Journal of Structural Geology

Papers
(The median citation count of Journal of Structural Geology is 3. 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
Present-day in-situ stresses in Southern Gulf of Suez, Egypt: Insights for stress rotation in an extensional rift basin57
Characterization of in-situ stresses and its implications for production and reservoir stability in the depleted El Morgan hydrocarbon field, Gulf of Suez rift basin, Egypt44
Damage zone heterogeneity on seismogenic faults in crystalline rock; a field study of the Borrego Fault, Baja California37
Characteristic of stress evolution on fault surface and coal bursts mechanism during the extraction of longwall face in Yima mining area, China35
Architecture and evolution of an extensionally-inverted thrust (Mt. Tancia Thrust, Central Apennines): Geological, structural, geochemical, and K–Ar geochronological constraints35
Tectonic evolution of the intra-uplift Vigodi-Gugriana-Khirasra-Netra Fault System in the seismically active Kachchh rift basin, India: Implications for the western continental margin of the Indian pl34
Evolution of the South-Iberian paleomargin: From hyperextension to continental subduction34
The fold-thrust belt stress cycle: Superposition of normal, strike-slip, and thrust faulting deformation regimes34
Rift propagation in rotational versus orthogonal extension: Insights from 4D analogue models31
Fault damage zones width: Implications for the tectonic evolution of the northern border of the Araripe Basin, Brazil, NE Brazil30
Rift segment interaction in orthogonal and rotational extension experiments: Implications for the large-scale development of rift systems29
Transpressional structuring of the High Atlas belt, Morocco29
Damage zone characterization combining scan-line and scan-area analysis on a km-scale Digital Outcrop Model: The Qala Fault (Gozo)27
Influence of preexisting salt diapirs during thrust wedge evolution and secondary welding: Insights from analog modeling27
Timescales of faulting through calcite geochronology: A review26
Structural inheritance and border fault reactivation during active early-stage rifting along the Thyolo fault, Malawi26
Structural and kinematic evolution of strike-slip shear zones around and in the Central Tianshan: Insights for eastward tectonic wedging in the southwest Central Asian Orogenic Belt25
Research on dynamic compressive behaviors of marble under high strain rates with split Hopkinson pressure bar25
Hydraulic characterization of a fault zone from fracture distribution25
Multiple orogenic gold mineralization events in a collisional orogen: Insights from an extruded terrane along the southeastern margin of the Tibetan Plateau24
Flow pathways in multiple-direction fold hinges: Implications for fractured and karstified carbonate reservoirs24
The role of structural reactivation for gold mineralization in northeastern Hunan Province, South China24
Scale-dependent fracture networks24
Effect of contact surface area on frictional behaviour of dry and saturated rock joints23
Multi-scale fracture network characterisation on carbonate platforms23
The Patos-Pernambuco shear system of NE Brazil: Partitioned intracontinental transcurrent deformation revealed by enhanced aeromagnetic data22
The ephemeral development of C′ shear bands: A numerical modelling approach21
Timing of Arabia-Eurasia collision: Constraints from restoration of crustal-scale cross-sections21
Transformation weakening: Diffusion creep in eclogites as a result of interaction of mineral reactions and deformation21
Research on the progressive failure process and fracture mechanism of rocks with the structural evolution perspective21
The 3D structure of a normal fault from multiple outcrop observations21
Structural evolution of the Cruzeiro do Nordeste shear zone (NE Brazil): Brasiliano-Pan-African- ductile-to-brittle transition and Cretaceous brittle reactivation20
Morphotectonic and earthquake data analysis of interactional faults in Sabzevaran Area, SE Iran20
The Mountain Front Flexure in the Lurestan region of the Zagros belt: Crustal architecture and role of structural inheritances20
Structural evolution of the eastern segment of the Irtysh Shear Zone: Implications for the collision between the East Junggar Terrane and the Chinese Altai Orogen (northwestern China)20
Fault-controlled upwelling of low-T hydrothermal fluids tracked by travertines in a fold-and-thrust belt, Monte Alpi, southern apennines, Italy20
Structural evolution of southern Sichuan Basin (South China) and its control effects on tectonic fracture distribution in Longmaxi shale20
Folding and fracturing of rocks adjacent to salt diapirs20
Structural characterization of naturally fractured geothermal reservoirs in the central Upper Rhine Graben19
Reconstruction of the stress regime in the Jiaolai Basin, East Asian margin, as decoded from fault-slip analysis19
Are slump folds reliable indicators of downslope flow in recent mass transport deposits?19
Applicability of powder-based 3D printing technology in shear behavior analysis of rock mass containing non-persistent joints19
The role of structural inheritance in the development of high-displacement crustal faults in the necking domain of rifted margins: The Klakk Fault Complex, Frøya High, offshore mid-Norway19
Growth of a thrust fault array in space and time: An example from the deep-water Niger delta18
Hydraulic fracturing in transversely isotropic tight sandstone reservoirs: A numerical study based on bonded-particle model approach18
New insights on the geometry and kinematics of the Shunbei 5 strike-slip fault in the central Tarim Basin, China18
Dissolution precipitation creep as a process for the strain localisation in mafic rocks18
Structural styles and evolution of a thin-skinned fold-and-thrust belt with multiple detachments in the eastern Sichuan Basin, South China18
Recognising surface versus sub-surface deformation of soft-sediments: Consequences and considerations for palaeoseismic studies18
A study on the optimal conditions for formation of complex fracture networks in fractured reservoirs18
Shale fault zone structure and stress dependent anisotropic permeability and seismic velocity properties (Opalinus Clay, Switzerland)17
Dating recurrent shear zone activity and the transition from ductile to brittle deformation: White mica geochronology applied to the Neoproterozoic Dom Feliciano Belt in South Brazil17
Estimating effective permeability using connectivity and branch length distribution of fracture network17
Transpressive strain partitioning between the Major Gercino Shear Zone and the Tijucas Fold Belt, Dom Feliciano Belt, Santa Catarina, southern Brazil17
Numerical simulation of hydraulic fracturing process in a naturally fractured reservoir based on a discrete fracture network model16
Deformation mechanics in inclined, brittle-ductile transpression zones: Insights from 3D finite element modelling16
Seismic expression of shear zones: Insights from 2-D point-spread-function based convolution modelling16
Semi-brittle deformation of antigorite serpentinite under forearc mantle wedge conditions16
Connectivity and network development of carbonate-hosted fault damage zones from western Malta16
Distinguishing coeval patterns of contraction and collapse around flow lobes in mass transport deposits16
Displacement-dependent microstructural and petrophysical properties of deformation bands and gouges in poorly lithified sandstone deformed at shallow burial depth (Crotone Basin, Italy)16
Linked detachment folds, thrust faults, and salt diapirs: Observations and analog models15
Mineral precipitation as a mechanism of fault core growth15
Hematite fault rock thermochronometry and textures inform fault zone processes15
Structural geometry and evolution of an intracratonic strike-slip fault zone: A case study from the north SB5 fault zone in the Tarim Basin, China15
Fault zone structures and strain localization in clinoptilolite-tuff (Nižný Hrabovec, Slovak Republic)15
Vertical stress history and paleoburial in foreland basins unravelled by stylolite roughness paleopiezometry: Insights from bedding-parallel stylolites in the Bighorn Basin, Wyoming, USA.15
Unveiling ductile deformation during fast exhumation of a granitic pluton in a transfer zone15
Deformation styles related to intraplate strike-slip fault systems of the Saharan-Tunisian Southern Atlas (North Africa): New kinematic models15
Constraints upon fault zone properties by combined structural analysis of virtual outcrop models and discrete fracture network modelling15
From outcrop scanlines to discrete fracture networks, an integrative workflow15
Fracture density variations within a reservoir-scale normal fault zone: A case study from shallow-water carbonates of southern Italy15
Subvertical, linear and progressive deformation related to gold mineralization at the Galat Sufar South deposit, Nubian Shield, NE Sudan15
Natural fault and fracture network characterization for the southern Ekofisk field: A case study integrating seismic attribute analysis with image log interpretation14
Normal fault networks and their spatial relationships in Plio-Quaternary sedimentary series: A case study in the Zanjan Depression, NW Iran14
Structural development at the leading edge of the salt-bearing Kuqa fold-and-thrust belt, southern Tian Shan, NW China14
Sensitivity analysis of segmentation techniques and voxel resolution on rock physical properties by X-ray imaging14
Fracture propagation and coalescence at bedding plane in layered rocks14
Present-day structural frame of the Santander Massif and Pamplona Wedge: The interaction of the Northern Andes14
Distributed normal faulting in the tip zone of the South Alkyonides Fault System, Gulf of Corinth, constrained using 36Cl exposure dating of late-Quaternary wave-cut platforms14
Mechanical insights into the development of fracture corridors in layered rocks14
Growth of cataclastic bands into a fault zone: A multiscalar process by microcrack coalescence in sandstones of Rio do Peixe Basin, NE Brazil14
Which average, how many grains, and how to estimate robust confidence intervals in unimodal grain size populations14
An alternative model for the role of salt depositional configuration and preexisting salt structures in the evolution of the Southern Pyrenees, Spain14
Investigating thrust-fault growth and segment linkage using displacement distribution analysis in the active Duzhanzi thrust fault zone, Northern Tian Shan of China13
Late evolution of the inner Northern Apennines from the structure of the Monti del Chianti-Monte Cetona ridge (Tuscany, Italy)13
Ongoing shortening in the Dinarides fold-and-thrust belt: A new structural model of the 1979 (Mw 7.1) Montenegro earthquake epicentral region13
Active fault segmentation in Northern Tunisia13
How petrophysical properties influence the seismic signature of carbonate fault damage zone: Insights from forward-seismic modelling13
Role of multiple inherited basement structures on orogen geometry and evolution: Insights from analogue modelling13
The role of deformation-reaction interactions to localize strain in polymineralic rocks: Insights from experimentally deformed plagioclase-pyroxene assemblages13
Structurally controlled development of a sulfuric hypogene karst system in a fold-and-thrust belt (Majella Massif, Italy)12
Detachment fold duplexes within gravity-driven fold and thrust systems12
The Jal Az-Zor escarpment as a product of complex duplex folding and strike-slip tectonics; A new study in Kuwait, northeastern Arabian Peninsula12
The use of immersive virtual reality for teaching fieldwork skills in complex structural terrains12
Outcrop-scale fracture analysis and seismic modelling of a basin-bounding normal fault in platform carbonates, central Italy12
Shear zone evolution during core complex exhumation – Implications for continental detachments12
How wide is a fault damage zone? Using network topology to examine how fault-damage zones overprint regional fracture networks12
Multiscale spatial analysis of fracture arrangement and pattern reconstruction using Ripley's K-function12
Deformation fabrics and strain localization mechanisms in graphitic carbon-bearing rocks from the Ailaoshan-Red River strike-slip fault zone12
Paleostress and statistical analysis using quartz veins from mineralized and non-mineralized zones: Application for exploration targeting12
Deformation and temperature variation along thrust-sense shear zones in the hinterland-foreland transition zone of collisional settings: A case study from the Barbagia Thrust (Sardinia, Italy)12
Structural style and kinematic analysis of folding in the southern Dezful Embayment oilfields, SW Iran12
Sinistral strike-slip shearing along the Jiali shear zone around the Eastern Himalaya syntaxis region: Evidences for oligocene eastward limited translation of Tibet12
Spatial variation of nearly NS-trending normal faulting in the southern Yadong-Gulu rift, Tibet: New constraints from the Chongba Yumtso fault, Duoqing Co graben12
Deformation bands and their impact on fluid flow: Insights from geometrical modelling and multi-scale flow simulations in sandstones11
Contractional salt-tectonic system in the south Dezful embayment, Zagros11
A continuum meshfree method for sandbox-style numerical modeling of accretionary and doubly vergent wedges11
The effect of hydrous mineral content on competitive strain localization mechanisms in felsic granulites11
Large-scale natural fracture network patterns: Insights from automated mapping in the Lilstock (Bristol Channel) limestone outcrops11
Crustal growth in the Mesoarchean plutonic belt from the Memve'ele area (Ntem Complex-southwestern Cameroon): Evidence of “early earth” transpressional tectonics11
Influence of two-phase extension on the fault network and its impact on hydrocarbon migration in the Linnan sag, Bohai Bay Basin, East China11
Fabric and anisotropy of slates: From classical studies to new results11
Forward kinematic modeling of fault-bend folding11
Deformation history of the Puna plateau, Central Andes of northwestern Argentina11
Unravelling the development of regional-scale shear zones by a multidisciplinary approach: The case study of the Ferriere-Mollières Shear Zone (Argentera Massif, Western Alps)11
Calcite pseudomorphs after aragonite: A tool to unravel the structural history of high-pressure marbles (Evia Island, Greece)10
Influence of water on deformation and failure of gypsum rock10
Late Cenozoic river system reorganization and its origin within the Qilian Shan, NE Tibet10
Shear localisation, strain partitioning and frictional melting in a debris avalanche generated by volcanic flank collapse10
Active tectonics and kinematics of Fethiye-Göcek Bay, SW Turkey: Insight about the eastern edge of Pliny-Strabo Trenches10
Analysis of spatial arrangement of fractures in two dimensions using point process statistics10
Tracking progressive deformation of an orogenic wedge through two successive internal thrusts: Insights from structure, deformation profile, strain, and vorticity of the Main Central thrust (MCT) and 10
Fracture networks in shale-hosted igneous intrusions: Processes, distribution and implications for igneous petroleum systems10
Amorphous material in experimentally deformed mafic rock and its temperature dependence: Implications for fault rheology during aseismic creep and seismic rupture10
Stability of basement-rooted faults in the Delaware Basin of Texas and New Mexico, USA10
Segmentation and increasing activity in the Neogene-Quaternary Teruel Basin rift (Spain) revealed by morphotectonic approach10
Constraining the ductile deformation mechanisms of garnet across pressure-temperature space10
X-ray computed micro-tomography of spiral garnets: A new test of how they form10
Lithological and structural control on fracture frequency distribution within a carbonate-hosted relay ramp10
Structural analysis of sulfate vein networks in Gale crater (Mars)10
Geomechanical models for the quantitatively prediction of multi-scale fracture distribution in carbonate reservoirs10
3D-thrust fault pattern control on negative inversion: An analogue modelling perspective on central Italy10
Structural style of the NW Zagros Mountains and the role of basement thrusting for its Mountain Front Flexure, Kurdistan Region of Iraq10
Fractal and multifractal characterization of stochastic fracture networks and real outcrops10
Timing and distribution of bedding-parallel veins, in evaporitic rocks, Bouhedma Formation, Northern Chotts, Tunisia10
Analogue modelling of strain partitioning along a curved strike-slip fault system during backarc-convex orocline formation: Implications for the Cerna-Timok fault system of the Carpatho-Balkanides10
Stress, microstructure, and deformation mechanisms during subduction underplating at the depth of tremor and slow slip, Franciscan Complex, northern California9
One line on the map: A review of the geological history of the Semail Thrust, Oman-UAE mountains9
The role of trapped fluids during the development and deformation of a carbonate/shale intra-wedge tectonic mélange (Mt. Massico, Southern Apennines, Italy)9
The joint sets on the Lilstock Benches, UK. Observations based on mapping a full resolution UAV-based image9
Fault-induced mechanical anisotropy and its effects on fracture patterns in crystalline rocks9
Spatio-temporal structural evolution of the Kohat fold and thrust belt of Pakistan9
The effects of quartz Dauphiné twinning on strain localization in a mid-crustal shear zone9
Single-event throws along the Delta Fault (Baikal rift) reconstructed from ground penetrating radar, geological and geomorphological data9
Fluid assisted rejuvenation of precursor brittle fractures as the habitats of ductile shear zones: An example from the ~2.6 Ga Bundelkhand Granitoid of north-central India9
Quantitative prediction of multiperiod fracture distributions in the Cambrian-Ordovician buried hill within the Futai Oilfield, Jiyang Depression, East China9
Lateral subhorizontal middle to lower crustal flow in response to continental collision: Evidence from the Diancang Shan complex along the Ailao Shan-Red River belt, Southeastern Tibetan Plateau9
Tectonic transformation from orogen-perpendicular to orogen-parallel extension in the North Himalayan Gneiss Domes: Evidence from a structural, kinematic, and geochronological investigation of the Ram9
Discrete fracture network (DFN) modelling of a high-level radioactive waste repository host rock and the effects on its hydrogeological behaviour9
Intracrystalline vorticity record of flow kinematics during shear zone reactivation9
Structural control on fluid circulation in a graben system: Constraints from the Saint Pierre Bois quarry (Vosges, France)9
Shear strain and volume change associated with sigmoidal vein arrays in the Boda Claystone9
Frictional strength and fluidization of water-saturated kaolinite gouges at seismic slip velocities9
Geomorphology of contractional salt tectonics along the Kuqa fold-thrust belt, northwestern China: Testing pre-kinematic diapir versus source-fed thrust and detachment fold models9
Paleostress analysis of the Yeşilyurt-Elazığ Fault Zone and its importance for the tectonic evolution, East Turkey9
Multistage strain localisation and fluid-assisted cataclasis in carbonate rocks during the seismic cycle: Insights from the Belluno Thrust (eastern Southern Alps, Italy)9
Mechanical stratigraphy influences deformation band pattern in arkosic sandstones, Rio do Peixe Basin, Brazil9
3D fault-zone architecture across the brittle–plastic transition along the Median Tectonic Line, SW Japan: Fault-rock characterization9
Potential formation mechanisms of early diagenetic displacive veins in the Permian Boda Claystone Formation9
Active faulting and seismic hazard in the Outer Western Carpathians (Polish Galicia): Evidence from fractured Quaternary gravels8
Structural evolution and exhumation of the Yulong dome: Constraints on middle crustal flow in southeastern Tibetan Plateau in response to the India-Eurasia collision8
Salt tectonics in salt-bearing rift basins: Progradational loading vs extension8
Throw-rate variations within linkage zones during the growth of normal faults: Case studies from the Western Volcanic Zone, Iceland8
Sheath fold development around deformable inclusions: Integration of field-analysis (Cima Lunga unit, Central Alps) and 3D numerical models8
Using migrating growth strata to confirm a ∼230-km-long detachment thrust in the southern Tarim Basin8
Discrete fracture network model of the vapor zone leakages at the Copahue geothermal field8
Polyphase deformation in the Badu complex: Insights into Triassic intraplate orogeny in South China8
Geometry of folded and boudinaged pegmatite veins emplaced within a strike-slip shear zone: A case study from the Caledonian orogen, northern Scotland8
Microstructures of epidote-prehnite bearing damaged granitoids (northern Victoria Land, Antarctica): clues for the interaction between faulting and hydrothermal fluids8
Chemical interaction driven by deep fluids in the damage zone of a seismogenic carbonate fault8
Power-law relationship between joint spacing and bed thickness in sedimentary rocks and implications for layered rock mechanics8
Mechanical properties and recrystallization of quartz in presence of H2O: Combination of cracking, subgrain rotation and dissolution-precipitation processes8
Unraveling the emplacement history of a Portuguese post-tectonic Variscan pluton using magnetic fabrics and gravimetry8
The evolution of slate microfabrics during progressive accretion of foreland basin sediments8
Bed thickness-dependent fracturing and inter-bed coupling define the nonlinear fracture spacing-bed thickness relationship in layered rocks: Numerical modeling8
Deformation history of the Qianlishan Complex, Khondalite Belt, North China: Structures, ages and tectonic implications8
Refraction of micro-fractures due to shear-induced mechanical stratigraphy in a low-grade meta-sedimentary rock8
Secondary minibasins in orogens: Examples from the Sivas Basin (Turkey) and the sub-Alpine fold-and-thrust belt (France)8
3D digital outcrop modelling of the Lower Cretaceous Los Santos formation sandstones, Mesa de Los Santos region (Colombia): Implications for structural analysis7
Effect of pressure on the deformation of quartz aggregates in the presence of H2O7
Influence of paleo-uplift on structural deformation of salt-bearing fold-and-thrust belt: Insights from physical modeling7
Detailed structural analysis of digital outcrops: A learning example from the Kermanshah-Qulqula radiolarite basin, Zagros Belt, Iran7
Monazite as a monitor of shear strain in orogenic crust7
The critical control of arkosic sandstone porosity on deformation band formation: Insights from the Shulu across-fault borehole in the Bohai Bay Basin, China7
Grain size and grain size distribution of a lithified fault core in carbonates rocks using multi-scale image analysis: The example of the San Benedetto-Gioia dei Marsi fault (Central Italy)7
Paleostress field reconstruction in the western Dharwar craton, south India: Evidence from brittle faults and associated structures of younger granites7
Experimental fracture sealing in reservoir sandstones and its relation to rock texture7
Orthogonal microscopy image acquisition analysis technique for rock sections in polarizer angle domain7
Potential of a virtual reality environment based on very-high-resolution satellite imagery for structural geology measurements of lava flows7
3D digital outcrop model-based analysis of fracture network along the seismogenic Mt. Vettore Fault System (Central Italy): the importance of inherited fractures7
Seismological data versus rheological modelling: Comparisons across the Aegean Region for improving the seismic hazard assessment7
Morphology and topology of dolostone lithons in the regional Carboneras Fault Zone, Southern Spain7
Self-similar length-displacement scaling achieved by scale-dependent growth processes: Evidence from the Atacama Fault System7
Structural and metamorphic inheritance controls strain partitioning during orogenic shortening (Kalak Nappe Complex, Norwegian Caledonides)7
Topological analysis of fracture networks integrated with flow simulation models for equivalent fracture permeability estimation7
Rheological evolution of a pseudotachylyte-bearing deep crustal shear zone in the western Canadian shield7
Complete deformation history of the transition zone between oblique and orthogonal collision belts of the SE Tibetan Plateau: Crustal shortening and rotation caused by the indentation of India into Eu7
Influence of ramp geometry and orientation on fault propagation folding: Insights from the 3D finite element method7
Feldspar and orthopyroxene piezometers constrained using quartz–feldspar and olivine–orthopyroxene mineral pairs from natural mylonites7
Composition and deformation patterns of the caprock on salt extrusions in southern Iran – Field study on the Karmostaj and Siah Taq diapirs7
Anticline growth by shortening during crustal exhumation of the Moroccan Atlantic margin7
Reply to comment on “how to build an extensional basin in a contractional setting? Numerical and physical modeling applied to the Mejerda basin at the front of the eastern Tell of Tunisia”7
Variation in structural styles within fold-and-thrust belts: Insights from field mapping, cross-sections balancing, and 2D-kinematic modelling in the Jura mountains (Eastern France)7
The characteristics of natural open fractures in acoustic borehole image logs from the pre-salt Barra Velha formation, Santos Basin, Brazil7
Deformation and structural evolution of mantle peridotites during exhumation on transform faults: A forced transition from ductile to brittle regime7
A new subsampling methodology to optimize the characterization of two-dimensional bedrock fracture networks7
Influence of décollement friction on anisotropy of magnetic susceptibility in a fold-and-thrust belt model6
Evolution of fracture networks and connectivity during fault–bend folding: Insights from the Sinon Anticline in the southwestern Hongseong–Imjingang Belt, Korea6
A non-active fault within an active restraining bend: The case of the Hasbaya fault, Lebanon6
Deformation mechanisms of granulite-facies mafic shear zones from hole U1473A, Atlantis Bank, Southwest Indian Ridge (IODP Expedition 360)6
Sequence of deformation at the front of an orogen: Lublin basin case study (Poland)6
Building tectonic framework of a blind active fault zone using field and ground-penetrating radar data6
Inversion of polyphase calcite-twin data for deviatoric stress tensors: 2. Application to the Huangling Dome, northern South China6
Evolution of stretching lineations in granulite-hosted ductile shear zones, Eastern Ghats Province, India: Role of temperature, strain rate and pre-existing stretching lineations6
Selective clast survival in an experimentally-produced pseudotachylyte6
Sampling interval-size effects and differential sensitivities of different morphology parameters of rock joint6
Geometry and topology of tectonolineaments in the Gorce Mts. (Outer Carpathians) in Poland6
Characterizing syn-convergent extension along the Neybaz-Chatak detachment shear zone, Central Iran: Insights from microstructures, quartz petrofabrics and flow vorticity analysis6
Analysis of fault bend folding kinematic models and comparison with an analog experiment6
On the petrology and microstructures of small-scale ductile shear zones in granitoid rocks: An overview6
Detachment folding, growth mechanism and seismic potential in the Jammu Sub-Himalaya6
Secondary detachments within carbonates of the Saraburi Group, Triassic Khao Khwang fold and Thrust Belt, Thailand6
The role of antithetic faults in transferring displacement across contractional relay zones on normal faults6
Complex shape of the Palaeoproterozoic Serpovidny refolded mega-sheath fold in northern Fennoscandia revealed by magnetic and structural data6
Rheological behaviour of mafic dykes deformed in a granite host, Wanna, Eyre Peninsula, South Australia6
Shear zone fabrics and their significance in curved, inverted basin-derived thrust systems6
Magnetic fabric of the early-Ediacaran Itapetim monzogranitic pluton: magma flow during oblique extension along strike-slip shear zones (Eastern Brazil)6
Quartz fluid inclusion abundance and off-fault damage in a deeply exhumed, strike-slip, seismogenic fault6
The effect of muscovite on the microstructural evolution and rheology of quartzite in general shear6
West Spitsbergen fold and thrust belt: A digital educational data package for teaching structural geology6
The role of kink boundaries in the deformation and recrystallisation of polycrystalline ice6
Topological analysis of fault network in naturally fractured reservoirs: A case study from the pre-salt section of the Santos Basin, Brazil6
Formation of multi-stage and clustered fractures at 3.6–4.9 km in the Shizigou structure, SW Qaidam basin6
Y-B-P-R or S-C-C′? Suggestion for the nomenclature of experimental brittle fault fabric in phyllosilicate-granular mixtures6
The influence of preexisting host rock damage on fault network localization6
Structural and petrological characteristics of a Jurassic detachment fault from the Mont-Blanc massif (Col du Bonhomme area, France)6
Scaling analysis, correlation length and compaction estimates of natural and simulated stylolites6
Strain and vorticity analyses using rotated porphyroclasts in the Tanbour metamorphic rocks: Evidence of transpressional deformation along the Sanandaj-Sirjan metamorphic belt, SW Iran6
Development and passive exhumation of high-pressure shear zones (Blueschist Unit, Syros): Insights from quartz and columnar calcite microstructures6
A revised orientation-based correction method for SfM-MVS point clouds of outcrops using ground control planes with marks6
Spatial variations of ductile strain in fold-and-thrust belts: From model to nature6
Evolution of shear bands and cracks in multi-stage triaxial tests with water-saturated sandstone: A study of micro-tectonics with a fractal perspective6
Upper lithospheric transfer zones driving the non-cylindricity of the West-Pyrenean orogenic prism (Mauléon hyperextended basin)5
Compiling regional structures in geological databases: The giant quartz veins of the Pyrenees as a case study5
Deformation, crustal melting and magmatism in the crustal-scale East-Variscan Shear Zone (Aiguilles-Rouges and Mont-Blanc massifs, Western Alps)5
Role of fluid in strain softening within the Main Central thrust in Sikkim: The origin of quartz-rich mylonites5
Accommodation structures during kink band evolution; quantitative methods applied to Late Variscan deformation of Portugal5
Along-rift propagation of Pleistocene-Holocene faults from a central volcano5
Offset components and fault-block motion during the 2016 central Italy earthquake (Mw 6.6, Monte Vettore fault system)5
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