Earth and Planetary Science Letters

Papers
(The H4-Index of Earth and Planetary Science Letters is 36. 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 2020-11-01 to 2024-11-01.)
ArticleCitations
China's Chang'e-5 landing site: Geology, stratigraphy, and provenance of materials112
Young lunar mare basalts in the Chang'e-5 sample return region, northern Oceanus Procellarum98
Gondwana's interlinked peripheral orogens86
First evidence of eclogites overprinted by ultrahigh temperature metamorphism in Everest East, Himalaya: Implications for collisional tectonics on early Earth71
IMS observations of infrasound and acoustic-gravity waves produced by the January 2022 volcanic eruption of Hunga, Tonga: A global analysis67
A Neoproterozoic low-δ18O ma65
Qinghai-Tibet Plateau wetting reduces permafrost thermal responses to climate warming63
Assessing seasonal and interannual water storage variations in Taiwan using geodetic and hydrological data63
Crustal-scale wedge tectonics at the narrow boundary between the Tibetan Plateau and Ordos block61
Redox controls during magma ocean degassing60
TTG generation by fluid-fluxed crustal melting: Direct evidence from the Proterozoic Georgetown Inlier, NE Australia58
Early evolution of the solar accretion disk inferred from Cr-Ti-O isotopes in individual chondrules58
Explosivity of basaltic lava fountains is controlled by magma rheology, ascent rate and outgassing54
Global and local drivers of the Ediacaran Shuram carbon isotope excursion52
Slab dehydration in warm subduction zones at depths of episodic slip and tremor51
Geophysical and cosmochemical evidence for a volatile-rich Mars50
Origin of volatile element depletion among carbonaceous chondrites48
The micrometeorite flux at Dome C (Antarctica), monitoring the accretion of extraterrestrial dust on Earth48
An evaluation of the C/N ratio of the mantle from natural CO2-rich gas analysis: Geochemical and cosmochemical implications46
Holocene variability of East Asian summer monsoon as viewed from the speleothem δ44
Geodetic imaging of shallow creep along the Xianshuihe fault and its frictional properties43
The 2018-ongoing Mayotte submarine eruption: Magma migration imaged by petrological monitoring43
Short duration of Early Permian Qiangtang-Panjal large igneous province: Implications for origin of the Neo-Tethys Ocean43
A disordered kinetic model for clumped isotope bond reordering in carbonates43
The tilted Iceland Plume and its effect on the North Atlantic evolution and magmatism42
Sediment and ocean crust both melt at subduction zones42
Controls on the abundance, provenance and age of organic carbon buried in continental margin sediments40
Magnesium isotopic fractionation during basalt differentiation as recorded by evolved magmas40
Spatio-temporal foreshock evolution of the 2019 M 6.4 and M 7.1 Ridgecrest, California earthquakes40
Northwest Pacific-Izanagi plate tectonics since Cretaceous times from western Pacific mantle structure38
Long-lived (ca. 22–24 Myr) partial melts in the eastern Himalaya: Petrochronologic constraints and tectonic implications38
Evidence for crustal removal, tectonic erosion and flare-ups from the Japanese evolving forearc sediment provenance38
A dynamic lithosphere–asthenosphere boundary near the equatorial Mid-Atlantic Ridge38
Exploring laser ablation U–Pb dating of regional metamorphic garnet – The Straits Schist, Connecticut, USA37
Global zircon analysis records a gradual rise of continental crust throughout the Neoarchean37
Was climatic cooling during the earliest Carboniferous driven by expansion of seed plants?37
Thermobarometry of CO2-rich, silica-undersaturated melts constrains cratonic lithosphere thinning through time in areas of kimberlitic magmatism36
Nucleosynthetic Pt isotope anomalies and the Hf-W chronology of core formation in inner and outer solar system planetesimals36
Frontal ablation and mass loss of the Patagonian icefields36
The stabilizing effect of high pore-fluid pressure along subduction megathrust faults: Evidence from friction experiments on accretionary sediments from the Nankai Trough36
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