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Accretion timescales and style of asteroidal differentiation in an
26
Al-poor protoplanetary disk
Kirsten Kolbjørn Larsen
*
,
Martin Schiller
,
Martin Bizzarro
*
Corresponding author for this work
34
Citations (Scopus)
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26
Al-poor protoplanetary disk'. Together they form a unique fingerprint.
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Earth & Environmental Sciences
planetesimal
100%
accretion
68%
timescale
52%
olivine
38%
isotope
31%
thermal evolution
24%
melting
23%
chondrite
22%
solar system
22%
meteorite
21%
pyroxene group
19%
silicate
17%
crystal
14%
ordinary chondrite
13%
heat production
13%
carbonaceous chondrite
13%
station
11%
fractional crystallization
11%
half life
10%
energy source
10%
source rock
9%
shell
8%
crust
7%
melt
7%
cooling
7%
loss
5%
material
4%
Chemical Compounds
Isotope
63%
Melting
47%
Fractional Crystallization
25%
Reaction Half Life
17%
Cooling
16%
Orbital
15%
Enthalpy
14%
Heat
13%
Energy
8%