Source:http://linkedlifedata.com/resource/pubmed/id/17809369
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Predicate | Object |
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rdf:type | |
lifeskim:mentions | |
pubmed:issue |
4417
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pubmed:dateCreated |
2010-6-8
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pubmed:abstractText |
Electron microprobe analyses of an extraordinarily large metal grain from the Murchison type 2 carbonaceous chondrite gave 0.24 mole percent silicon. Thermodynamic calculations show that this is a natural consequence of condensation of alloys from the solar nebular gas at a total pressure l0(-5) less, similar P(tot) < l0(-3) atmosphere, provided they failed to equilibrate with it after cooling to < 1200 kelvins.
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pubmed:language |
eng
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pubmed:journal | |
pubmed:status |
PubMed-not-MEDLINE
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pubmed:month |
Oct
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pubmed:issn |
0036-8075
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pubmed:author | |
pubmed:issnType |
Print
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pubmed:day |
26
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pubmed:volume |
206
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pubmed:owner |
NLM
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pubmed:authorsComplete |
Y
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pubmed:pagination |
449-51
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pubmed:year |
1979
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pubmed:articleTitle |
Silicon in carbonaceous chondrite metal: relic of high-temperature condensation.
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pubmed:publicationType |
Journal Article
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