Journal of Structural Geology

Papers
(The median citation count of Journal of Structural Geology is 2. 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 2020-11-01 to 2024-11-01.)
ArticleCitations
Present-day in-situ stresses in Southern Gulf of Suez, Egypt: Insights for stress rotation in an extensional rift basin64
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, Egypt50
Timescales of faulting through calcite geochronology: A review43
The fold-thrust belt stress cycle: Superposition of normal, strike-slip, and thrust faulting deformation regimes38
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 pl37
Rift segment interaction in orthogonal and rotational extension experiments: Implications for the large-scale development of rift systems33
Damage zone characterization combining scan-line and scan-area analysis on a km-scale Digital Outcrop Model: The Qala Fault (Gozo)30
Multiple orogenic gold mineralization events in a collisional orogen: Insights from an extruded terrane along the southeastern margin of the Tibetan Plateau29
The role of structural reactivation for gold mineralization in northeastern Hunan Province, South China28
Flow pathways in multiple-direction fold hinges: Implications for fractured and karstified carbonate reservoirs28
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 Belt27
Scale-dependent fracture networks27
Influence of preexisting salt diapirs during thrust wedge evolution and secondary welding: Insights from analog modeling27
The Patos-Pernambuco shear system of NE Brazil: Partitioned intracontinental transcurrent deformation revealed by enhanced aeromagnetic data26
Applicability of powder-based 3D printing technology in shear behavior analysis of rock mass containing non-persistent joints26
Research on the progressive failure process and fracture mechanism of rocks with the structural evolution perspective25
Multi-scale fracture network characterisation on carbonate platforms25
New insights on the geometry and kinematics of the Shunbei 5 strike-slip fault in the central Tarim Basin, China24
Fracture networks in shale-hosted igneous intrusions: Processes, distribution and implications for igneous petroleum systems23
Structural characterization of naturally fractured geothermal reservoirs in the central Upper Rhine Graben22
Folding and fracturing of rocks adjacent to salt diapirs22
Structural evolution of southern Sichuan Basin (South China) and its control effects on tectonic fracture distribution in Longmaxi shale22
Structural evolution of the Cruzeiro do Nordeste shear zone (NE Brazil): Brasiliano-Pan-African- ductile-to-brittle transition and Cretaceous brittle reactivation22
Fault-controlled upwelling of low-T hydrothermal fluids tracked by travertines in a fold-and-thrust belt, Monte Alpi, southern apennines, Italy22
Structural styles and evolution of a thin-skinned fold-and-thrust belt with multiple detachments in the eastern Sichuan Basin, South China21
Numerical simulation of hydraulic fracturing process in a naturally fractured reservoir based on a discrete fracture network model21
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-Norway21
Recognising surface versus sub-surface deformation of soft-sediments: Consequences and considerations for palaeoseismic studies21
Dissolution precipitation creep as a process for the strain localisation in mafic rocks20
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 Brazil20
Reconstruction of the stress regime in the Jiaolai Basin, East Asian margin, as decoded from fault-slip analysis20
Fracture propagation and coalescence at bedding plane in layered rocks20
Constraints upon fault zone properties by combined structural analysis of virtual outcrop models and discrete fracture network modelling20
Shale fault zone structure and stress dependent anisotropic permeability and seismic velocity properties (Opalinus Clay, Switzerland)20
Connectivity and network development of carbonate-hosted fault damage zones from western Malta19
Estimating effective permeability using connectivity and branch length distribution of fracture network19
Mineral precipitation as a mechanism of fault core growth18
Linked detachment folds, thrust faults, and salt diapirs: Observations and analog models18
The use of immersive virtual reality for teaching fieldwork skills in complex structural terrains18
Semi-brittle deformation of antigorite serpentinite under forearc mantle wedge conditions18
Structural geometry and evolution of an intracratonic strike-slip fault zone: A case study from the north SB5 fault zone in the Tarim Basin, China17
Natural fault and fracture network characterization for the southern Ekofisk field: A case study integrating seismic attribute analysis with image log interpretation17
How petrophysical properties influence the seismic signature of carbonate fault damage zone: Insights from forward-seismic modelling17
Growth of cataclastic bands into a fault zone: A multiscalar process by microcrack coalescence in sandstones of Rio do Peixe Basin, NE Brazil17
An alternative model for the role of salt depositional configuration and preexisting salt structures in the evolution of the Southern Pyrenees, Spain17
Mechanical insights into the development of fracture corridors in layered rocks17
Shear zone evolution during core complex exhumation – Implications for continental detachments17
Detachment fold duplexes within gravity-driven fold and thrust systems16
Unveiling ductile deformation during fast exhumation of a granitic pluton in a transfer zone16
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)16
Fracture density variations within a reservoir-scale normal fault zone: A case study from shallow-water carbonates of southern Italy16
Seismic expression of shear zones: Insights from 2-D point-spread-function based convolution modelling16
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-Balkanides15
Large-scale natural fracture network patterns: Insights from automated mapping in the Lilstock (Bristol Channel) limestone outcrops15
Structural development at the leading edge of the salt-bearing Kuqa fold-and-thrust belt, southern Tian Shan, NW China15
Influence of water on deformation and failure of gypsum rock15
Late evolution of the inner Northern Apennines from the structure of the Monti del Chianti-Monte Cetona ridge (Tuscany, Italy)15
Ongoing shortening in the Dinarides fold-and-thrust belt: A new structural model of the 1979 (Mw 7.1) Montenegro earthquake epicentral region15
Spatial variation of nearly NS-trending normal faulting in the southern Yadong-Gulu rift, Tibet: New constraints from the Chongba Yumtso fault, Duoqing Co graben15
How wide is a fault damage zone? Using network topology to examine how fault-damage zones overprint regional fracture networks15
Deformation styles related to intraplate strike-slip fault systems of the Saharan-Tunisian Southern Atlas (North Africa): New kinematic models15
Differential deformation of a strike-slip fault in the Paleozoic carbonate reservoirs of the Tarim Basin, China14
Power-law relationship between joint spacing and bed thickness in sedimentary rocks and implications for layered rock mechanics14
Outcrop-scale fracture analysis and seismic modelling of a basin-bounding normal fault in platform carbonates, central Italy14
Role of multiple inherited basement structures on orogen geometry and evolution: Insights from analogue modelling14
Influence of two-phase extension on the fault network and its impact on hydrocarbon migration in the Linnan sag, Bohai Bay Basin, East China14
One line on the map: A review of the geological history of the Semail Thrust, Oman-UAE mountains14
Structurally controlled development of a sulfuric hypogene karst system in a fold-and-thrust belt (Majella Massif, Italy)14
Multiscale spatial analysis of fracture arrangement and pattern reconstruction using Ripley's K-function14
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 Ram13
Characteristics and controlling factors of natural fractures in deep lacustrine shale oil reservoirs of the Permian Fengcheng Formation in the Mahu Sag, Junggar Basin, China13
Calcite pseudomorphs after aragonite: A tool to unravel the structural history of high-pressure marbles (Evia Island, Greece)13
Contractional salt-tectonic system in the south Dezful embayment, Zagros13
A continuum meshfree method for sandbox-style numerical modeling of accretionary and doubly vergent wedges13
Natural fractures in ultra-deep reservoirs of China: A review13
Sheath fold development around deformable inclusions: Integration of field-analysis (Cima Lunga unit, Central Alps) and 3D numerical models13
Structural style of the NW Zagros Mountains and the role of basement thrusting for its Mountain Front Flexure, Kurdistan Region of Iraq13
Deformation bands and their impact on fluid flow: Insights from geometrical modelling and multi-scale flow simulations in sandstones13
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)13
Sampling interval-size effects and differential sensitivities of different morphology parameters of rock joint12
Geomorphology of contractional salt tectonics along the Kuqa fold-thrust belt, northwestern China: Testing pre-kinematic diapir versus source-fed thrust and detachment fold models12
Using migrating growth strata to confirm a ∼230-km-long detachment thrust in the southern Tarim Basin12
Mechanical stratigraphy influences deformation band pattern in arkosic sandstones, Rio do Peixe Basin, Brazil12
Deformation fabrics and strain localization mechanisms in graphitic carbon-bearing rocks from the Ailaoshan-Red River strike-slip fault zone12
Deformation history of the Puna plateau, Central Andes of northwestern Argentina12
Y-B-P-R or S-C-C′? Suggestion for the nomenclature of experimental brittle fault fabric in phyllosilicate-granular mixtures12
Intracrystalline vorticity record of flow kinematics during shear zone reactivation12
Forward kinematic modeling of fault-bend folding12
3D digital outcrop model-based analysis of fracture network along the seismogenic Mt. Vettore Fault System (Central Italy): the importance of inherited fractures12
3D-thrust fault pattern control on negative inversion: An analogue modelling perspective on central Italy12
Mechanical properties and recrystallization of quartz in presence of H2O: Combination of cracking, subgrain rotation and dissolution-precipitation processes12
Stability of basement-rooted faults in the Delaware Basin of Texas and New Mexico, USA11
Geometry of folded and boudinaged pegmatite veins emplaced within a strike-slip shear zone: A case study from the Caledonian orogen, northern Scotland11
Quantitative prediction of multiperiod fracture distributions in the Cambrian-Ordovician buried hill within the Futai Oilfield, Jiyang Depression, East China11
Crustal growth in the Mesoarchean plutonic belt from the Memve'ele area (Ntem Complex-southwestern Cameroon): Evidence of “early earth” transpressional tectonics11
Fault systems in the offshore sector of the Campi Flegrei caldera (southern Italy): Implications for nested caldera structure, resurgent dome, and volcano-tectonic evolution11
Analysis of spatial arrangement of fractures in two dimensions using point process statistics11
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 11
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 India11
Shear localisation, strain partitioning and frictional melting in a debris avalanche generated by volcanic flank collapse11
Active tectonics and kinematics of Fethiye-Göcek Bay, SW Turkey: Insight about the eastern edge of Pliny-Strabo Trenches11
Timing and distribution of bedding-parallel veins, in evaporitic rocks, Bouhedma Formation, Northern Chotts, Tunisia11
Stress, microstructure, and deformation mechanisms during subduction underplating at the depth of tremor and slow slip, Franciscan Complex, northern California11
Frictional strength and fluidization of water-saturated kaolinite gouges at seismic slip velocities11
3D digital outcrop modelling of the Lower Cretaceous Los Santos formation sandstones, Mesa de Los Santos region (Colombia): Implications for structural analysis10
The joint sets on the Lilstock Benches, UK. Observations based on mapping a full resolution UAV-based image10
Influence of paleo-uplift on structural deformation of salt-bearing fold-and-thrust belt: Insights from physical modeling10
Unraveling the emplacement history of a Portuguese post-tectonic Variscan pluton using magnetic fabrics and gravimetry10
Building tectonic framework of a blind active fault zone using field and ground-penetrating radar data10
Constraining the ductile deformation mechanisms of garnet across pressure-temperature space10
Bed thickness-dependent fracturing and inter-bed coupling define the nonlinear fracture spacing-bed thickness relationship in layered rocks: Numerical modeling10
Multistage strain localisation and fluid-assisted cataclasis in carbonate rocks during the seismic cycle: Insights from the Belluno Thrust (eastern Southern Alps, Italy)10
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 Plateau10
Discrete fracture network (DFN) modelling of a high-level radioactive waste repository host rock and the effects on its hydrogeological behaviour10
Single-event throws along the Delta Fault (Baikal rift) reconstructed from ground penetrating radar, geological and geomorphological data10
Microstructures of epidote-prehnite bearing damaged granitoids (northern Victoria Land, Antarctica): clues for the interaction between faulting and hydrothermal fluids10
On the petrology and microstructures of small-scale ductile shear zones in granitoid rocks: An overview10
Deformation history of the Qianlishan Complex, Khondalite Belt, North China: Structures, ages and tectonic implications10
Secondary minibasins in orogens: Examples from the Sivas Basin (Turkey) and the sub-Alpine fold-and-thrust belt (France)10
Structural control on fluid circulation in a graben system: Constraints from the Saint Pierre Bois quarry (Vosges, France)10
Fractal and multifractal characterization of stochastic fracture networks and real outcrops10
Spatio-temporal structural evolution of the Kohat fold and thrust belt of Pakistan9
3D fault-zone architecture across the brittle–plastic transition along the Median Tectonic Line, SW Japan: Fault-rock characterization9
Polyphase deformation in the Badu complex: Insights into Triassic intraplate orogeny in South China9
Validity of the stress inversion of orientation data from a dike swarm with a radial-parallel pattern transition9
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 Eu9
Chemical interaction driven by deep fluids in the damage zone of a seismogenic carbonate fault9
Formation of multi-stage and clustered fractures at 3.6–4.9 km in the Shizigou structure, SW Qaidam basin9
Discrete fracture network model of the vapor zone leakages at the Copahue geothermal field9
Deformation, crustal melting and magmatism in the crustal-scale East-Variscan Shear Zone (Aiguilles-Rouges and Mont-Blanc massifs, Western Alps)9
The evolution of slate microfabrics during progressive accretion of foreland basin sediments9
Experimental fracture sealing in reservoir sandstones and its relation to rock texture9
Dry, damp, or drenched? The effect of water saturation on the frictional properties of clay fault gouges9
Effect of pressure on the deformation of quartz aggregates in the presence of H2O9
Fault-induced mechanical anisotropy and its effects on fracture patterns in crystalline rocks9
Composition and deformation patterns of the caprock on salt extrusions in southern Iran – Field study on the Karmostaj and Siah Taq diapirs9
The critical control of arkosic sandstone porosity on deformation band formation: Insights from the Shulu across-fault borehole in the Bohai Bay Basin, China9
Topological analysis of fracture networks integrated with flow simulation models for equivalent fracture permeability estimation9
The effect of muscovite on the microstructural evolution and rheology of quartzite in general shear9
Potential of a virtual reality environment based on very-high-resolution satellite imagery for structural geology measurements of lava flows9
The brittle evolution of Western Norway – A space-time model based on fault mineralizations, K–Ar fault gouge dating and paleostress analysis9
Structural styles and linkage evolution in the middle segment of a strike-slip fault: A case from the Tarim Basin, NW China9
A new subsampling methodology to optimize the characterization of two-dimensional bedrock fracture networks8
Salt tectonics in salt-bearing rift basins: Progradational loading vs extension8
Timing and duration of meteoric water infiltration in the Quiberon detachment zone (Armorican Massif, Variscan belt, France)8
Monazite as a monitor of shear strain in orogenic crust8
Structural and petrological characteristics of a Jurassic detachment fault from the Mont-Blanc massif (Col du Bonhomme area, France)8
Active faulting and seismic hazard in the Outer Western Carpathians (Polish Galicia): Evidence from fractured Quaternary gravels8
Development and passive exhumation of high-pressure shear zones (Blueschist Unit, Syros): Insights from quartz and columnar calcite microstructures8
Influence of ramp geometry and orientation on fault propagation folding: Insights from the 3D finite element method8
Feldspar and orthopyroxene piezometers constrained using quartz–feldspar and olivine–orthopyroxene mineral pairs from natural mylonites8
Detachment folding, growth mechanism and seismic potential in the Jammu Sub-Himalaya8
The effect of fault-induced compaction on petrophysical properties of deformation bands in poorly lithified sandstones8
Factors influencing fault-propagation folding in the Kuqa Depression: Insights from geomechanical models8
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)8
Geometry and topology of tectonolineaments in the Gorce Mts. (Outer Carpathians) in Poland8
Deep and ultra-deep basin brittle deformation with focus on China8
Mesozoic strike-slip fault system at the margin of the Junggar Basin, NW China8
Seismological data versus rheological modelling: Comparisons across the Aegean Region for improving the seismic hazard assessment8
Upper lithospheric transfer zones driving the non-cylindricity of the West-Pyrenean orogenic prism (Mauléon hyperextended basin)8
Rigorizing the use of the coefficient of variation to diagnose fracture periodicity and clustering8
Accommodation structures during kink band evolution; quantitative methods applied to Late Variscan deformation of Portugal8
Orthogonal microscopy image acquisition analysis technique for rock sections in polarizer angle domain7
Salt diapir downbuilding: Fast analytical models based on rates of salt supply and sedimentation7
West Spitsbergen fold and thrust belt: A digital educational data package for teaching structural geology7
The influence of preexisting host rock damage on fault network localization7
Detailed structural analysis of digital outcrops: A learning example from the Kermanshah-Qulqula radiolarite basin, Zagros Belt, Iran7
Strain and vorticity analyses using rotated porphyroclasts in the Tanbour metamorphic rocks: Evidence of transpressional deformation along the Sanandaj-Sirjan metamorphic belt, SW Iran7
The characteristics of natural open fractures in acoustic borehole image logs from the pre-salt Barra Velha formation, Santos Basin, Brazil7
Rheological evolution of a pseudotachylyte-bearing deep crustal shear zone in the western Canadian shield7
Topological analysis of fault network in naturally fractured reservoirs: A case study from the pre-salt section of the Santos Basin, Brazil7
Transpression in the Sanandaj-Sirjan Zone (Zagros Orogen, Iran) during the Jurassic and Early Cretaceous: Evidence from the North Shahrekord Shear Zone7
Small-scale size effects on the shearing behavior and sliding stiffness reduction-displacement curves of rock-plastic gouge simulant under low normal stresses7
Anticline growth by shortening during crustal exhumation of the Moroccan Atlantic margin7
A revised orientation-based correction method for SfM-MVS point clouds of outcrops using ground control planes with marks7
Structural restoration of an Eo-Mesoarchean (3.8–2.9 Ga) terrane, Eastern China, dissected by the Tanlu fault zone7
Reservoir quality evaluation and prediction in ultra-deep tight sandstones in the Kuqa depression, China7
Evidence of hydrothermal fluid circulation driving elemental mass redistribution in an active fault zone7
A refined approach for quantitative kinematic vorticity number estimation using microstructures7
Scaling analysis, correlation length and compaction estimates of natural and simulated stylolites7
Shear zone fabrics and their significance in curved, inverted basin-derived thrust systems7
Soft-sediment deformation structures in cave deposits and their possible causes (Kalacka Cave, Tatra Mts., Poland)6
Contractional fold amplification through bed-parallel gypsum vein (“beef”) formation6
A gravitational origin for volcano-tectonic faults in the Campi Flegrei caldera (southern Italy) inferred from detailed field observations6
Post-Oligocene evolution of Indo-Burma wedge: Insights from deformation structures of Tripura Mizoram fold belt6
Fault damage zone and its effect on deep shale gas: Insights from 3D seismic interpretation in the southern Sichuan Basin, China6
Spatial and spacing distribution of joints at (over-) saturation in the turbidite sandstones of the Marnoso-Arenacea Fm. (Northern Apennines, Italy)6
Characterizing syn-convergent extension along the Neybaz-Chatak detachment shear zone, Central Iran: Insights from microstructures, quartz petrofabrics and flow vorticity analysis6
Dynamically recrystallized grains identified via the application of Gaussian mixture model to EBSD data6
Natural fractures in deep continental shale oil reservoirs: A case study from the Permian Lucaogou formation in the Eastern Junggar Basin, Northwest China6
Compiling regional structures in geological databases: The giant quartz veins of the Pyrenees as a case study6
Analogue modeling of the role of salt in the structuration of thin-skinned pull-apart basins: The case study of El Hamma basin, Central Tunisia6
Olivine-rich veins in high-pressure serpentinites: A far-field paleo-stress snapshot during subduction6
Evolution of fracture networks and connectivity during fault–bend folding: Insights from the Sinon Anticline in the southwestern Hongseong–Imjingang Belt, Korea6
Crystal preferred orientations, deformation mechanisms and seismic properties of high pressure metamorphic rocks from the Central Qiangtang metamorphic belt, Tibetan Plateau6
Subsurface fracture characterization in a folded ultra-deep tight-gas sandstone reservoir: A case study from the Keshen gas field, Tarim Basin, China6
Secondary detachments within carbonates of the Saraburi Group, Triassic Khao Khwang fold and Thrust Belt, Thailand6
Crack path at bedding planes of cracked layered rocks6
Magnetic fabric of the early-Ediacaran Itapetim monzogranitic pluton: magma flow during oblique extension along strike-slip shear zones (Eastern Brazil)6
Rheological behaviour of mafic dykes deformed in a granite host, Wanna, Eyre Peninsula, South Australia6
Reply to Mazzarini et al. comment on ‘Unveiling ductile deformation during fast exhumation of a granitic pluton in a transfer zone’6
Ternary fault permeability diagram: An innovative way to estimate fault zones hydraulics6
Constraining kinematic and temporal evolution of a normal-sense shear zone: Insights into the Simplon Shear Zone (Western Alps)6
Crystallographically controlled void space at grain boundaries in the Harkless quartzite6
Selective clast survival in an experimentally-produced pseudotachylyte6
The use of network topology to assess connectivity of deformation bands in sandstone: A quantitative approach based on digital outcrop models6
The spatial distributions of mineralisation6
Influence of décollement friction on anisotropy of magnetic susceptibility in a fold-and-thrust belt model6
How do inherited dip-slip faults affect the development of new extensional faults? Insights from wet clay analog models6
Using virtual outcrop models and google earth to teach structural geology concepts6
A fast way to estimate the clay fabric from shale fragments. Key example from a strained thrust footwall (Pyrenees).6
Microstructures, geochemistry, and geochronology of mica fish: Review and advances6
Deformation mechanisms of granulite-facies mafic shear zones from hole U1473A, Atlantis Bank, Southwest Indian Ridge (IODP Expedition 360)6
Evolution of deformation bands, insights from structural diagenesis6
New scaling of fractures in a giant carbonate platform from outcrops and subsurface6
The role of antithetic faults in transferring displacement across contractional relay zones on normal faults6
2D modeling and simulation of deformation bands’ effect on fluid flow: Implications for hydraulic properties in siliciclastic reservoirs6
Complex shape of the Palaeoproterozoic Serpovidny refolded mega-sheath fold in northern Fennoscandia revealed by magnetic and structural data6
Coseismic slip gradient at the western terminus of the 1920 Haiyuan Mw 7.9 earthquake6
Structural analysis of layered evaporites using internal deformation patterns: Examples from Santos and Campos basins, Brazil6
Along-rift propagation of Pleistocene-Holocene faults from a central volcano6
Fracture-pattern growth in the deep, chemically reactive subsurface6
Analysis of fault bend folding kinematic models and comparison with an analog experiment6
Finding the right place in Mohr circle space: Geologic evidence and implications for applying a non-linear failure criterion to fractured rock6
The influence of back-arc extension direction on the strain partitioning associated with continental indentation: Analogue modelling and implications for the Circum-Moesian Fault System of South-Easte6
Along-strike permeability variation in carbonate-hosted fault zones6
Sequence of deformation at the front of an orogen: Lublin basin case study (Poland)6
The kinematics of a salt sheet recorded in an array of distorted intrasalt stringers (Les Avellanes Diapir – South-Central Pyrenees)5
Slip partitioning and inclined transpression in the Bazargan fold and thrust belt, Central Iran Microcontinent, Kerman area, SE Iran5
What steers the “folding to faulting” transition in carbonate-dominated seismic fold-and-thrust belts? New insights from the Eastern Southern Alps (Northern Italy)5
Structural and temporal relationships between volcanic activity, hydrothermal alteration, epithermal Ag–Pb–Zn mineralization and regional stress regime in the Quevar Volcanic Complex (Puna plateau, Sa5
Syn-kinematic inversion in an intracontinental extensional field? A structural analysis of the Waterberg Thrust, northern Namibia5
Episodic deformation and reactions in mylonitic high-grade metamorphic granulites from Dronning Maud Land, Antarctica5
Fluctuation in the fluid and tectonic pressures in the South Almora Thrust Zone (SATZ), Kumaun Lesser Himalaya; paleoseismic implications5
Role of fluid in strain softening within the Main Central thrust in Sikkim: The origin of quartz-rich mylonites5
Mechanical behaviors of intact antigorite as functions of temperature: Faulting, slow stick-slip and stable sliding5
Using the Schmidt hammer on folds: An example from the Cantabrian Zone (NW Iberian Peninsula)5
The effect of grain size and porosity on the nature of compaction localisation in high-porosity sandstone5
Fragment size distributions in brittle deformed rocks5
Crystallographic preferred orientations and microtexture of the Himalayan eclogites revealing records of syn-deformation peak metamorphic stage and subsequent exhumation5
A knowledge-data framework and geospatial fuzzy logic-based approach to model and predict structural complexity5
Criteria to discriminate between different models of thrust ramping in gravity-driven fold and thrust systems5
Are open-source aerial images useful for fracture network characterisation? Insights from a multi-scale approach in the Zagros Mts.5
Structural and rheological features of the northeastern Sanyang shear zone in the eastern Jiangnan orogen: Indications for early Paleozoic orogeny in the South China Block5
A dynamic atlas of interference patterns in superimposed, opposite sense ductile shear zones5
Enhancement of ductile deformation in polycrystalline anorthite due to the addition of water5
Open fracture clustering: Integrating subsurface and outcrop analogues, Asmari Formation, SW Iran5
Rheology of a coaxial shear zone in the Virginia Blue Ridge: Wet quartzite dislocation creep at ~250–280 °C5
Magnetic fabrics as strain markers in folded soft-sediment layers5
Buried thrust belt front of the western Central Andes of northern Chile: Style, age, and relationship with basement heterogeneities5
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