Hf-W thermochronometry: Closure temperature and constraints on the accretion and cooling history of the H chondrite parent body

Earth and Planetary Science Letters

Volumn 270, Issue 1-2, 2008, Pages 106-118

  Kleine, Thorsten ^a   Touboul, Mathieu ^a   Van Orman, James A ^b   Bourdon, Bernard ^a   Maden, Colin ^a   Mezger, Klaus ^c   Halliday, Alex N ^d  

^a ETH ZURICH   (Switzerland)

^b CASE WESTERN RESERVE UNIVERSITY   (United States)

^c UNIVERSITY OF MÜNSTER   (Germany)

^d UNIVERSITY OF OXFORD   (United Kingdom)

Author keywords

chondrules; closure temperature; H chondrites; thermochronometry; W isotopes

Indexed keywords

COMPUTER SIMULATION; GEOCHRONOLOGY; ISOTOPES; PETROLOGY; SILICATES; TEMPERATURE;

METAL-SILICATE ISOCHRONS; SILICATE FRACTIONS; THERMOCHRONOMETRY;

GEOCHEMISTRY;

ACCRETION; CHONDRITE; CHONDRULE; HIGH TEMPERATURE; ISOTOPIC RATIO; LEAD-LEAD DATING; PARENT BODY; PETROLOGY; RUBIDIUM-STRONTIUM DATING; THERMOCHRONOLOGY;

ALLIUM CEPA;

EID: 43449110417     PISSN: 0012821X     EISSN: None     Source Type: Journal    
DOI: 10.1016/j.epsl.2008.03.013     Document Type: Article

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