Geology

Papers
(The median citation count of Geology is 4. 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 2021-08-01 to 2025-08-01.)
ArticleCitations
ERRATUM: Across-strike asymmetry of the Andes orogen linked to the age and geometry of the Nazca plate120
Geoelectric evidence for a wide spatial footprint of active extension in central Colorado75
Determining the age and origin of a Tertiary karstic system by in situ U-Pb geochronology on speleothems61
Did transit through the galactic spiral arms seed crust production on the early Earth?57
Two-pronged kill mechanism at the end-Triassic mass extinction47
A new model for the growth of normal faults developed above pre-existing structures: COMMENT46
To rush into the secret house of death: The fate of a Tournaisian plant45
Clues on the Australasian impact crater site inferred from detailed mineralogical study of a monazite inclusion in a Muong Nong tektite: COMMENT43
Cenozoic sediment bypass versus Laramide exhumation and erosion of the Eagle Ford Group: Perspective from modelling of organic and inorganic proxy data (Maverick Basin, Texas, USA)42
Hydrological fluctuations in the Tarim Basin, northwest China, over the past millennium41
Volcanic origin of the mercury anomalies at the Cretaceous-Paleogene transition of Bidart, France40
The mechanical genesis of “fairy circle” depressions37
Identifying crystal accumulation and melt extraction during formation of high-silica granite37
ERRATUM: Inception of ridge-ridge-ridge triple junctions: Morphostructural analysis and dynamics in the early back-arc extension of the northern Okinawa Trough37
Forced Cenozoic continental subduction of Tarim craton-like lithosphere below the Tianshan revealed by ambient noise tomography37
Tracing black shales in the source of a porphyry Mo deposit using molybdenum isotopes36
Origin of Archean Pb isotope variability through open-system Paleoarchean crustal anatexis35
Extreme erosion by submarine slides35
Paleoclimates inform on a weakening and amplitude-reduced East Asian winter monsoon in the warming future34
Generation of Archean TTGs via sluggish subduction34
Contemporary and future dust sources and emission fluxes from gypsum- and quartz-dominated eolian systems, New Mexico and Texas, USA32
An invasion model for the start of Paleo-Pacific subduction31
Seafloor spreading and the delivery of sulfur and metals to Earth’s oceans31
Crustal architectural controls on critical metal ore systems in South China based on Hf isotopic mapping31
Morphologic signatures of autogenic waterfalls: A case study in the San Gabriel Mountains, California30
Crystal plasticity enhances trace element mobility in garnet30
Hot atmospheric formation of carbonate accretionary lapilli at the Cretaceous-Paleogene boundary, Brazos River, Texas, from clumped isotope thermometry30
Erratum30
Past eruptions of a newly discovered active, shallow, silicic submarine volcano near Tokyo Bay, Japan30
Orbital control of Pleistocene euxinia in Lake Magadi, Kenya29
Unusually fracture-free seafloor in the southern North Atlantic between Newfoundland and Iberia explained through compounding tectonic inheritance since the Paleoproterozoic29
Xenoliths reveal a hot Moho and thin lithosphere at the Cordillera-craton boundary of western Canada29
Magma mingling and ascent in the minutes to hours before an explosive eruption as recorded by banded pumice29
Oxygen isotope evidence for progressively assimilating trans-crustal magma plumbing systems in Iceland29
Curved orogenic belts, back-arc basins, and obduction as consequences of collision at irregular continental margins28
Three-dimensional glacial isostatic adjustment modeling reconciles conflicting geographic trends in North American marine isotope stage 5a relative sea level observations27
The Neoproterozoic glacial broom27
Disconformity-controlled hydrothermal dolomitization and cementation during basin evolution: Upper Triassic carbonates, UAE27
In situ carbon storage potential in a buried volcano27
Nd isotopic evidence for enhanced mafic weathering leading to Ordovician cooling27
Limited sulfur degassing and muted environmental impact of Ontong Java Plateau lavas27
North America's Midcontinent Rift magma volume: A coincidental rendezvous of a plume with a rift27
Opening of the North Atlantic Ocean and the rise of Scandinavian mountains26
Unraveling the histories of Proterozoic shales through in situ Rb-Sr dating and trace element laser ablation analysis26
Orogen-scale inverted metamorphism during Cretaceous–Paleogene terminal suturing along the North American Cordillera, Alaska, USA26
Contribution of the oldest Paleoproterozoic marine sulfate evaporites to Bushveld Complex Lower Zone mineralization26
Shearing-enhanced deep fluid circulation induces seismic anisotropy in the lower crust at slow-spreading oceanic ridges25
Post-salt carbonates control salt-tectonic minibasin formation25
Lateral variation in slab window viscosity inferred from global navigation satellite system (GNSS)–observed uplift due to recent mass loss at Patagonia ice fields25
A water transport system across the mantle transition zone beneath western North America as imaged by electrical conductivity data25
Fluid environment controls along-strike variation in slip style: Midcrustal geological signatures from the Red River fault, China25
Near-constant retreat rate of a terrestrial margin of the Laurentide Ice Sheet during the last deglaciation25
Molybdenum isotope signature of microbial nitrogen utilization in siboglinid tubeworms25
Mid-Proterozoic geomagnetic field was more consistent with a dipole than a quadrupole24
Silicification of trilobites and biofilm from the Cambrian Weeks Formation, Utah: Evidence for microbial mediation of silicification24
Accumulation of windblown sand in impact craters on Mars24
Spatio-temporal evolution of the Christiana-Santorini-Kolumbo volcanic field, Aegean Sea23
Clues on the Australasian impact crater site inferred from detailed mineralogical study of a monazite inclusion in a Muong Nong tektite: REPLY23
Dehydration of subducted slab gabbro in Lau Basin and its implications23
Mercury efficiently volatilized but not completely removed from sediments around igneous intrusions23
Preferential preservation of low-elevation biotas in the nonmarine fossil record23
Olivine in komatiite records origin and travel from the deep upper mantle23
Reconciling plate motion and faulting at a rift-rift-rift triple junction23
What controlled the thickness of continental crust in the Archean?23
Apatite Lu–Hf dating of late Archean banded iron formations22
Eoarchean apatite uncovers felsic foundations of the Pilbara Craton22
First dating of an early Chibanian (Middle Pleistocene) glacial overdeepening in the Alpine Foreland using the 4He/U-Th method22
Crustal fluids cause strong Lu-Hf fractionation and Hf-Nd-Li isotopic provinciality in the mantle of continental subduction zones22
Eruption dynamics leading to a volcanic thunderstorm—The January 2020 eruption of Taal volcano, Philippines22
Disparate crustal thicknesses beneath oceanic transform faults and adjacent fracture zones revealed by gravity anomalies22
Direct constraints on in situ stress state from deep drilling into the Nankai subduction zone, Japan21
Raman thermometry and (U-Th)/He thermochronometry reveal Neogene transpressional exhumation in the Nacimiento block of central California, USA21
Ultrahigh-temperature granites and a curious thermal eye in the post-collisional South Bohemian batholith of the Variscan orogenic belt (Europe)21
Small impact cratering processes produce distinctive charcoal assemblages21
Apparent preservation of primary foraminiferal Mg/Ca ratios and Mg-banding in recrystallized foraminifera21
Early Earth zircons formed in residual granitic melts produced by tonalite differentiation: REPLY21
Comment: Late Triassic continental eclogite in the central Tibetan Plateau reveals 2500-km-long Paleo-Tethys continental subduction21
A sea of change: Tracing parasitic dynamics through the past millennia in the northern Adriatic, Italy21
Hydrodynamic invalidation of synformal traps for dissolved CO221
A tropically hot mid-Cretaceous North American Western Interior Seaway21
Groundwater seepage is a key driver of theater-headed valley formation in limestone21
Early Au-rich sulfide liquid saturation explains the low Au endowment of continental intraplate alkaline magmas21
Three-dimensional electrical resistivity structure reveals the cascade rupture process of the 1988 Lancang-Gengma earthquake doublet21
Bacterial magnetofossil evidence for enhanced Pacific Ocean respired carbon storage during buildup of Antarctic glaciation20
Trends and rhythms in carbonatites and kimberlites reflect thermo-tectonic evolution of Earth20
Zn-, Mg- and O-isotope evidence for the origin of mantle eclogites from Roberts Victor kimberlite (Kaapvaal Craton, South Africa)20
A translithospheric magmatic system revealed beneath Changbaishan volcano20
Anchoring the Swedish Time Scale to the radiocarbon time scale—An absolute age for De Geer’s zero varve20
Sediment routing in an incised valley during Hurricane Harvey (2017) in Houston, Texas, USA: Implications for modern sedimentation20
Upper Paleozoic komatiites near Mashhad, NE Iran20
Traces of major collisional events in the asteroid belt in late Eocene marine sediments in Italy20
Transient fault creep on the Xidatan (Tibet) fault driven by viscoelastic relaxation following the 2001 Kokoxili earthquake20
Fossil Java Sea corals record Laurentide ice sheet disappearance19
Climatic regulation of atmospheric mercury deposition: Evidence from mercury isotopes in an alpine peat core19
Hadean zircon formed due to hydrated ultramafic protocrust melting19
ERRATUM: New estimates of the magnitude of the sea-level jump during the 8.2 ka event19
The funnel-shaped crustal architecture in central Tibet and its insights into the progression of lithospheric removal19
Formation of low-gradient bedrock chutes by dry rockfall on planetary surfaces19
Early Earth zircons formed in residual granitic melts produced by tonalite differentiation19
Crustal transpressional fault geometry influenced by viscous lower crustal flow19
Inclination and heterogeneity of layered geological sequences influence dike-induced ground deformation19
Garnet versus amphibole: Implications for magmatic differentiation and slab melting19
Reconstructing source-to-sink systems from detrital zircon core and rim ages19
Exploring the impact of deglaciation on fault slip in the Sangre de Cristo Mountains, Colorado, USA19
Intact stalked crinoids from the late Aptian of NE Spain offer insights into the Mesozoic Marine Revolution in the Tethys19
Hikurangi megathrust slip behavior influenced by lateral variability in sediment subduction19
Generation of Archean TTGs via sluggish subductions: COMMENT18
Metamorphism obscures primary taphonomic pathways in the early Cambrian Sirius Passet Lagerstätte, North Greenland18
Physical transport of magmatic sulfides promotes copper enrichment in hydrothermal ore fluids18
Evidence for nonlocal sediment transport on hillslopes from fault scarp morphology18
Ridgeward flow of compositionally heterogeneous mantle produces near-ridge seamount chains in the South Pacific18
Strength of the winter North Atlantic jet stream has deviated from its natural trend under anthropogenic warming18
Fault permeability from stochastic modeling of clay smears18
Alkali-carbonate melts in the cratonic mantle evidenced by a wehrlite xenolith from the Majuagaa kimberlite, West Greenland17
Mantle serpentinization and associated hydrogen flux at North Atlantic magma-poor rifted margins17
Effects on global warming by microbial methanogenesis in alkaline lakes during the Late Paleozoic Ice Age (LPIA)17
Mantle wedge olivine modifies slab-derived fluids: Implications for fluid transport from slab to arc magma source17
Slab window–related magmatism as a probe for pyroxenite heterogeneities in the upper mantle17
Don’t mind the “charcoal gap”: A reassessment of Devonian wildfire17
Extensional mountain building along convergent plate boundary: Insights from the active Taiwan mountain belt17
Distinctive source and hydration state of gold-ore–forming arc magmas17
Resolving pressure differences within the Grand Canyon Precambrian basement: Implications for Proterozoic tectonics17
Rhabdophane Th-Pb ages indicate reactivation of Mesoarchean structures in west Pilbara Craton during breakup of Greater India and Australia-Antarctica17
Quantitative relationships between river and channel-belt planform patterns17
Correlating mantle cooling with tectonic transitions on early Earth17
Whole-lithosphere shear during oblique rifting17
Oceanic isostasy as a trigger for the rift-to-drift transition16
Impact of stream power gradients on storage of sediment and carbon on channel margins and floodplains16
Phanerozoic variation in dolomite abundance linked to oceanic anoxia: COMMENT16
Extreme twin densities in calcite—A shock indicator16
Ultraslow cooling of an ultrahot orogen16
Guttulatic calcite: A carbonate microtexture that reveals frigid formation conditions16
Moho carbonation at an ocean-continent transition16
Increase in magma supply to Sakurajima volcano’s (Japan) shallow magma chamber over the past 500 years16
Hydrothermal sulfate surges promote rare earth element transport and mineralization16
Exceptional age constraint on a fossiliferous sedimentary succession preceding the Cretaceous Thermal Maximum16
Origin of the Sierras Pampeanas, Argentina: Flat-slab subduction and inherited structures16
A new exceptionally preserved fauna from a lowest Silurian black shale: Insights into the recovery of deep-water ecosystems after the Late Ordovician mass extinction15
Early Pleistocene climate-induced erosion of the Alaska Range formed the Nenana Gravel15
Solid as a rock: Tectonic control of graben extension and dike propagation15
Calcitic shells in the aragonite sea of the earliest Cambrian15
Halogen ratios in crustal fluids through time—Proxies for the emergence of aerobic life?15
Early accretion and prolonged carbonation of the Pacific Ocean's oldest crust15
Slab damage and the pulsating retreat of the Ionian-Apennines subduction15
Evolution of a microfracture network induced by hydrocarbon generation during experimental maturation of organic-rich lacustrine shale15
Timing of carbon uptake by oceanic crust determined by rock reactivity14
Magma recharge patterns control eruption styles and magnitudes at Popocatépetl volcano (Mexico)14
Post-subduction porphyry Cu magmas in the Sanjiang region of southwestern China formed by fractionation of lithospheric mantle–derived mafic magmas14
Frictional and microstructural evidence for a weak Wasatch fault zone14
Cryophilic polychaetes at the subtropical Laurentian margin of the Iapetus Ocean: Evidence for cold-water ocean circulation and upwelling14
Evaluating preservation bias in the continental growth record against the monazite archive14
Intensified bottom water formation in the southwest Pacific during the early Eocene greenhouse—Insights from neodymium isotopes14
Intersection between tectonic faults and magmatic systems promotes swarms with large-magnitude earthquakes around the Tengchong volcanic field, southeastern Tibetan Plateau14
Oligocene melting of subducted mélange and its mantle dynamics in northeast Asia14
Fluid-fluxed melting of juvenile lower crust traced by molybdenum isotopes14
Climate control on the relationship between erosion rate and fluvial topography14
Role of volatiles in intrusion emplacement and sulfide deposition in the supergiant Norilsk-Talnakh Ni-Cu-PGE ore deposits14
Molybdenum isotopes in mafic igneous rocks record slabmantle interactions from subarc to postarc depths14
Stagnation and tearing of the subducting northwest Pacific slab14
The role of surface processes in basin inversion and breakup unconformity14
Significance of U-Pb detrital zircon geochronology for mudstone provenance14
Silicification of trilobites and biofilm from the Cambrian Weeks Formation, Utah: Evidence for microbial mediation of silicification: REPLY13
Phanerozoic emergence of global continental collision and onset of massive crustal eclogitization13
Toroidal flow around the Tonga slab moved the Samoan plume during the Pliocene13
Identifying and characterizing missing source orogens for syn-orogenic basins based on detrital accessory mineral U-Pb geochronology and trace element geochemistry13
Boninitic blueschists record subduction initiation and subsequent accretion of an arc–forearc in the northeast Proto-Tethys Ocean13
Modern ocean island basalt–like 182W signature in Paleoarchean mafic rocks: Implications for the generation, preservation, and destruction of early mantle heterogeneities13
Detrital glass in a Bering Sea sediment core yields a ca. 160 ka Marine Isotope Stage 6 age for Old Crow tephra13
Spontaneous reheating of crystallizing lava13
Ash deposits link Oceanic Anoxic Event 2 to High Arctic volcanism13
Polychromatic polarization: Boosting the capabilities of the good old petrographic microscope13
Tracking cycles of Phanerozoic opening and closing of ocean basins using detrital rutile and zircon geochronology and geochemistry13
Rupture direction of paleoearthquakes on the Alpine Fault, New Zealand, as recorded by curved slickenlines13
Phanerozoic variation in dolomite abundance linked to oceanic anoxia: COMMENT13
Protracted mantle heat conduction after lithospheric foundering beneath the Malagasy orogen13
Sponge-rich sediment recycling in a Paleozoic continental arc driven by mélange melting13
Carbon cycling during the India-Asia collision revealed by δ26Mg–δ66Zn–δ98Mo evidence from ultrapotassic volcanoes in NW Tibet12
Constraints of boron and oxygen stable isotopes on dehydration fluids, sediment-derived melts, and crustal assimilation of the Toba volcanic system (Indonesia)12
Landscapes on the edge: River intermittency in a warming world12
Recognizing big mantle wedges in deep time: Constraints from the Western Mongolia Collage in Central Asia12
Widespread glasses generated by cometary fireballs during the late Pleistocene in the Atacama Desert, Chile: COMMENT12
Calcite U-Pb ages constrain petroleum migration pathways in tectonic complex basins12
A multidisciplinary approach to reconstructing the history of early animal life on Earth12
Tesserae: Surface differences across Venus’s “continents”12
Active faulting controls bedform development on a deep-water fan12
Laser-ablation Lu-Hf dating reveals Laurentian garnet in subducted rocks from southern Australia12
The reconstruction of coastal carbonate sequence stratigraphy: A modern-systems approach12
Coesite discovered in Australasian microtektites12
The source of tungsten-associated magmas in the northern Canadian Cordillera and implications for the basement12
Extreme isotopic heterogeneity in impact melt rocks: Implications for Martian meteorites12
“Excess Ar” by laboratory alteration of biotite12
Hydrologically driven modulation of cutoff regime in meandering rivers12
Natural levees increase in prevalence in the backwater zone: Coastal Trinity River, Texas, USA: COMMENT12
Can deepwater bottom currents generate clinothems? An example of a large, asymmetric mounded drift in Upper Jurassic to Lower Cretaceous sediments from northwestern Australia12
Eruptive tempo of Emeishan large igneous province, southwestern China and northern Vietnam: Relations to biotic crises and paleoclimate changes around the Guadalupian-Lopingian boundary12
Sediment waves control origins of submarine canyons12
Widespread glasses generated by cometary fireballs during the late Pleistocene in the Atacama Desert, Chile: REPLY12
Hyper-enrichment of gold via quartz fracturing and growth of polymetallic melt droplets11
A unique record of prokaryote cell pyritization11
Plow versus Ice Age: Erosion rate variability from glacial–interglacial climate change is an order of magnitude lower than agricultural erosion in the Upper Mississippi River Valley, USA11
Large negative δ238U anomalies in endogenic-type travertine systems11
Nanoscale mineralogical evidence confirms Cu transport as chloride complexes in brines in the Central European Kupferschiefer district11
Post-subduction porphyry Cu magmas in the Sanjiang region of southwestern China formed by fractionation of lithospheric mantle–derived mafic magmas: REPLY11
A power-based abrasion law for use in landscape evolution models11
Tracking the spatial extent of redox variability in the mid-Proterozoic ocean11
Preserved intercratonic lithosphere reveals Proterozoic assembly of Australia11
Strongly peraluminous granites provide independent evidence for an increase in biomass burial across the Precambrian–Phanerozoic boundary11
Life in the Cambrian shallows: Exceptionally preserved arthropod and mollusk microfossils from the early Cambrian of Sweden11
Crustal thickness of the Grenville orogen: A Mesoproterozoic Tibet?11
Latitudinal diversity gradient dynamics during Carboniferous to Triassic icehouse and greenhouse climates11
South Tarim tied to north India on the periphery of Rodinia and Gondwana and implications for the evolution of two supercontinents11
No evidence for a volcanic trigger for late Cambrian carbon-cycle perturbations11
High-precision U-Pb geochronology for the Miocene Climate Optimum and a novel approach for calibrating age models in deep-sea sediment cores11
Formation of lower arc crust by magmatic underplating revealed by high-precision geochronology11
Downward continued ocean bottom seismometer data show continued hydrothermal evolution of mature oceanic upper crust11
Mid-Proterozoic geomagnetic field was more consistent with a dipole than a quadrupole: COMMENT11
Fjord network in Namibia: A snapshot into the dynamics of the late Paleozoic glaciation10
Lithospheric-scale dynamics during continental subduction: Evidence from a frozen-in plate interface10
Decrypting the polymetamorphic record of the Himalaya10
Tracking ancient unconformity development with martite (U-Th)/He thermochronometry10
Lithosphere–asthenosphere interactions beneath northeast China and the origin of its intraplate volcanism10
Ocean oxygenation and ecological restructuring caused by the late Paleozoic evolution of land plants10
The early opening of the Equatorial Atlantic gateway and the evolution of Cretaceous peak warming10
Late Miocene to recent tectonic evolution of the Macquarie Triple Junction10
Nannofossil imprints across the Paleocene–Eocene thermal maximum10
Stable tungsten isotopic composition of seawater over the past 80 million years10
Laramide bulldozing of lithosphere beneath the Arizona transition zone, southwestern United States10
Steady decline in mean annual air temperatures in the first 30 k.y. after the Cretaceous-Paleogene boundary10
Rare earth element transport and mineralization linked to fluids from carbonatite systems10
Are Holocene coseismic marine terrace sequences complete paleoseismic records? Rapid erosion of a new marine terrace created during the 2016 Mw 7.8 Kaikōura earthquake suggests not!10
Dating submarine landslides using the transient response of gas hydrate stability10
Portable optically stimulated luminescence age map of a paleoseismic exposure10
A window into development of a complex ice-marginal lake prior to the Late Glacial Maximum (LGM) in Austria10
Seismic evidence for lithospheric boudinage and its implications for continental rifting10
Marine redox and nutrient dynamics linked to the Cambrian radiation of animals10
Shale mobility: From salt-like shale flow to fluid mobilization in gravity-driven deformation, the late Albian–Turonian White Pointer Delta (Ceduna Subbasin, Great Bight, Australia)10
Surface exposure constraints on the mantle water budget10
Linking metamorphism and plate boundaries over the past 2 billion years10
Formation and reorganization time scales of aeolian landscapes9
Trench-parallel mid-ocean ridge subduction driven by along-strike transmission of slab pull9
Biotite as a recorder of an exsolved Li-rich volatile phase in upper-crustal silicic magma reservoirs9
Late Oligocene–Miocene evolution of deep-water circulation in the abyssal South China Sea: Insights from Nd isotopes of fossil fish teeth9
Bedrock rivers are steep but not narrow: Hydrological and lithological controls on river geometry across the USA9
Controls on topography and erosion of the north-central Andes9
A chlorine isotope transect across Sudbury Basin (Canada) impact deposits reveals systematic isotope fractionation9
Constraining the Baltic Sea sediment chronology using tephrochronology9
Orbitally paced global oceanic deoxygenation decoupled from volcanic CO2 emission during the middle Cretaceous Oceanic Anoxic Event 1b (Aptian-Albian transition)9
Formation of rare-element pegmatites in the Chinese Altai: Contribution of two-stage melting9
The role of flat slab subduction, ridge subduction, and tectonic inheritance in Andean deformation9
When did the North Anatolian fault reach southern Marmara, Turkey?9
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