Earth and Planetary Science Letters

Papers
(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 2020-04-01 to 2024-04-01.)
ArticleCitations
Sedimentary host phases of mercury (Hg) and implications for use of Hg as a volcanic proxy119
China's Chang'e-5 landing site: Geology, stratigraphy, and provenance of materials99
The early Eocene rise of the Gonjo Basin, SE Tibet: From low desert to high forest90
Young lunar mare basalts in the Chang'e-5 sample return region, northern Oceanus Procellarum89
Qaidam Basin leaf fossils show northeastern Tibet was high, wet and cool in the early Oligocene79
Astronomical forcing and sedimentary noise modeling of lake-level changes in the Paleogene Dongpu Depression of North China70
Gondwana's interlinked peripheral orogens68
Does pulsed Tibetan deformation correlate with Indian plate motion changes?68
S-type granites: Their origin and distribution through time as determined from detrital zircons67
Paired metamorphism in the Neoarchean: A record of accretionary-to-collisional orogenesis in the North China Craton67
Potassium isotope fractionation during chemical weathering of basalts65
First evidence of eclogites overprinted by ultrahigh temperature metamorphism in Everest East, Himalaya: Implications for collisional tectonics on early Earth62
Mantle influx compensates crustal thinning beneath the Cathaysia Block, South China: Evidence from SINOPROBE reflection profiling60
Rock strength and structural controls on fluvial erodibility: Implications for drainage divide mobility in a collisional mountain belt59
Qinghai-Tibet Plateau wetting reduces permafrost thermal responses to climate warming56
Crustal-scale wedge tectonics at the narrow boundary between the Tibetan Plateau and Ordos block56
IMS observations of infrasound and acoustic-gravity waves produced by the January 2022 volcanic eruption of Hunga, Tonga: A global analysis55
A Neoproterozoic low-δ18O m54
Late Pliocene onset of the Cona rift, eastern Himalaya, confirms eastward propagation of extension in Himalayan-Tibetan orogen49
Early evolution of the solar accretion disk inferred from Cr-Ti-O isotopes in individual chondrules49
Peel-back controlled lithospheric convergence explains the secular transitions in Archean metamorphism and magmatism49
Assessing seasonal and interannual water storage variations in Taiwan using geodetic and hydrological data48
Enhanced chemical weathering triggered an expansion of euxinic seawater in the aftermath of the Sturtian glaciation47
Low-temperature oceanic crust alteration and the isotopic budgets of potassium and magnesium in seawater47
A high-resolution Middle to Late Permian paleotemperature curve reconstructed using oxygen isotopes of well-preserved brachiopod shells46
Novel insights from Fe-isotopes into the lithological heterogeneity of Ocean Island Basalts and plume-influenced MORBs46
The oceanic biogeochemistry of nickel and its isotopes: New data from the South Atlantic and the Southern Ocean biogeochemical divide46
TTG generation by fluid-fluxed crustal melting: Direct evidence from the Proterozoic Georgetown Inlier, NE Australia45
Ice loss in the Northeastern Tibetan Plateau permafrost as seen by 16 yr of ESA SAR missions45
Slab dehydration in warm subduction zones at depths of episodic slip and tremor44
Redox controls during magma ocean degassing43
Dilatancy-induced fluid pressure drop during dynamic rupture: Direct experimental evidence and consequences for earthquake dynamics43
Subduction initiation of the SE Paleo-Asian Ocean: Evidence from a well preserved intra-oceanic forearc ophiolite fragment in central Inner Mongolia, North China43
Evaluating a primary carbonate pathway for manganese enrichments in reducing environments42
Europium and barium enrichments in compositionally zoned felsic tuffs: A smoking gun for the origin of chemical and physical gradients by cumulate melting42
Geophysical and cosmochemical evidence for a volatile-rich Mars42
Detrital zircon evidence for change in geodynamic regime of continental crust formation 3.7–3.6 billion years ago42
Explosivity of basaltic lava fountains is controlled by magma rheology, ascent rate and outgassing42
Origin and evolution of fault-controlled hydrothermal dolomitization fronts: A new insight41
A catalogue of impact craters larger than 200 m and surface age analysis in the Chang'e-5 landing area41
Mechanisms and patterns of magmatic fluid transport in cooling hydrous intrusions41
Chemical evolution of the continental crust from a data-driven inversion of terrigenous sediment compositions41
Origin of volatile element depletion among carbonaceous chondrites41
The tungsten-182 record of kimberlites above the African superplume: Exploring links to the core-mantle boundary40
A plume-modified lithospheric barrier to the southeastward flow of partially molten Tibetan crust inferred from magnetotelluric data39
U-Pb zircon age constraints on the earliest eruptions of the Deccan Large Igneous Province, Malwa Plateau, India39
Expanse of Greater India in the late Cretaceous39
Generation of Eoarchean continental crust from altered mafic rocks derived from a chondritic mantle: The ∼3.72 Ga Aktash gneisses, Tarim Craton (NW China)38
Interannual flow dynamics driven by frontal retreat of a lake-terminating glacier in the Chinese Central Himalaya38
An evaluation of the C/N ratio of the mantle from natural CO2-rich gas analysis: Geochemical and cosmochemical implications38
The micrometeorite flux at Dome C (Antarctica), monitoring the accretion of extraterrestrial dust on Earth38
Short duration of Early Permian Qiangtang-Panjal large igneous province: Implications for origin of the Neo-Tethys Ocean38
Global and local drivers of the Ediacaran Shuram carbon isotope excursion37
A disordered kinetic model for clumped isotope bond reordering in carbonates37
Astrochronology of the Ediacaran Shuram carbon isotope excursion, Oman36
The 2018-ongoing Mayotte submarine eruption: Magma migration imaged by petrological monitoring36
Holocene variability of East Asian summer monsoon as viewed from the speleothem δ36
Spatio-temporal foreshock evolution of the 2019 M 6.4 and M 7.1 Ridgecrest, California earthquakes36
Active crustal deformation and rotations in the southwestern Balkans from continuous GPS measurements36
A dynamic lithosphere–asthenosphere boundary near the equatorial Mid-Atlantic Ridge35
Exhumation history of the north-central Shanxi Rift, North China, revealed by low-temperature thermochronology34
Petrochronological close-up on the thermal structure of a paleo-subduction zone (W. Alps)34
Long-lived (ca. 22–24 Myr) partial melts in the eastern Himalaya: Petrochronologic constraints and tectonic implications34
Towards balancing the oceanic Ni budget34
Deciphering the evolution and forcing mechanisms of glaciation over the Himalayan-Tibetan orogen during the past 20,000 years33
Characteristic landslide distributions: An investigation of landscape controls on landslide size33
Inter-relationship and environmental significance of stalagmite δ13C and δ18O records from Zhenzhu Cave, north China, over the last 130 ka33
Was climatic cooling during the earliest Carboniferous driven by expansion of seed plants?33
Subsolar Al/Si and Mg/Si ratios of non-carbonaceous chondrites reveal planetesimal formation during early condensation in the protoplanetary disk33
A coupled carbon-silicon cycle model over Earth history: Reverse weathering as a possible explanation of a warm mid-Proterozoic climate32
The effect of wind speed averaging time on the calculation of sand drift potential: New scaling laws32
Pervasive sources of isotopically light zinc in the North Atlantic Ocean32
Geochronologic constraints on deformation and metasomatism along an exhumed mylonitic shear zone using apatite U-Pb, geochemistry, and microtextural analysis31
Frontal ablation and mass loss of the Patagonian icefields31
The tilted Iceland Plume and its effect on the North Atlantic evolution and magmatism31
The stabilizing effect of high pore-fluid pressure along subduction megathrust faults: Evidence from friction experiments on accretionary sediments from the Nankai Trough31
Temperature signals of ice core and speleothem isotopic records from Asian monsoon region as indicated by precipitation δ18O31
A 3800 yr paleoseismic record (Lake Hazar sediments, eastern Turkey): Implications for the East Anatolian Fault seismic cycle31
Simulation of early Eocene water isotopes using an Earth system model and its implication for past climate reconstruction30
Northwest Pacific-Izanagi plate tectonics since Cretaceous times from western Pacific mantle structure30
Global zircon analysis records a gradual rise of continental crust throughout the Neoarchean30
Geodetic imaging of shallow creep along the Xianshuihe fault and its frictional properties30
Climatic fluctuations modeled for carbon and sulfur emissions from end-Triassic volcanism30
The evolution and distribution of recycled oceanic crust in the Earth's mantle: Insight from geodynamic models29
Expanded lacustrine sedimentation in the Qaidam Basin on the northern Tibetan Plateau: Manifestation of climatic wetting during the Oligocene icehouse29
The multiple sulphur isotope fingerprint of a sub-seafloor oxidative sulphur cycle driven by iron29
Post-depositional REE mobility in a Paleoarchean banded iron formation revealed by La-Ce geochronology: A cautionary tale for signals of ancient oxygenation29
Magnesium isotopic fractionation during basalt differentiation as recorded by evolved magmas29
The triple oxygen isotope composition of Precambrian chert29
Slab-controlled elemental–isotopic enrichments during subduction initiation magmatism and variations in forearc chemostratigraphy29
Temperature changes across the Paleocene-Eocene Thermal Maximum – a new high-resolution TEX86 temperature record from the Eastern North Sea Basin29
Origin of a global carbonate layer deposited in the aftermath of the Cretaceous-Paleogene boundary impact29
Strong shear softening induced by superionic hydrogen in Earth's inner core29
Atmospheric river changes shaped mid-latitude hydroclimate since the mid-Holocene28
Pulsed oxygenation events drove progressive oxygenation of the early Mesoproterozoic ocean28
Exploring laser ablation U–Pb dating of regional metamorphic garnet – The Straits Schist, Connecticut, USA28
Episodic formation of refractory inclusions in the Solar System and their presolar heritage28
New early oligocene zircon U-Pb dates for the ‘Miocene’ Wenshan Basin, Yunnan, China: Biodiversity and paleoenvironment28
Primary CO2-bearing fluid inclusions in granulitic garnet usually do not survive28
Evidence for crustal removal, tectonic erosion and flare-ups from the Japanese evolving forearc sediment provenance28
Towards understanding the origin of massive dolostones28
Controls on the magmatic fraction of extension at mid-ocean ridges28
Controls on the abundance, provenance and age of organic carbon buried in continental margin sediments28
Climatic patterns over the European Alps during the LGM derived from inversion of the paleo-ice extent28
Was the Pamir salient built along a Late Paleozoic embayment on the southern Asian margin?28
Deformation-enhanced recrystallization of titanite drives decoupling between U-Pb and trace elements27
Ti-in-quartz thermobarometry and TiO2 solubility in rhyolitic melts: New experiments and parametrization27
Partitioning riverine sulfate sources using oxygen and sulfur isotopes: Implications for carbon budgets of large rivers27
Plate tectonics and mantle controls on plume dynamics27
Highly dynamic marine redox state through the Cambrian explosion highlighted by authigenic δ238U records27
Unravelling Middle to Late Jurassic palaeoceanographic and palaeoclimatic signals in the Hebrides Basin using belemnite clumped isotope thermometry27
An extended period of extremely weak geomagnetic field suggested by palaeointensities from the Ediacaran Grenville dykes (SE Canada)27
The 22 July 2020 M 7.8 Shumagin seismic gap earthquake: Partial rupture of a weakly coupled megathrust27
Large isotopic variability at the micron-scale in ‘Shuram’ excursion carbonates from South Australia27
Origin of hydrogen isotopic variations in chondritic water and organics27
Sediment and ocean crust both melt at subduction zones27
Understanding ancient tectonic settings through detrital zircon analysis26
Thermobarometry of CO2-rich, silica-undersaturated melts constrains cratonic lithosphere thinning through time in areas of kimberlitic magmatism26
Hypocentral dependent shallow slip distribution and rupture extents along a strike-slip fault26
Resistivity saturation of hcp Fe-Si alloys in an internally heated diamond anvil cell: A key to assessing the Earth's core conductivity26
Chondritic mercury isotopic composition of Earth and evidence for evaporative equilibrium degassing during the formation of eucrites26
Can volcanism build hydrogen-rich early atmospheres?26
Nucleosynthetic Pt isotope anomalies and the Hf-W chronology of core formation in inner and outer solar system planetesimals26
Geomorphologic exploration targets at the Zhurong landing site in the southern Utopia Planitia of Mars25
Late Cenozoic topographic evolution of the Eastern Cordillera and Puna Plateau margin in the southern Central Andes (NW Argentina)25
Hotspots and mantle plumes revisited: Towards reconciling the mantle heat transfer discrepancy25
Crustal tilting and differential exhumation of Gangdese Batholith in southern Tibet revealed by bedrock pressures25
Orbitally-paced climate change in the early Cambrian and its implications for the history of the Solar System25
Limited iodate reduction in shipboard seawater incubations from the Eastern Tropical North Pacific oxygen deficient zone25
Detrital rutile ages can deduce the tectonic setting of sedimentary basins25
Photochemical modelling of atmospheric oxygen levels confirms two stable states25
Astronomically forced climate change in the late Cambrian25
Mantle source characteristics and magmatic processes during the 2021 La Palma eruption25
Scaling laws for the geometry of an impact-induced magma ocean25
Chromium isotope systematics and the diagenesis of marine carbonates24
Preconditioning by sediment accumulation can produce powerful turbidity currents without major external triggers24
The young Sun's XUV-activity as a constraint for lower CO2-limits in the Earth's Archean atmosphere24
Subcretionary tectonics: Linking variability in the expression of subduction along the Cascadia forearc24
Petrogenetic processes at the tipping point of plate tectonics: Hf-O isotope ternary modelling of Earth's last TTG to sanukitoid transition24
Provenance and erosional impact of Quaternary megafloods through the Yarlung-Tsangpo Gorge from zircon U-Pb geochronology of flood deposits, eastern Himalaya24
Strain localization and fluid-assisted deformation in apatite and its influence on trace elements and U–Pb systematics24
Assessing the presence of volatile-bearing mineral phases in the cratonic mantle as a possible cause of mid-lithospheric discontinuities24
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
Appraisal of alkenone- and archaeal ether-based salinity indicators in mid-latitude Asian lakes23
Behaviour of chromium and chromium isotopes during estuarine mixing in the Beaulieu Estuary, UK23
Black Sea paleosalinity evolution since the last deglaciation reconstructed from alkenone-inferred Isochrysidales diversity23
Cosmogenic 10Be production records reveal dynamics of geomagnetic dipole moment (GDM) over the Laschamp excursion (20–60 ka)23
New cosmogenic nuclide burial-dating model indicates onset of major glaciations in the Alps during Middle Pleistocene Transition23
Deep learning for laboratory earthquake prediction and autoregressive forecasting of fault zone stress23
Three North African dust source areas and their geochemical fingerprint23
Co-seismic rupture of the 2021, M 7.4 Maduo earthquake (northern Tibet): Short-cutting of the Kunlun fault big bend23
Controls on the cadmium isotope composition of modern marine sediments23
Evidence for methane isotopic bond re-ordering in gas reservoirs sourcing cold seeps from the Sea of Marmara23
Morpho-tectonic control on the distribution of C3-C4 plants in the central Himalayan Siwaliks during Late Plio-Pleistocene23
On the petrogenesis of lunar troctolites: New insights into cumulate mantle overturn & mantle exposures in impact basins23
Evidence for a regional warm bias in the Early Cretaceous TEX86 record23
Detection of significant climatic precession variability in early Pleistocene glacial cycles23
The 2010 Haiti earthquake revisited: An acoustic intensity map from remote atmospheric infrasound observations23
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, Peru23
The role of inherited crustal and lithospheric architecture during the evolution of the Red Sea: Insights from three dimensional analogue experiments23
Predicting the proximity to macroscopic failure using local strain populations from dynamic in situ X-ray tomography triaxial compression experiments on rocks23
Isotopic fingerprinting of biogeochemical processes and iron sources in the iron-limited surface Southern Ocean23
Multicomponent diffusion of F, Cl and OH in apatite with application to magma ascent rates22
The 2019 Ridgecrest, California earthquake sequence: Evolution of seismic and aseismic slip on an orthogonal fault system22
Periodic oceanic euxinia and terrestrial fluxes linked to astronomical forcing during the Late Devonian Frasnian–Famennian mass extinction22
Polarity-reversal subduction zone initiation triggered by buoyant plateau obstruction22
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 InSAR22
The fate of fluvially-deposited organic carbon during transient floodplain storage22
Rock abundance and evolution of the shallow stratum on Chang'e-4 landing site unveiled by lunar penetrating radar data22
Westerly jet stream controlled climate change mode since the Last Glacial Maximum in the northern Qinghai-Tibet Plateau22
Calcium isotope constraints on OIB and MORB petrogenesis: The importance of melt mixing22
The evolution of lithium isotope signatures in fluids draining actively weathering hillslopes22
Flotation mechanism of sulphide melt on vapour bubbles in partially molten magmatic systems22
Carbonatites as a record of the carbon isotope composition of large igneous province outgassing22
Quantitative estimates of Holocene glacier meltwater variations on the Western Tibetan Plateau22
Layered crustal azimuthal anisotropy beneath the northeastern Tibetan Plateau revealed by Rayleigh-wave Eikonal tomography22
Thick, strong sediment subduction along south-central Chile and its role in great earthquakes22
Event-dominated transport, provenance, and burial of organic carbon in the Japan Trench22
Reversible scavenging traps hydrothermal iron in the deep ocean22
Reconstruction of the 2018 tsunamigenic flank collapse and eruptive activity at Anak Krakatau based on eyewitness reports, seismo-acoustic and satellite observations22
Centimeter-resolution topographic modeling and fine-scale analysis of craters and rocks at the Chang'E-4 landing site22
Into the deep and beyond: Carbon and nitrogen subduction recycling in secondary peridotites22
Enhanced water loss from the martian atmosphere during a regional-scale dust storm and implications for long-term water loss22
Pervasive low-velocity layer atop the 410-km discontinuity beneath the northwest Pacific subduction zone: Implications for rheology and geodynamics22
Lower-altitude of the Himalayas before the mid-Pliocene as constrained by hydrological and thermal conditions22
Rise and fall of the Acadian altiplano: Evidence for a Paleozoic orogenic plateau in New England21
Competition between preslip and deviatoric stress modulates precursors for laboratory earthquakes21
Linking surface deformation to thermal and mechanical magma chamber processes21
Copper-mineralised porphyries sample the evolution of a large-volume silicic magma reservoir from rapid assembly to solidification21
Subduction initiation and the rise of the Shillong Plateau21
Kinematics of the ∼1000 km Haiyuan fault system in northeastern Tibet from high-resolution Sentinel-1 InSAR velocities: Fault architecture, slip rates, and partitioning21
Evidence for crustal seismic anisotropy at the InSight lander site21
Controls on boron isotopes in a cold-water coral and the cost of resilience to ocean acidification21
On Archean craton growth and stabilisation: Insights from lithospheric resistivity structure of the Superior Province21
Glacial pumping of a magma-charged lithosphere: A model for glaciovolcanic causality in magmatic arcs21
A possible high-temperature origin of the Moon and its geochemical consequences21
Tsunami earthquakes: Vertical pop-up expulsion at the forefront of subduction megathrust21
Do sea level variations influence mid-ocean ridge magma supply? A test using crustal thickness and bathymetry data from the East Pacific Rise21
Thermal conductivity of Fe-bearing post-perovskite in the Earth's lowermost mantle21
Reappraisal of purported ca. 3.7 Ga stromatolites from the Isua Supracrustal Belt (West Greenland) from detailed chemical and structural analysis21
Transport properties of Fe-Ni-Si alloys at Earth's core conditions: Insight into the viability of thermal and compositional convection21
Seismic and geodetic progression of the 2018 summit caldera collapse of Kīlauea volcano21
Evolution of the early to late Archean mantle from Hf-Nd-Ce isotope systematics in basalts and komatiites from the Pilbara Craton21
The role of incremental magma chamber growth on ore formation in porphyry copper systems21
Widespread silicic and alkaline magmatism synchronous with the Deccan Traps flood basalts, India21
Hydrothermal alteration associated with the Chicxulub impact crater upper peak-ring breccias21
Assessing the potential capability of reconstructing glacial Atlantic water masses and AMOC using multiple proxies in CESM21
Molybdenum isotope systematics of lavas from the East Pacific Rise: Constraints on the source of enriched mid-ocean ridge basalt21
Long-term evolution of a plume-induced subduction in the Neotethys realm21
Disparities in oxygen isotopes of detrital and igneous zircon identify erosional bias in crustal rock record21
Using stable isotopes to distinguish atmospheric nitrate production and its contribution to the surface ocean across hemispheres21
Long-term Phanerozoic sea level change from solid Earth processes21
Combination of Δ47 and U-Pb dating in tectonic calcite veins unravel the last pulses related to the Pyrenean Shortening (Spain)21
Zinc- and cadmium-isotope evidence for redox-driven perturbations to global micronutrient cycles during Oceanic Anoxic Event 2 (Late Cretaceous)21
The temporal distribution of Earth's supermountains and their potential link to the rise of atmospheric oxygen and biological evolution21
Experimental stabilization of carbonate sediments to calcite: Insights into the depositional and diagenetic controls on calcite microcrystal texture21
Deglaciation of Pope Glacier implies widespread early Holocene ice sheet thinning in the Amundsen Sea sector of Antarctica20
Crack to pulse transition and magnitude statistics during earthquake cycles on a self-similar rough fault20
Fluid overpressure in subduction plate boundary caused by mantle-derived fluids20
Impact of power-law rheology on the viscoelastic relaxation pattern and afterslip distribution following the 2010 Mw 8.8 Maule earthquake20
The Ca and Mg isotope record of the Cryogenian Trezona carbon isotope excursion20
The coupled Hf-Nd isotope record of the early Earth in the Pilbara Craton20
Breakup with benefits - hydrothermal mineral systems related to the disintegration of a supercontinent20
Role of sulfate in the transport and enrichment of REE in hydrothermal systems20
Mercury isotope evidence for regional volcanism during the Frasnian-Famennian transition20
Coexisting diverse P–T–t paths during Neoarchean Sagduction: Insights from numerical modeling and applications to the eastern North China Craton20
Shear attenuation and anelastic mechanisms in the central Pacific upper mantle20
Late Ediacaran paleogeography of Avalonia and the Cambrian assembly of West Gondwana20
Seismic hazard of the western Makran subduction zone: Insight from mechanical modelling and inferred frictional properties20
Role of erosion in creating thrust recesses in a critical-taper wedge: An example from Eastern Tibet20
Cryogenian interglacial greenhouse driven by enhanced volcanism: Evidence from mercury records20
The phases of the Moon: Modelling crystallisation of the lunar magma ocean through equilibrium thermodynamics20
Southeastern margin of the Tibetan Plateau stopped expanding in the late Miocene20
Phyllosilicate controls on magnesium isotopic fractionation during weathering of granites: Implications for continental weathering and riverine system20
Miocene to present oceanographic variability in the Scotia Sea and Antarctic ice sheets dynamics: Insight from revised seismic-stratigraphy following IODP Expedition 38220
Major Early-Middle Devonian oceanic oxygenation linked to early land plant evolution detected using high-resolution U isotopes of marine limestones20
Aquifer deformation and active faulting in Salt Lake Valley, Utah, USA20
Island-wide variation in provenance of riverine sedimentary organic carbon: A case study from Taiwan20
Mountain building, mantle convection, and supercontinents: revisited20
Timescales of subduction initiation and evolution of subduction thermal regimes20
Indian continental lithosphere and related volcanism beneath Myanmar: Constraints from local earthquake tomography20
Local melt contamination and global climate impact: Dating the emplacement of Karoo LIP sills into organic-rich shale20
Evaluation of shallow-water carbonates as a seawater zinc isotope archive20
Mineral inclusions are not immutable: Evidence of post-entrapment thermally-induced shape change of quartz in garnet20
Shale and pyrite Re-Os ages from the Hornby Bay and Amundsen basins provide new chronological markers for Mesoproterozoic stratigraphic successions of northern Canada20
Covariation of cross-divide differences in denudation rate and χ: Implications for drainage basin reorganization in the Qilian Shan, northeast Tibet20
Asian monsoon evolution linked to Pacific temperature gradients since the Late Miocene19
Fault roughness controls sliding instability19
Onset of magma ocean solidification on Mars inferred from Mn-Cr chronometry19
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