Late accretion as a natural consequence of planetary growth

about

Evaporative fractionation of volatile stable isotopes and their bearing on the origin of the Moon Preservation of Earth-forming events in the tungsten isotopic composition of modern flood basalts.Dawn; the Vesta-HED connection; and the geologic context for eucrites, diogenites, and howardites

P2860

Q34025998-F4FC5DD9-D77B-4216-A2AA-E3B3E2E585A7 Q36016577-85213483-AB34-43B2-949C-F56C5C9A43F8 Q53963738-618DCB05-6ED2-4C3D-944D-78CA920FC106

P2860

Late accretion as a natural consequence of planetary growth

Item

http://www.wikidata.org/entity/Q58480970

description

im Juli 2012 veröffentlichter wissenschaftlicher Artikel

@de

wetenschappelijk artikel

@nl

наукова стаття, опублікована в липні 2012

@uk

name

Late accretion as a natural consequence of planetary growth

@en

Late accretion as a natural consequence of planetary growth

@nl

type

Item

label

Late accretion as a natural consequence of planetary growth

@en

Late accretion as a natural consequence of planetary growth

@nl

prefLabel

Late accretion as a natural consequence of planetary growth

@en

Late accretion as a natural consequence of planetary growth

@nl

P1476

Late accretion as a natural consequence of planetary growth

@en

P2093

Douglas Rumble III

http://www.w3.org/2001/XMLSchema#string

Liping Qin

http://www.w3.org/2001/XMLSchema#string

P2860

Chips off of Asteroid 4 Vesta: Evidence for the Parent Body of Basaltic Achondrite Meteorites

Late accretion on the earliest planetesimals revealed by the highly siderophile elements.

Hf-W-Th evidence for rapid growth of Mars and its status as a planetary embryo.

Volatile accretion history of the terrestrial planets and dynamic implications.

Highly siderophile element constraints on accretion and differentiation of the Earth-Moon system

Core formation and metal–silicate fractionation of osmium and iridium from gold

Evolution of the martian mantle inferred from the 187Re–187Os isotope and highly siderophile element abundance systematics of shergottite meteorites

Origin of felsic achondrites Graves Nunataks 06128 and 06129, and ultramafic brachinites and brachinite-like achondrites by partial melting of volatile-rich primitive parent bodies

Highly siderophile element composition of the Earth’s primitive upper mantle: Constraints from new data on peridotite massifs and xenoliths

Widespread magma oceans on asteroidal bodies in the early Solar System

P2888

ngeo1527

P304

614-617

http://www.w3.org/2001/XMLSchema#string

P31

scholarly article

P356

10.1038/NGEO1527

http://www.w3.org/2001/XMLSchema#string

P407

English

P433

http://www.w3.org/2001/XMLSchema#string

P478

http://www.w3.org/2001/XMLSchema#string

P50

Richard J. Walker

James M.D. Day

P577

2012-07-22T00:00:00Z

http://www.w3.org/2001/XMLSchema#dateTime

Late accretion as a natural consequence of planetary growth

about

P2860

P2860

Late accretion as a natural consequence of planetary growth

description

name

type

label

prefLabel

P1433

P1476

P2093

P2860

P2888

P304

P31

P356

P407

P433

P478

P50

P577

P356

P1433

P1476

P2093

P2860

P2888

P304

P31

P356

P407

P433

P478

P50

P577