Earth and Planetary Science Letters

(The TQCC of Earth and Planetary Science Letters is 13. 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 2020-07-01 to 2024-07-01.)
Sedimentary host phases of mercury (Hg) and implications for use of Hg as a volcanic proxy132
China's Chang'e-5 landing site: Geology, stratigraphy, and provenance of materials104
The early Eocene rise of the Gonjo Basin, SE Tibet: From low desert to high forest97
Young lunar mare basalts in the Chang'e-5 sample return region, northern Oceanus Procellarum95
Gondwana's interlinked peripheral orogens78
Paired metamorphism in the Neoarchean: A record of accretionary-to-collisional orogenesis in the North China Craton70
First evidence of eclogites overprinted by ultrahigh temperature metamorphism in Everest East, Himalaya: Implications for collisional tectonics on early Earth66
IMS observations of infrasound and acoustic-gravity waves produced by the January 2022 volcanic eruption of Hunga, Tonga: A global analysis63
Mantle influx compensates crustal thinning beneath the Cathaysia Block, South China: Evidence from SINOPROBE reflection profiling60
A Neoproterozoic low-δ18O m60
Qinghai-Tibet Plateau wetting reduces permafrost thermal responses to climate warming59
Crustal-scale wedge tectonics at the narrow boundary between the Tibetan Plateau and Ordos block59
Assessing seasonal and interannual water storage variations in Taiwan using geodetic and hydrological data57
Low-temperature oceanic crust alteration and the isotopic budgets of potassium and magnesium in seawater54
Late Pliocene onset of the Cona rift, eastern Himalaya, confirms eastward propagation of extension in Himalayan-Tibetan orogen54
Early evolution of the solar accretion disk inferred from Cr-Ti-O isotopes in individual chondrules54
TTG generation by fluid-fluxed crustal melting: Direct evidence from the Proterozoic Georgetown Inlier, NE Australia51
Slab dehydration in warm subduction zones at depths of episodic slip and tremor49
Redox controls during magma ocean degassing49
Ice loss in the Northeastern Tibetan Plateau permafrost as seen by 16 yr of ESA SAR missions48
A catalogue of impact craters larger than 200 m and surface age analysis in the Chang'e-5 landing area47
Global and local drivers of the Ediacaran Shuram carbon isotope excursion45
Geophysical and cosmochemical evidence for a volatile-rich Mars45
Explosivity of basaltic lava fountains is controlled by magma rheology, ascent rate and outgassing45
Origin and evolution of fault-controlled hydrothermal dolomitization fronts: A new insight44
Origin of volatile element depletion among carbonaceous chondrites43
The 2018-ongoing Mayotte submarine eruption: Magma migration imaged by petrological monitoring43
The micrometeorite flux at Dome C (Antarctica), monitoring the accretion of extraterrestrial dust on Earth42
The tungsten-182 record of kimberlites above the African superplume: Exploring links to the core-mantle boundary42
Short duration of Early Permian Qiangtang-Panjal large igneous province: Implications for origin of the Neo-Tethys Ocean42
A disordered kinetic model for clumped isotope bond reordering in carbonates41
A plume-modified lithospheric barrier to the southeastward flow of partially molten Tibetan crust inferred from magnetotelluric data41
Expanse of Greater India in the late Cretaceous41
Holocene variability of East Asian summer monsoon as viewed from the speleothem δ40
An evaluation of the C/N ratio of the mantle from natural CO2-rich gas analysis: Geochemical and cosmochemical implications40
Astrochronology of the Ediacaran Shuram carbon isotope excursion, Oman40
Interannual flow dynamics driven by frontal retreat of a lake-terminating glacier in the Chinese Central Himalaya39
The tilted Iceland Plume and its effect on the North Atlantic evolution and magmatism39
Towards balancing the oceanic Ni budget38
Petrochronological close-up on the thermal structure of a paleo-subduction zone (W. Alps)37
A dynamic lithosphere–asthenosphere boundary near the equatorial Mid-Atlantic Ridge37
Spatio-temporal foreshock evolution of the 2019 M 6.4 and M 7.1 Ridgecrest, California earthquakes37
Long-lived (ca. 22–24 Myr) partial melts in the eastern Himalaya: Petrochronologic constraints and tectonic implications37
Deciphering the evolution and forcing mechanisms of glaciation over the Himalayan-Tibetan orogen during the past 20,000 years36
Temperature changes across the Paleocene-Eocene Thermal Maximum – a new high-resolution TEX86 temperature record from the Eastern North Sea Basin36
Northwest Pacific-Izanagi plate tectonics since Cretaceous times from western Pacific mantle structure36
The stabilizing effect of high pore-fluid pressure along subduction megathrust faults: Evidence from friction experiments on accretionary sediments from the Nankai Trough35
Global zircon analysis records a gradual rise of continental crust throughout the Neoarchean35
Geodetic imaging of shallow creep along the Xianshuihe fault and its frictional properties34
Magnesium isotopic fractionation during basalt differentiation as recorded by evolved magmas34
The effect of wind speed averaging time on the calculation of sand drift potential: New scaling laws34
Controls on the abundance, provenance and age of organic carbon buried in continental margin sediments34
Was climatic cooling during the earliest Carboniferous driven by expansion of seed plants?34
Controls on the magmatic fraction of extension at mid-ocean ridges33
Origin of hydrogen isotopic variations in chondritic water and organics33
Evidence for crustal removal, tectonic erosion and flare-ups from the Japanese evolving forearc sediment provenance33
Temperature signals of ice core and speleothem isotopic records from Asian monsoon region as indicated by precipitation δ18O33
Thermobarometry of CO2-rich, silica-undersaturated melts constrains cratonic lithosphere thinning through time in areas of kimberlitic magmatism33
Exploring laser ablation U–Pb dating of regional metamorphic garnet – The Straits Schist, Connecticut, USA32
Post-depositional REE mobility in a Paleoarchean banded iron formation revealed by La-Ce geochronology: A cautionary tale for signals of ancient oxygenation32
Origin of a global carbonate layer deposited in the aftermath of the Cretaceous-Paleogene boundary impact32
Strong shear softening induced by superionic hydrogen in Earth's inner core32
Plate tectonics and mantle controls on plume dynamics32
Frontal ablation and mass loss of the Patagonian icefields32
Expanded lacustrine sedimentation in the Qaidam Basin on the northern Tibetan Plateau: Manifestation of climatic wetting during the Oligocene icehouse32
Towards understanding the origin of massive dolostones31
Sediment and ocean crust both melt at subduction zones31
Understanding ancient tectonic settings through detrital zircon analysis31
Chondritic mercury isotopic composition of Earth and evidence for evaporative equilibrium degassing during the formation of eucrites31
Highly dynamic marine redox state through the Cambrian explosion highlighted by authigenic δ238U records31
Hotspots and mantle plumes revisited: Towards reconciling the mantle heat transfer discrepancy31
New early oligocene zircon U-Pb dates for the ‘Miocene’ Wenshan Basin, Yunnan, China: Biodiversity and paleoenvironment31
Atmospheric river changes shaped mid-latitude hydroclimate since the mid-Holocene30
Astronomically forced climate change in the late Cambrian30
Partitioning riverine sulfate sources using oxygen and sulfur isotopes: Implications for carbon budgets of large rivers30
Pulsed oxygenation events drove progressive oxygenation of the early Mesoproterozoic ocean30
Orbitally-paced climate change in the early Cambrian and its implications for the history of the Solar System30
Scaling laws for the geometry of an impact-induced magma ocean30
Assessing the presence of volatile-bearing mineral phases in the cratonic mantle as a possible cause of mid-lithospheric discontinuities30
Nucleosynthetic Pt isotope anomalies and the Hf-W chronology of core formation in inner and outer solar system planetesimals30
Co-seismic rupture of the 2021, M 7.4 Maduo earthquake (northern Tibet): Short-cutting of the Kunlun fault big bend29
Was the Pamir salient built along a Late Paleozoic embayment on the southern Asian margin?29
Petrogenetic processes at the tipping point of plate tectonics: Hf-O isotope ternary modelling of Earth's last TTG to sanukitoid transition29
Hypocentral dependent shallow slip distribution and rupture extents along a strike-slip fault29
Deformation-enhanced recrystallization of titanite drives decoupling between U-Pb and trace elements29
An extended period of extremely weak geomagnetic field suggested by palaeointensities from the Ediacaran Grenville dykes (SE Canada)29
The 22 July 2020 M 7.8 Shumagin seismic gap earthquake: Partial rupture of a weakly coupled megathrust28
Isotopic fingerprinting of biogeochemical processes and iron sources in the iron-limited surface Southern Ocean28
Resistivity saturation of hcp Fe-Si alloys in an internally heated diamond anvil cell: A key to assessing the Earth's core conductivity28
Mantle source characteristics and magmatic processes during the 2021 La Palma eruption28
Photochemical modelling of atmospheric oxygen levels confirms two stable states28
Strain localization and fluid-assisted deformation in apatite and its influence on trace elements and U–Pb systematics28
Unravelling Middle to Late Jurassic palaeoceanographic and palaeoclimatic signals in the Hebrides Basin using belemnite clumped isotope thermometry27
Kinematics of the ∼1000 km Haiyuan fault system in northeastern Tibet from high-resolution Sentinel-1 InSAR velocities: Fault architecture, slip rates, and partitioning27
Timescales of subduction initiation and evolution of subduction thermal regimes27
Deep learning for laboratory earthquake prediction and autoregressive forecasting of fault zone stress27
Long-term Phanerozoic sea level change from solid Earth processes27
The young Sun's XUV-activity as a constraint for lower CO2-limits in the Earth's Archean atmosphere27
Flotation mechanism of sulphide melt on vapour bubbles in partially molten magmatic systems27
The 2010 Haiti earthquake revisited: An acoustic intensity map from remote atmospheric infrasound observations27
Fluid mixing as primary trigger for cassiterite deposition: Evidence from in situ δ18O-δ11B analysis of tourmaline from the world-class San Rafael tin (-copper) deposit, Peru27
Enhanced water loss from the martian atmosphere during a regional-scale dust storm and implications for long-term water loss26
Controls on the cadmium isotope composition of modern marine sediments26
Geomorphologic exploration targets at the Zhurong landing site in the southern Utopia Planitia of Mars26
Three North African dust source areas and their geochemical fingerprint26
Crustal tilting and differential exhumation of Gangdese Batholith in southern Tibet revealed by bedrock pressures26
Preconditioning by sediment accumulation can produce powerful turbidity currents without major external triggers26
Limited iodate reduction in shipboard seawater incubations from the Eastern Tropical North Pacific oxygen deficient zone26
Fault roughness controls sliding instability26
Quantitative estimates of Holocene glacier meltwater variations on the Western Tibetan Plateau26
Can volcanism build hydrogen-rich early atmospheres?26
The role of inherited crustal and lithospheric architecture during the evolution of the Red Sea: Insights from three dimensional analogue experiments26
Copper-mineralised porphyries sample the evolution of a large-volume silicic magma reservoir from rapid assembly to solidification26
The fate of fluvially-deposited organic carbon during transient floodplain storage25
Widespread silicic and alkaline magmatism synchronous with the Deccan Traps flood basalts, India25
Cosmogenic 10Be production records reveal dynamics of geomagnetic dipole moment (GDM) over the Laschamp excursion (20–60 ka)25
Calcium isotope constraints on OIB and MORB petrogenesis: The importance of melt mixing25
Subcretionary tectonics: Linking variability in the expression of subduction along the Cascadia forearc25
Controls on boron isotopes in a cold-water coral and the cost of resilience to ocean acidification25
The phases of the Moon: Modelling crystallisation of the lunar magma ocean through equilibrium thermodynamics25
Major Early-Middle Devonian oceanic oxygenation linked to early land plant evolution detected using high-resolution U isotopes of marine limestones25
Reversible scavenging traps hydrothermal iron in the deep ocean25
New cosmogenic nuclide burial-dating model indicates onset of major glaciations in the Alps during Middle Pleistocene Transition25
Long-term evolution of terrestrial weathering and its link to Earth's oxygenation25
High pressure-temperature phase relations of basaltic crust up to mid-mantle conditions25
Breakup with benefits - hydrothermal mineral systems related to the disintegration of a supercontinent25
On Archean craton growth and stabilisation: Insights from lithospheric resistivity structure of the Superior Province25
Westerly jet stream controlled climate change mode since the Last Glacial Maximum in the northern Qinghai-Tibet Plateau25
Metal-silicate mixing by large Earth-forming impacts25
Transport properties of Fe-Ni-Si alloys at Earth's core conditions: Insight into the viability of thermal and compositional convection24
Role of sulfate in the transport and enrichment of REE in hydrothermal systems24
Event-dominated transport, provenance, and burial of organic carbon in the Japan Trench24
Coexisting diverse P–T–t paths during Neoarchean Sagduction: Insights from numerical modeling and applications to the eastern North China Craton24
Competition between preslip and deviatoric stress modulates precursors for laboratory earthquakes24
Periodic oceanic euxinia and terrestrial fluxes linked to astronomical forcing during the Late Devonian Frasnian–Famennian mass extinction24
Disparities in oxygen isotopes of detrital and igneous zircon identify erosional bias in crustal rock record24
Combination of Δ47 and U-Pb dating in tectonic calcite veins unravel the last pulses related to the Pyrenean Shortening (Spain)24
Mercury isotope evidence for regional volcanism during the Frasnian-Famennian transition24
Multicomponent diffusion of F, Cl and OH in apatite with application to magma ascent rates24
Reconstruction of the 2018 tsunamigenic flank collapse and eruptive activity at Anak Krakatau based on eyewitness reports, seismo-acoustic and satellite observations24
Dislocation interactions during low-temperature plasticity of olivine and their impact on the evolution of lithospheric strength24
Warm and oxidizing slabs limit ingassing efficiency of nitrogen to the mantle24
Reappraisal of purported ca. 3.7 Ga stromatolites from the Isua Supracrustal Belt (West Greenland) from detailed chemical and structural analysis24
Using stable isotopes to distinguish atmospheric nitrate production and its contribution to the surface ocean across hemispheres24
Chromium isotope systematics and the diagenesis of marine carbonates24
Evidence for methane isotopic bond re-ordering in gas reservoirs sourcing cold seeps from the Sea of Marmara24
Black Sea paleosalinity evolution since the last deglaciation reconstructed from alkenone-inferred Isochrysidales diversity24
On the petrogenesis of lunar troctolites: New insights into cumulate mantle overturn & mantle exposures in impact basins24
The 2019 Ridgecrest, California earthquake sequence: Evolution of seismic and aseismic slip on an orthogonal fault system24
The deep Shumagin gap filled: Kinematic rupture model and slip budget analysis of the 2020 Mw 7.8 Simeonof earthquake constrained by GNSS, global seismic waveforms, and floating InSAR24
Cryogenian interglacial greenhouse driven by enhanced volcanism: Evidence from mercury records24
Hf isotopic ratios in zircon reveal processes of anatexis and pluton construction23
Centimeter-resolution topographic modeling and fine-scale analysis of craters and rocks at the Chang'E-4 landing site23
Seismic swarms produced by rapid fluid injection into a low permeability laboratory fault23
Evidence for crustal seismic anisotropy at the InSight lander site23
Pervasive low-velocity layer atop the 410-km discontinuity beneath the northwest Pacific subduction zone: Implications for rheology and geodynamics23
Seismic hazard of the western Makran subduction zone: Insight from mechanical modelling and inferred frictional properties23
Polarity-reversal subduction zone initiation triggered by buoyant plateau obstruction23
Long-term evolution of a plume-induced subduction in the Neotethys realm23
Subduction initiation and the rise of the Shillong Plateau23
Reworking subducted sediments in arc magmas and the isotopic diversity of the continental crust: The case of the Ordovician Famatinian crustal section, Argentina23
Miocene to present oceanographic variability in the Scotia Sea and Antarctic ice sheets dynamics: Insight from revised seismic-stratigraphy following IODP Expedition 38223
Predicting the proximity to macroscopic failure using local strain populations from dynamic in situ X-ray tomography triaxial compression experiments on rocks23
Molybdenum isotope systematics of lavas from the East Pacific Rise: Constraints on the source of enriched mid-ocean ridge basalt23
Thermal conductivity of Fe-bearing post-perovskite in the Earth's lowermost mantle23
Evaluation of shallow-water carbonates as a seawater zinc isotope archive23
Zinc- and cadmium-isotope evidence for redox-driven perturbations to global micronutrient cycles during Oceanic Anoxic Event 2 (Late Cretaceous)23
Assessing the potential capability of reconstructing glacial Atlantic water masses and AMOC using multiple proxies in CESM23
The temporal distribution of Earth's supermountains and their potential link to the rise of atmospheric oxygen and biological evolution22
Glacial pumping of a magma-charged lithosphere: A model for glaciovolcanic causality in magmatic arcs22
Aquifer deformation and active faulting in Salt Lake Valley, Utah, USA22
The evolution of lithium isotope signatures in fluids draining actively weathering hillslopes22
Impact of power-law rheology on the viscoelastic relaxation pattern and afterslip distribution following the 2010 Mw 8.8 Maule earthquake22
Into the deep and beyond: Carbon and nitrogen subduction recycling in secondary peridotites22
Granite geochemistry is not diagnostic of the role of water in the source22
Layered crustal azimuthal anisotropy beneath the northeastern Tibetan Plateau revealed by Rayleigh-wave Eikonal tomography22
Integrated magnetotelluric and petrological analysis of felsic magma reservoirs: Insights from Ethiopian rift volcanoes22
Lower-altitude of the Himalayas before the mid-Pliocene as constrained by hydrological and thermal conditions22
Late Ediacaran paleogeography of Avalonia and the Cambrian assembly of West Gondwana22
The Ca and Mg isotope record of the Cryogenian Trezona carbon isotope excursion22
Controls by rheological structure of the lithosphere on the temporal evolution of continental magmatism: Inferences from the Pannonian Basin system22
Southeastern margin of the Tibetan Plateau stopped expanding in the late Miocene22
Rock abundance and evolution of the shallow stratum on Chang'e-4 landing site unveiled by lunar penetrating radar data22
The role of incremental magma chamber growth on ore formation in porphyry copper systems22
Hydrothermal alteration associated with the Chicxulub impact crater upper peak-ring breccias22
Toarcian climate and carbon cycle perturbations – its impact on sea-level changes, enhanced mobilization and oxidation of fossil organic matter22
Indian continental lithosphere and related volcanism beneath Myanmar: Constraints from local earthquake tomography22
Linking surface deformation to thermal and mechanical magma chamber processes22
Mineral inclusions are not immutable: Evidence of post-entrapment thermally-induced shape change of quartz in garnet22
Phyllosilicate controls on magnesium isotopic fractionation during weathering of granites: Implications for continental weathering and riverine system21
Partial melting of ultrahigh-pressure eclogite by omphacite-breakdown facilitates exhumation of deeply-subducted crust21
Covariation of cross-divide differences in denudation rate and χ: Implications for drainage basin reorganization in the Qilian Shan, northeast Tibet21
Rise and fall of the Acadian altiplano: Evidence for a Paleozoic orogenic plateau in New England21
Uniform oxygen fugacity of shergottite mantle sources and an oxidized martian lithosphere21
Oceanic anoxia and extinction in the latest Ordovician21
Bulk composition of regolith fines on lunar crater floors: Initial investigation by LRO/Mini-RF21
Local melt contamination and global climate impact: Dating the emplacement of Karoo LIP sills into organic-rich shale21
Enhanced ocean connectivity and volcanism instigated global onset of Cretaceous Oceanic Anoxic Event 2 (OAE2) ∼94.5 million years ago21
Evolution of the early to late Archean mantle from Hf-Nd-Ce isotope systematics in basalts and komatiites from the Pilbara Craton21
Pushing the boundary: A calibrated Ediacaran-Cambrian stratigraphic record from the Nama Group in northwestern Republic of South Africa21
Constraints on Archean crust recycling and the origin of mantle redox variability from the δ44/40Ca – δ18O – fO2 signatures of cratonic eclogites21
Diffusion anisotropy of Ti in zircon and implications for Ti-in-zircon thermometry21
Clay minerals affect calcium (magnesium) carbonate precipitation and aging21
Adakite generation as a result of fluid-fluxed melting at normal lower crustal pressures21
The competing effects of terrestrial evapotranspiration and raindrop re-evaporation on the deuterium excess of continental precipitation21
Deglaciation of Pope Glacier implies widespread early Holocene ice sheet thinning in the Amundsen Sea sector of Antarctica21
Mountain building, mantle convection, and supercontinents: revisited21
Meso- to nano-scale evidence of fluid-assisted co-seismic slip along the normal Mt. Morrone Fault, Italy: Implications for earthquake hydrogeochemical precursors21
A high-resolution map of Hawaiian ULVZ morphology from ScS phases21
Inverse methods for consistent quantification of seafloor anoxia using uranium isotope data from marine sediments20
Spatial distribution of 1.4-1.3 Ga LIPs and carbonatite-related REE deposits: Evidence for large-scale continental rifting in the Columbia (Nuna) supercontinent20
Asian monsoon evolution linked to Pacific temperature gradients since the Late Miocene20
Shale and pyrite Re-Os ages from the Hornby Bay and Amundsen basins provide new chronological markers for Mesoproterozoic stratigraphic successions of northern Canada20
A short-lived 26Al induced hydrothermal alteration event in the outer solar system: Constraints from Mn/Cr ages of carbonates20
Anomalously low aftershock productivity of the 2019 M 8.0 energetic intermediate-depth faulting beneath Peru20
Elasticity of hydrous ringwoodite at mantle conditions: Implication for water distribution in the lowermost mantle transition zone20
Ancient refractory asthenosphere revealed by mantle re-melting at the Arctic Mid Atlantic Ridge20
The cascading foreshock sequence of the Ms 6.4 Yangbi earthquake in Yunnan, China20
The transformation of aragonite to calcite in the presence of magnesium: Implications for marine diagenesis20
Decoupled oxygenation of the Ediacaran ocean and atmosphere during the rise of early animals20
A short-lived oxidation event during the early Ediacaran and delayed oxygenation of the Proterozoic ocean20
Deciphering relationships between the Nicobar and Bengal submarine fans, Indian Ocean20
Arrest of the Mw 6.8 January 24, 2020 Elaziğ (Turkey) earthquake by shallow fault creep20
A high-TOC shale in a low productivity world: The late Mesoproterozoic Arctic Bay Formation, Nunavut20
Bridgmanite is nearly dry at the top of the lower mantle20
“Brittle structural facies” analysis: A diagnostic method to unravel and date multiple slip events of long-lived faults20
Discharge rate of explosive volcanic eruption controls runout distance of pyroclastic density currents20
The metal–silicate partitioning of carbon during Earth's accretion and its distribution in the early solar system20
The coupled Hf-Nd isotope record of the early Earth in the Pilbara Craton20
Assessing the role of clay and salts on the origin of MARSIS basal bright reflections20
Birth of the Pearl River at 30 Ma: Evidence from sedimentary records in the northern South China Sea20
Isotopic and textural analysis of giant unmelted micrometeorites – identification of new material from intensely altered 16O-poor water-rich asteroids20
Earth's oldest hotspot track at ca. 1.8 Ga advected by a global subduction system20
Post-collisional batholiths do contribute to continental growth19
Along-strike variations in intermediate-depth seismicity and arc magmatism along the Alaska Peninsula19
Electrical resistivity imaging of continental United States from three-dimensional inversion of EarthScope USArray magnetotelluric data19
Mg-Ba-Sr-Nd isotopic evidence for a mélange origin of early Paleozoic arc magmatism19
Refining trace metal temperature proxies in cold-water scleractinian and stylasterid corals19
Mantle sources and magma evolution in Europe's largest rare earth element belt (Gardar Province, SW Greenland): New insights from sulfur isotopes19
Reversing transverse dunes: Modelling of airflow switching using 3D computational fluid dynamics19
An iron isotope perspective on back-arc basin development: Messages from Mariana Trough basalts19
Late Triassic uplift, magmatism and extension of the northern North China block: Mantle signatures in the surface19
Novel watermass reconstruction in the Early Mississippian Appalachian Seaway based on integrated proxy records of redox and salinity19
A lithospheric-scale thrust-wedge model for the formation of the northern Tibetan plateau margin: Evidence from high-resolution seismic imaging19
Isotopic disequilibrium of Cu in marine ferromanganese crusts: Evidence from ab initio predictions of Cu isotope fractionation on sorption to birnessite19
Isotopic constraints on sources, production, and phase partitioning for nitrate in the atmosphere and snowfall in coastal East Antarctica19
Rate of active shortening across the southern thrust front of the Greater Caucasus in western Georgia from kinematic modeling of folded river terraces above a listric thrust19
Bioturbation feedbacks on the phosphorus cycle19
A tale of two domes: Neogene to recent volcanism and dynamic uplift of northeast Brazil and southwest Africa19
Onset of magma ocean solidification on Mars inferred from Mn-Cr chronometry19