Magnetic evidence for a partially differentiated carbonaceous chondrite parent body

Proceedings of the National Academy of Sciences of the United States of America

Volumn 108, Issue 16, 2011, Pages 6386-6389

  Carporzen, Laurent ^a,f   Weiss, Benjamin P ^a   Elkins Tanton, Linda T ^a   Shuster, David L ^b,c   Ebel, Denton ^d   Gattacceca, Jérôme ^e  

^a MASSACHUSETTS INSTITUTE OF TECHNOLOGY   (United States)

^b BERKELEY GEOCHRONOLOGY CENTER   (United States)

^c UNIVERSITY OF CALIFORNIA   (United States)

^d DIVISION OF INVERTEBRATE ZOOLOGY   (United States)

^e CNRS   (France)

^f INSTITUT DE PHYSIQUE DU GLOBE DE PARIS   (France)

Author keywords

Differentiation; Early solar system; Magnetic field; Paleointensity; Planetesimal

Indexed keywords

ALLENDE; ARTICLE; ASTRONOMY; MAGNETIC FIELD; MAGNETISM; MELTING POINT; PRIORITY JOURNAL; TEMPERATURE;

EID: 79955641172     PISSN: 00278424     EISSN: 10916490     Source Type: Journal    
DOI: 10.1073/pnas.1017165108     Document Type: Article

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