What controls salt‐detached contraction in the translational domain of the outer Kwanza Basin, offshore Angola?7
Growth and linkage of normal faults experiencing multiple non‐coaxial extension: A case from the Qikou Sag, Bohai Bay Basin, East China7
Detrital apatite geochemistry and thermochronology from the Oligocene/Miocene Alpine foreland record the early exhumation of the Tauern Window7
Biostratigraphy and provenance analysis of the Cretaceous to Palaeogene deposits in southern Tibet: Implications for the India‐Asia collision7
Evolution of syn‐ to early post‐rift facies in rift basins: insights from the Cretaceous–Paleocene of the Great South Basin, New Zealand7
Architecture of the evaporite accumulation and salt structures dynamics in Tiddlybanken Basin, southeastern Norwegian Barents Sea7
Ordovician tectonic transition from passive margin into peripheral foreland in the southern Ordos: A diagnostic insight into the closure of Erlangping Ocean between the North Qinling Arc and North Chi7
Tectonic evolution of the Triassic Songpan‐Ganzi basin as constrained by a synthesis of multi‐proxy provenance data7
Tectonic control on mass‐transport deposit and canyon‐fed fan system in the Ulleung Basin, East Sea (Sea of Japan)7
Middle Albian provenance, sediment dispersal and foreland basin dynamics in southwestern Montana, North American Cordillera7
The influence of multiple salt layers on rift‐basin development; The Slyne and Erris basins, offshore NW Ireland7
Landscape responses to intraplate deformation in the Kalahari constrained by sediment provenance and chronology in the Okavango Basin7
Basement highs: Definitions, characterisation and origins7
Tectono‐stratigraphic evolution of the rift and post‐rift systems in the Northern Campos Basin, offshore Brazil7
Tectonic evolution and subsidence history of the Cretaceous basins in southern Egypt: The Komombo Basin7
Provenance of Neogene sandstones in western Taiwan traced with garnet geochemistry and zircon geochronology7
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