2024-10-09 |
Tracing the stepwise warming trend in the tropical Indian Ocean through a 40-year record of oxygen isotope composition in Maldives corals |
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2024-10-09 |
Heterogeneous cooling subsidence of oceanic lithosphere controlled by spreading rate |
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2024-10-08 |
Bioavailability of molybdenite to support nitrogen fixation on early Earth by an anoxygenic phototroph |
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2024-10-07 |
Dynamic evolution of competing same-dip double subduction: New perspectives of the Neo-Tethyan plate tectonics |
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2024-10-07 |
From birth to death: The role of upper-crustal thermal maturation and volcanism in porphyry ore formation revealed in the Yerington district |
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2024-10-05 |
Composition and age constraints on a Hadean enriched mantle source revealed by the Paleoarchean São Tomé layered intrusion, NE Brazil |
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2024-10-04 |
Lithium isotopes track changes in continental weathering regimes across the end-Permian mass extinction in Southwest China |
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2024-10-04 |
Magnetotelluric evidence for the formation of the layered Sask Craton by flat slab subduction |
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2024-10-04 |
Clumped isotopes constrain thermogenic and secondary microbial methane origins in coal bed methane |
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2024-10-02 |
Experimental investigation of hydrogen isotope fractionation during hydration of olivine-hosted melt inclusions: Implications for D/H in Baffin Island picrites |
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2024-10-02 |
Martian seismic anisotropy underneath Elysium Planitia revealed by direct <em>S</em> wave splitting |
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2024-10-02 |
Regional-scale, high-resolution measurements of hilltop curvature reveal tectonic, climatic, and lithologic controls on hillslope morphology |
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2024-09-30 |
A distinct type of MORB formed by two-stage melting of a hybrid mantle during Gondwana breakup |
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2024-09-30 |
Long-term isostatic relaxation of large terrestrial impact structures: structural characteristics inferred from scaled analogue experiments |
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2024-09-28 |
Potential formational scenarios of the mud volcanoes in the Zhurong landing area in Utopia Planitia, observed by Tianwen-1 |
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2024-09-28 |
Metamorphic CO<sub>2</sub> fluxes offset the net geological carbon sink in the Himalayan-Tibetan orogen |
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2024-09-28 |
Snapshots of magmatic evolution revealed by zircon depth profiling |
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2024-09-27 |
The fate of ultramafic-rich mélanges in cold to hot subduction zones: Implications for diapirism (or not) and chemical geodynamics |
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2024-09-26 |
Editorial Board |
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2024-09-25 |
Receiver function image of the mantle transition zone beneath western China: Fragmented subduction and counterflow upwelling |
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2024-09-24 |
Evidence for a missing late veneer from <sup>182</sup>W and <sup>142</sup>Nd systematics in the Archean São Francisco Craton |
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2024-09-24 |
Characterization and geodynamic interpretation of Nazca Plate bathymetric anomalies |
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2024-09-24 |
Paleomagnetic constraints on the primary iron minerals of the late Paleoproterozoic Xuanlong-type ironstone in the North China Craton |
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2024-09-22 |
Tracing island arc petrogenesis using potassium isotopes |
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2024-09-22 |
Astronomical forcing of terrestrial organic carbon burial in East Asia during the Eocene |
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2024-09-21 |
Early generation of a refractory inclusions-enriched H-chondritic parent body: A safe harbor for Ca, Al-rich inclusions |
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2024-09-21 |
Potassium isotope evidence for subducted upper and lower oceanic crust in ocean island basalt sources |
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2024-09-20 |
Climate impact on river incision on hotspot volcanoes: insights from paleotopographic reconstructions and numerical modelling |
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2024-09-20 |
Dissolved ammonia catalyzes proto-dolomite precipitation at Earth surface temperature |
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2024-09-20 |
Vertical transport of anthropogenic lead by reversible scavenging in the South Atlantic Ocean |
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2024-09-19 |
Splitting intensity tomography to image depth-dependent seismic anisotropy patterns beneath the Italian Peninsula and surrounding regions |
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2024-09-19 |
Catastrophic outburst floods along the middle Yarlung Tsangpo River: Responses to coupled fault and glacial activity on the Southern Tibetan Plateau |
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2024-09-19 |
Earth-Moon refractory element similarity constrains a thoroughly-mixed Moon-forming disk |
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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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