THE Hf-W ISOTOPIC SYSTEM AND THE ORIGIN OF THE EARTH AND MOON

Disk frequencies and lifetimes in Young clusters

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Origin of the Moon in a giant impact near the end of the Earth's formation

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Disk Frequencies and Lifetimes in Young Clusters

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Lead Isotopic Ages of Chondrules and Calcium-Aluminum-Rich Inclusions

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Rapid accretion and early core formation on asteroids and the terrestrial planets from Hf–W chronometry

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Oligarchic growth of protoplanets

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A short timescale for terrestrial planet formation from Hf–W chronometry of meteorites

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The origin of the Moon and the single-impact hypothesis III

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Early solar system timescales according to 53Mn-53Cr systematics

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Tungsten isotopes in mantle plumes: Heads it's positive, tails it's negative

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MARCO POLO: near earth object sample return mission

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A New Sample of Warm Extreme Debris Disks from the ALLWISE Catalog

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Why might planets and moons have early dynamos?

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Deep fractionation of Hf in a solidifying magma ocean and its implications for tungsten isotopic heterogeneities in the mantle

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What was the Volatile Composition of the Planetesimals that Formed the Earth?

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Spallation, cosmic rays, meteorites, and planetology

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Formation of secondary atmospheres on terrestrial planets by late disk accretion

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Anatomy of rocky planets formed by rapid pebble accretion

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Terrestrial Planet Formation: Dynamical Shake-up and the Low Mass of Mars

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The Origin and Earliest History of the Earth

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Earth and Mars – Distinct inner solar system products

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Earth and Terrestrial Planet Formation

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N-body simulations of oligarchic growth of Mars: Implications for Hf–W chronology

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Formation of Terrestrial Planets

Izidoro, A., & Raymond, S. N. (2018) · Springer eBooks · doi:10.1007/978-3-319-55333-7_142 · Cited by 30

Bulk chemical and Hf–W isotopic consequences of incomplete accretion during planet formation

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Geology of the Martian crustal dichotomy boundary: Age, modifications, and implications for modeling efforts

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Isotopes as clues to the origin and earliest differentiation history of the Earth

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Big returns on small samples: Lessons learned from the analysis of small lunar samples and implications for the future scientific exploration of the Moon

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The Isotopic Composition of the Elements

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Collision Chains among the Terrestrial Planets. III. Formation of the Moon

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Dynamical evolution of the Earth–Moon progenitors – Whence Theia?

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Not so rare Earth? New developments in understanding the origin of the Earth and Moon

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The Origin of the Earth - What's New?

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The composition of Solar system asteroids and Earth/Mars moons, and the Earth–Moon composition similarity

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A model for osmium isotopic evolution of metallic solids at the core‐mantle boundary

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Rayleigh-Taylor instability after giant impacts: Imperfect equilibration of the Hf-W system and its effect on the core formation age

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Kuiper Belt and Comets: An Observational Perspective

Jewitt, D. C. (2007) · Springer eBooks · doi:10.1007/978-3-540-71958-8_1 · Cited by 20

Analytical Developments for High-Precision Measurements of W Isotopes in Iron Meteorites

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Natural variations in the rhenium isotopic composition of meteorites

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The Composition and Major Reservoirs of the Earth Around the Time of the Moon-Forming Giant Impact

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Early Differentiation and Its Long‐Term Consequences for Earth Evolution

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Constraints on terrestrial planet formation timescales and equilibration processes in the Grand Tack scenario from Hf-W isotopic evolution

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Influence of rotation on the metal rain in a Hadean magma ocean

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Evolution of volatile species in the earth’s mantle: A view from xenology

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Inductively Coupled Plasma Mass Spectrometry

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The early thermal evolution of Mars

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Cosmogenic effects on Cu isotopes in IVB iron meteorites

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The Origin of the Natural Satellites

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Is the mantle chemically stratified? Insights from sound velocity modeling and isotope evolution of an early magma ocean

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Giant impacts stochastically change the internal pressures of terrestrial planets

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Hafnium-tungsten evolution with pebble accretion during Earth formation

Olson, P. L., & Sharp, Z. D. (2023) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2023.118418 · Cited by 14

Explaining mercury via a single giant impact is highly unlikely

Franco, P., Izidoro, A., Winter, O. C., Torres, K. D. S., & Amarante, A. (2022) · Monthly Notices of the Royal Astronomical Society · doi:10.1093/mnras/stac2183 · Cited by 19

A Chromatographic Method for Separation of Tungsten (W) from Silicate Samples for High-Precision Isotope Analysis Using Negative Thermal Ionization Mass Spectrometry

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Extinct isotope heterogeneities in the mantles of Earth and Mars: Implications for mantle stirring rates

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How well can Pb isotopes date core formation?

Kamber, B. S., & Kramers, J. D. (2006) · Nature · doi:10.1038/nature05359 · Cited by 13

Tungsten diffusion in olivine

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Water storage and early hydrous melting of the Martian mantle

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Early planetary processes and light elements in iron-dominated cores

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Does U–Pb date Earth's core formation?

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Resilient habitability of nearby exoplanet systems

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Timing of Martian Core Formation from Models of Hf–W Evolution Coupled with N-body SimulationsPreprint

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Crash Chronicles: Relative contribution from comets and carbonaceous asteroids to Earth’s volatile budget in the context of an Early Instability

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A new estimate for the age of highly-siderophile element retention in the lunar mantle from late accretion

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Tungsten isotope evolution during Earth's formation and new constraints on the viability of accretion simulations

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Formation of Super-Earths and Mini-Neptunes from Rings of Planetesimals

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Terrestrial planet formation in extra-solar planetary systems

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Evaluating the Microbial Habitability of Rogue Planets and Proposing Speculative Scenarios on How They Might Act as Vectors for Panspermia

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The initial solar system abundance of 60 Fe and early core formation of the first asteroids

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A Review of the Lunar 182Hf-182W Isotope System Research

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Earth's precession rate evolution and rapid fall during the Late Proterozoic

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Uranium partitioning between liquid iron and silicate melt at high pressures: implications for uranium solubility in planetary coresPreprint

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Formation of Terrestrial Planets

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Isotopic Geochronological Constraints on the Formation and Evolution of the Moon

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Pebble accretion and siderophile element partitioning between Earth's mantle and core

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The Formation of Mars and the Origin of Its Volcanic Provinces

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Diversity of exoplanets

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The Composition and Major Reservoirs of the Earth Around the Time of the Moon-Forming Giant Impact

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Accretion of volatile elements on Earth without the need of a late veneer

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Why Hadean?

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WITHDRAWN: The terrestrial magma ocean hypothesis

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Nucleon scattering analysis with a lane-consistent dispersive optical potential for Hf, W and Ta isotopes

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Isotopic constraints on the age of the Earth’s core: Mutual consistency of the Hf-W and U-Pb systems

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Origins of Planetary Systems: Constraints and Challenges

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High-precision tungsten isotopic measurement by negative thermal ionization mass spectrometry (NTIMS)

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Core Formation and Mantle Differentiation on Mars

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The Thermal Field of the Earth

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Formation of Terrestrial Planets

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Cosmic hydrogen and ice loss lines

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Formation of Mercury by a grazing giant collision involving similar-mass bodies

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Formation of the primordial sialic material of the Earth: Possible mechanisms and sources

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Origin of the Earth

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Isotope-geochemical constraints on the formation of the early Earth’ crust

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Terrestrial planetary dynamics: a view from U, Th geochemistryPreprint

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A novel method for high-precision tungsten isotope measurements on small-size samples

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A tungsten-182 and trace element perspective on the origin of the FOcal ZOne (FOZO) component

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Scattering Blanketing Effect of Earth’s Proto-atmosphere: Enhanced Suppression of Planetary Radiation and Magma Ocean Cooling

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Towards a Dynamical Model of Mars’ Evolution

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Validation of Advanced Kinematic Model of Earth-Moon System by Observed Length of Day Curve

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Lead isotope evolution during the multi-stage core formation

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Extinct Radionuclides and the Earliest Differentiation of the Earth and Moon

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The Southern polar giant impact hypothesis for the origin of the Martian dichotomy and the evolution of volcanism on mars

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Formation of Terrestrial Planets

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What was the Volatile Composition of the Planetesimals that Formed the Earth?

Nuth, J. A. (2007) · Springer eBooks · doi:10.1007/978-0-387-78419-9_60 · Cited by 1

Moon, Origin of

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Marco Polo: Hunting and Capture of Material from a Primitive Asteroid

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1. Stars, Galaxies, and the Origin of Chemical Elements

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Geochronology – Aims and reminiscences

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The timing of core formation in the terrestrial planets

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W-Hf isotope abundances and the early origin and evolution of the Earth-Moon system

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Terrestrial accretion rates and the origin of the Moon

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Hf-W Chronometry and Inner Solar System Accretion Rates

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Early evolution of the Earth and Moon: new constraints from Hf-W isotope geochemistry

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Early Moon formation inferred from hafnium–tungsten systematics

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