2024-09-17 |
Rubidium isotopes reveal dehydration and melting of the subducting slab beneath the Mariana arc |
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2024-09-17 |
Insights into the last 100 ky of geomagnetic field variability using numerical dynamo simulations |
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2024-09-16 |
The very late-stage crystallization of the lunar magma ocean and the composition of immiscible urKREEP |
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2024-09-16 |
Low-velocity middle-and-lower crustal materials blocked by the red river fault in the SE margin of the Tibetan plateau |
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2024-09-16 |
Rise of mantle oxidation by Neoarchean subduction in the North China Craton |
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2024-09-15 |
Eoarchean granulite-facies metamorphism in the Itsaq Gneiss Complex, southwest Greenland |
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2024-09-15 |
Seismicity zoning at Coso geothermal field and stress changes from fluid production and migration |
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2024-09-15 |
Anomalously high relief on Denali, Alaska, caused by tectonic, lithologic, and climatic drivers |
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2024-09-15 |
Metasedimentary “carbon filter” and its implication for subduction zone carbon recycling |
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2024-09-15 |
New weak fault model that does not require high pore pressure |
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2024-09-12 |
Barium isotopes constrain the triggering mechanism of the Cretaceous OAE 2 in the Neotethys Ocean |
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2024-09-12 |
Evidence suggesting that earth had a ring in the Ordovician |
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2024-09-12 |
Rheological arrest vs. rapid growth of bubbles in crystal-rich magma |
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2024-09-12 |
Kinematic vorticity of shear zones that accommodate vertical crustal advection: Implications for metamorphic core complexes and pluton emplacement |
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2024-09-10 |
Historic ocean acidification of Loch Sween revealed by correlative geochemical imaging and high-resolution boron isotope analysis of <em>Boreolithothamniom</em> cf. <em>soriferum</em> |
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2024-09-09 |
Geological investigation of the lunar Apollo basin: From surface composition to interior structure |
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2024-09-09 |
Editorial Board |
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2024-09-08 |
Eocene climate and hydrology of eastern Asia controlled by orbital forcing and Tibetan Plateau uplift |
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2024-09-08 |
Interplay and feedback between tectonic regime, faulting, sealing horizons, and fluid flow in a hydrocarbon-hosting extensional basin: The Val d'Agri Basin case, Southern Italy |
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2024-09-08 |
Silicon isotope compositions of chondritic components: Insights into early disk processes |
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2024-09-07 |
The effects of trivalent cations (Al and Fe) on the grain growth rates of bridgmanite |
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2024-09-07 |
Structure and transport properties of FeS at planetary core conditions |
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2024-09-07 |
A threshold in submarine channel curvature explains erosion rate and type |
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2024-09-05 |
Constraining the evaporative loss of zinc during impact processes using terrestrial impact glasses |
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2024-09-04 |
Hydraulically linked reservoirs simultaneously fed the 1975–1984 Krafla Fires eruptions: Insights from petrochemistry |
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2024-09-04 |
Neogene surface uplift of the Lunpola Basin in Central Tibet: Implications for uplifting and flattening of orogenic plateaus |
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2024-09-04 |
Bayesian frameworks for integrating petrologic and geochronologic data |
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2024-09-04 |
Arctic Alaska deepwater organic carbon burial and environmental changes during the late Albian–early Campanian (103–82 Ma) |
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2024-09-03 |
Evolution of rift faulting in incipient, magma-poor divergent plate boundaries: New insights from the Okavango-Makgadikgadi Rift Zone, Botswana |
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2024-09-03 |
Long-term evolution of the Sulzberger Ice Shelf, West Antarctica: Insights from 74-year observations and 2022 Hunga-Tonga volcanic tsunami-induced calving |
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2024-09-03 |
A failed search for concordancy across multiple isotopic systems in lunar impactites: Implications for testing the Late Heavy Bombardment hypothesis |
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2024-09-01 |
Thickness of Pluto's Ice Shell from elastic deformation of the Sputnik Planitia forebulge: Response to infill load or vestige of impact event? |
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2024-09-01 |
Revised timing of rapid exhumation in the West Qinling: Implications for geodynamics of Oligocene-Miocene Tibetan plateau outward expansion |
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2024-09-01 |
Footwall refrigeration versus footwall hydration: Reassessing steep thermal gradients below detachment faults with <em>in situ</em> SIMS oxygen isotope analysis |
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2024-08-31 |
Phosphorus flux during the Ediacaran: Rooted in continental weathering or pelagic upwelling? |
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2024-08-31 |
Editorial Board |
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2024-08-29 |
Partial melting of arclogite and petrogenesis of alkaline-silicate complexes |
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2024-08-29 |
New evidence from the Paleoproterozoic Gunflint Iron Formation for microbially-driven, early diagenetic precipitation of siderite |
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2024-08-29 |
Limited arc magmatism and seismicity due to extensive mantle wedge serpentinization in the Makran subduction zone |
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2024-08-29 |
The reduced alloy in Earth's upper mantle: Experimental constraints on Fe-Ni-S-C(-O) melt compositions and deep mantle oxygen fugacity (5–16 GPa) |
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2024-08-28 |
Contrasting dynamics of marine bacterial-algal communities between the two main pulses of the Late Ordovician Mass Extinction |
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2024-08-28 |
Lithospheric rheology in West Tibet and Pamir constrained from the postseismic deformation of the 2005 Mw7.6 Kashmir (Pakistan) earthquake |
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2024-08-28 |
A benthic source of isotopically heavy Ni from continental margins and implications for global ocean Ni isotope mass balance |
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2024-08-24 |
Magma solidification effects during sill emplacement: Insights from laboratory experiments |
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2024-08-23 |
The helium and carbon isotopic signature of Ocean island basalts: Insights from Fogo volcano (Cape Verde archipelago) |
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2024-08-23 |
Volcanic tempo driven by rapid fluctuations in mantle temperature during large igneous province emplacement |
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2024-08-22 |
The impact of climate on relief in the northern Japanese Alps within the past 1 Myr–The case of the Tateyama mountains |
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2024-08-22 |
Topography of the 410 and 660 km discontinuities beneath the Tibetan plateau and adjacent areas |
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2024-08-22 |
Spatiotemporal dominance of afterslip and viscoelastic relaxation revealed by four decades of post-1973 Luhuo earthquake observations |
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2024-08-22 |
Successful subduction of oceanic plate after failed attempts in the Late Archean: Petrological and geochemical constraints |
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2024-08-21 |
Changing shape of mantle heterogeneity by melt migration beneath mid-ocean ridges |
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2024-08-21 |
Deccan volcanism's influence on Chicxulub impact signatures at the continental Cretaceous-Paleogene boundary in the Sichuan Basin, China |
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2024-08-21 |
The role of deformation on the early crystallization and rheology of basaltic liquids |
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2024-08-21 |
Insights into water mass change in the Yangtze River Basin from the spectral integration of GNSS and GRACE observations |
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2024-08-21 |
Previously unrecognized, 1000 km-long Qixiang Co fault governs eastward escape of central Tibet |
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2024-08-21 |
Extremely large Cl isotopic fractionation in Chang'e-5 impact glass beads |
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2024-08-21 |
Seismotectonic segmentation controlled by magmatic underplating in the central-southern segment of Tanlu fault zone, eastern China |
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2024-08-21 |
Pulsed fluid release from subducting slabs caused by a scale-invariant dehydration process |
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2024-08-20 |
Earth's longest lava flows erupted from its largest igneous province: The submarine Ontong Java Plateau |
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2024-08-16 |
Deciphering interseismic strain accumulation and its termination on the central-eastern Altyn Tagh fault from high-resolution velocity fields |
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2024-08-15 |
Monitoring crack opening via seismic velocity variation to assess that fatal effect of precipitation for landslide motion |
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2024-08-15 |
Editorial Board |
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2024-08-14 |
Rhenium Isotope Reconnaissance of Uranium Ore Concentrates |
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2024-08-14 |
Spatial and temporal variations of seismic azimuthal anisotropy following the 2019 ridgecrest earthquake sequence in southern california |
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2024-08-11 |
Effects of layered roof for stability and exploration of lunar lava tubes |
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2024-08-10 |
Source characteristics of the 2006 Pingtung earthquake doublet off southern Taiwan and the possible contribution of submarine landslides to the Tsunami |
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2024-08-10 |
Lunar mantle composition and timing of overturn indicated by Mg# and mineralogy distributions across the South Pole-Aitken basin |
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2024-08-08 |
Tracking quartz and zircon provenance in sedimentary rocks using Ti distributions: Unlocking the volcanic-plutonic connection in old igneous systems |
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2024-08-08 |
Crustal-mantle layering deposits in the Von Kármán crater, South Pole-Aitken basin |
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2024-08-05 |
Sediment remobilization over subaqueous sand waves: In-situ observation in the northern South China Sea |
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2024-08-05 |
Bottom Ekman transport drives transverse flows to shape contourite moat and drift systems |
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2024-08-04 |
Sediment geochemistry reveals abundant off-axis hydrothermal fields on the ultraslow-spreading Southwest Indian Ridge |
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2024-07-31 |
A Bayesian age from dispersed plagioclase and zircon dates in the Los Chocoyos ash, Central America |
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2024-07-28 |
Strength of continental lithosphere governed by the time since the last orogeny |
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2024-07-28 |
L-chondrite body breakup in Ordovician strata in China - A time tie point globally and across the inner solar system |
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2024-07-27 |
Ultramafic melt viscosity: A model |
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2024-07-27 |
Exhumation of ultra-high pressure (UHP) rocks modulated by rifted margin-subduction feedback: Implications for their preservation in old collisional orogens |
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2024-07-27 |
A seawater origin for greenalite in iron formation |
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2024-07-27 |
Reversal in estuarine sand supply driven by Holocene sea level rise: A model for sand transport in large structural estuaries, San Francisco Bay, California, USA |
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2024-07-27 |
Loading-induced stress variation on active faults and seismicity modulation in the Kuril Islands-Japan region |
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2024-07-27 |
Were Neoarchean atmospheric methane hazes and early Paleoproterozoic glaciations driven by the rise of oxygen in surface environments? |
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2024-07-27 |
Role of syn-magmatic strain localization in oceanic detachment faulting at ultraslow-spreading ridges |
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2024-07-26 |
Impact of riverine sediment mineralogy on seawater Nd isotope compositions in the northeastern part of the Indian Ocean during the last two glacial cycles |
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2024-07-26 |
Unraveling the tectonic evolution of the Andean hinterland (Argentina and Chile, 30°S) using multi-sample thermal history models |
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2024-07-26 |
Editorial Board |
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2024-07-25 |
Mantle deformation in the highly oblique indo-burma subduction system inferred from shear wave splitting measurements |
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2024-07-25 |
Atypical crustal structure of the Makran subduction zone and seismotectonic implications |
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2024-07-24 |
Vanadium isotope fractionation during plutonic differentiation and implications for the isotopic composition of the upper continental crust |
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2024-07-24 |
Overlapping hotspot tracks and melts from diffuse plume materials in the upper mantle generated intraplate seamount groups in the West Pacific |
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2024-07-23 |
Subduction-driven mantle flow beneath active back-arc basins inferred from seismic anisotropy tomography |
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2024-07-23 |
Revisiting zircon Eu anomaly as a proxy for crustal thickness: A case study of the Sierra Nevada Batholith |
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2024-07-22 |
Induced seismicity and surface deformation associated with long-term and abrupt geothermal operations in Blue Mountain, Nevada |
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2024-07-21 |
Global variability of the composition and temperature at the 410-km discontinuity from receiver function analysis of dense arrays |
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2024-07-21 |
Fast, furious, and gassy: Etna's explosive eruption from the mantle |
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2024-07-21 |
Recurrent marine anoxia in the Paleo-Tethys linked to constriction of seaways during the Early Triassic |
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2024-07-20 |
Mimas: A middle-aged moon of Saturn? |
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2024-07-19 |
Diverse source materials contributed to a secular increase in δ<sup>18</sup>O for the Paleo-Mesoproterozoic A<sub>2</sub>-type granites |
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2024-07-17 |
Fault structure and earthquake clustering in Aswan region (Egypt) revealed by high-precision earthquake location from 35 years of recorded natural and induced seismicity |
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2024-07-17 |
Calcium isotope evidence of increased carbonate saturation state during the Frasnian–Famennian boundary event |
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2024-07-17 |
Impacts of an active Pacific Meridional Overturning Circulation on the Pliocene climate and hydrological cycle |
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