2024-12-03 |
Elemental-organic geochemical evidence for the lacustrine metalimnetic oxygen minimum dynamics in the Mid-Late Triassic Chang 7 shales |
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2024-12-03 |
Corrigendum to “Molybdenum isotope systematics of lavas from the East Pacific Rise: Constraints on the source of enriched mid-ocean ridge basalt” [EPSL 578, 2022/117283] |
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2024-12-01 |
Inverted metamorphic gradient in the Zanhuang nappe/thrust system, north China indicates large-scale thrust stacking in an Archean Orogen |
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2024-12-01 |
Subduction-stalled plume tail triggers Tarim large igneous province |
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2024-12-01 |
Diffusion of Sr and Ba in plagioclase: Composition and silica activity dependencies, and application to volcanic rocks |
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2024-11-30 |
Active, long-lived upper-plate splay faulting revealed by thermochronology in the Alaska subduction zone |
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2024-11-30 |
Numeric ring-reconstructions based on massifs favor a non-oblique south pole-Aitken-forming impact event |
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2024-11-30 |
Editorial Board |
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2024-11-28 |
Soft barrier to megathrust rupture enabled by serpentinized mantle wedge: The Chile subduction zone |
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2024-11-28 |
Did the terrestrial planets of the solar system form by pebble accretion? |
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2024-11-28 |
Multilevel Mechanisms Driving Intraplate Volcanism in Central Mongolia Revealed by Adjoint Waveform Tomography of Receiver Function and Ambient Noise Data |
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2024-11-24 |
Melting the Marinoan Snowball Earth: The impact of deglaciation duration on the sea-level history of continental margins |
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2024-11-24 |
First cycle or polycyclic? Combining apatite and zircon detrital U-Pb geochronology and geochemistry to assess sediment recycling and effects of weathering |
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2024-11-23 |
Ocean crustal veins record dynamic interplay between plate-cooling-induced cracking and ocean chemistry |
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2024-11-23 |
Fluid-mediated transition from dynamic rupturing to aseismic slip at the base of the seismogenic continental crust |
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2024-11-23 |
Context matters: Modeling thermochronologic data in geologic frameworks using the Great Unconformity as a case study |
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2024-11-23 |
Seismic radial anisotropy in southeastern Tibetan Plateau and its implications for regional geodynamic evolution |
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2024-11-23 |
Methane sealed due to the formation of gas hydrate system in the South China Sea |
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2024-11-22 |
Chondrites as thermal and mechanical archives of accretion processes in the Solar protoplanetary disk |
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2024-11-21 |
Poroelastic effects on rupture propagation across fault stepovers |
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2024-11-20 |
Sound velocities and thermal equation of state of <em>fcc</em>-iron-nickel alloys at high pressure and high temperature: Implications for the cores of Moon and several planets |
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2024-11-16 |
Lower mantle water distribution from <em>ab initio</em> proton diffusivity in bridgmanite |
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2024-11-16 |
Local sedimentary effects shaped key sulfur records after the Great Oxidation Event |
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2024-11-16 |
Mechanisms and timing of carbonaceous chondrite delivery to the Earth |
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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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