2024-11-11 |
Weak paleointensities from 1.6 Ga Greenland dykes: Further evidence for a billion-year period of paleomagnetic dipole low during the Paleoproterozoic |
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2024-11-09 |
Magnetotelluric image of the Patagonian slab window: Constraints on upper mantle physical properties and sources of intraplate magmatism |
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2024-11-09 |
Coupling magma ascent models with volatile diffusion chronometry |
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2024-11-08 |
Shallow crustal rupture in a major <em>M<sub>W</sub></em> 7.5 earthquake above a deep crustal seismic swarm along the Noto Peninsula in western Japan |
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2024-11-08 |
Thermal evolution of the lunar magma ocean |
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2024-11-08 |
Mantle plume – mid ocean ridge interactions revealed from hotspot melt production rate along the Walvis Ridge-Rio Grande Rise |
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2024-11-08 |
How brittle detachments form and evolve through space and time |
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2024-11-08 |
Magmatic N<sub>2</sub> degassing dominates nitrogen loss during sediment subduction and granitoid genesis |
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2024-11-08 |
Unsteady slip pulses under spatially-varying prestress |
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2024-11-07 |
Direct in situ evidence of tidal roles in the formation of contourite depositional systems |
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2024-11-07 |
Exploring frictional properties of upper plate fault reactivation in subduction zones: The Atacama Fault System in northern Chile |
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2024-11-07 |
Stable silicon isotope fractionation reflects the routing of water through a mesoscale hillslope |
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2024-11-07 |
Constraints on the continental weathering intensity through the Permian using lithium isotopes of well-preserved brachiopod shells |
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2024-11-06 |
The slow slip event cycle along the Izmit segment of the North Anatolian Fault |
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2024-11-03 |
The chlorine evolution of arc magmas and the crustal water filter |
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2024-11-03 |
Variations in antimony isotope and toxic metals across the Guadalupian-Lopingian (Permian) boundary at Penglaitan, China: Implications for the Emeishan volcanism and marine extinction |
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2024-10-31 |
The sulfur isotopic composition of Cenozoic pyrite is affected by methane content and depositional environment |
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2024-10-31 |
Interaction of Kerguelen and Amsterdam-St. Paul dual hotspots with Southeast Indian Ridge |
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2024-10-30 |
Complex basalt evolution in the Chang'e-6 landing area |
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2024-10-29 |
Earth's precession rate evolution and rapid fall during the Late Proterozoic |
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2024-10-29 |
Anorthosites produced by water-fluxed anatexis of deep arc gabbros, Gangdese batholith, Tibet |
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2024-10-29 |
Iron-sulfur-carbon redox interactions in the continental subduction factory and their effect on volatile element storage in the mantle wedge |
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2024-10-29 |
Decoding the interplay between magma thermodynamics and lithospheric thermal state as a possible explanation for the origin of the Daly Gap |
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2024-10-29 |
Characterization of bedrock mass-wasting at fault-bound abyssal hills |
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2024-10-29 |
Prediction of barchan dunes migration using climatic models and speed-up effect of dune topography on air flow |
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2024-10-28 |
Magmatic degassing dynamics at Halema'uma'u Crater, Kīlauea, Hawaii |
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2024-10-25 |
Complicated thermo-chemical heterogeneity of the mantle transition zone beneath the Philippine Sea Plate revealed by SS precursors investigation |
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2024-10-25 |
Geochemical constraints on reaction temperature and pressure and heat- and mass-transfer efficiency at Rainbow Hydrothermal Field |
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2024-10-25 |
Quantifying the loss of continental crust into the mantle from volume/mass balance calculations in modern collisional mountains |
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2024-10-24 |
The origin of tectonic mélanges from the Kodiak complex and Shimanto Belt and its implication for subduction interface processes |
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2024-10-24 |
Decoupled deformation between crust and mantle beneath Indo-Burmese Wedge: A new seismotectonic model |
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2024-10-23 |
Controls on fluid discharge at cold seep-hydrate systems: 4D seismic monitoring of Woolsey Mound, Gulf of Mexico |
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2024-10-23 |
The persisting conundrum of mantle viscosity inferred from mantle convection and glacial isostatic adjustment processes |
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2024-10-23 |
Early and elongated epochs of planetesimal dynamo generation |
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2024-10-22 |
Earth's hypsometry and what it tells us about global sea level |
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2024-10-22 |
Garnet clinopyroxenite formation via amphibole-dehydration in continental arcs: Evidence from Fe isotopes |
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2024-10-20 |
Orbital identification of widespread hydrated silica deposits in Gale crater |
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2024-10-20 |
Low total REE zircon formed in equilibrium with hornblende in granulitized eclogites: Implications for exhumation rates |
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2024-10-20 |
Editorial Board |
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2024-10-17 |
Multiple hydrothermal events at martian surface revealed by H and Cl isotope systematics of melt inclusions and hydrous minerals from chassignite NWA 2737 |
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2024-10-16 |
2D numerical experiments on a plume-fed asthenosphere: Necessary preconditions and implications for geoid and dynamic topography |
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2024-10-16 |
Tracing hydrous eclogite melts in the source of sanukitoids |
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2024-10-16 |
The viscosity of a partially molten layer in a paleo-orogenic plateau |
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2024-10-16 |
Water ice particles detected by SELENE's Spectral Profiler at lunar shadowed regions in various local times and latitudes |
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2024-10-16 |
Detection of a ULVZ in the Central Pacific using high frequency Sdiff postcursors |
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2024-10-15 |
Microseisms associated with the southwest summer monsoon recorded on the seafloor of South China Sea |
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2024-10-13 |
Lithium isotope stratigraphy and Ordovician weathering |
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2024-10-12 |
Ring faulting and piston collapse in the mantle sustained the largest submarine eruption ever documented |
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2024-10-12 |
Postseismic deformation due to the 2021 <em>M<sub>W</sub></em> 7.4 Maduo (China) earthquake and implications for regional rheology and seismic hazards around the Bayan Har block |
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2024-10-11 |
Inferring relative sediment fluxes and landscape evolution trends from C, O and clumped isotopes and mineral composition in detrital carbonate |
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2024-10-11 |
Abiotic origin of organics in the martian regolith |
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2024-10-11 |
Rhenium isotope variations in Icelandic groundwaters and hydrothermal systems |
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2024-10-11 |
Prolonged sediment aggradation in an internal Himalayan valley due to out-of-sequence lateral fault growth |
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2024-10-10 |
Correlating 300 million years of catastrophes |
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2024-10-10 |
Control of stepwise subduction and slab breakoff on volcanism and uplift in the Tibetan Plateau |
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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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