Fractionation frends among IVA iron meteorites: Constrast with IIIAB trends

Geochimica et Cosmochimica Acta

Volumn 65, Issue 6, 2001, Pages 951-970

  Wasson, J T ^a,b   Richardson, J W ^a  

^a UNIVERSITY OF CALIFORNIA   (United States)

^b UNIVERSITY OF CALIFORNIA   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

COOLING; FRACTIONATION; GEOCHEMISTRY; IRON METEORITE;

EID: 0035060427     PISSN: 00167037     EISSN: None     Source Type: Journal    
DOI: 10.1016/S0016-7037(00)00597-4     Document Type: Article

References (40)

1. Oxygen isotope studies of achondrites
2. Determination of the interdiffusion coefficients in the Fe-Ni and Fe-Ni-P systems below 900°C
3. Systematic compositional variations in the Cape York iron meteorite
4. Cooling rates of 27 iron and stony-iron meteorites
5. Asteroid core crystallization by inward dendritic growth
6. Thermal histories of IVA stony-iron and iron meteorites: Evidence for asteroid fragmentation and reaccretion
7. Damage from the impacts of small asteroids
8. Diffusion of nickel into iron
9. Experimental investigations of trace element fractionations in iron meteorites: II: The influence of sulfur
10. A nonmetal interaction model for the segregation of trace metals during solidification of Fe-Ni-S. Fe-Ni-P, and Fe-Ni-S-P alloys
11. Chemical fractionation in meteorites-IV. Abundances of fourteen trace elements in L-chondrites: Implications for cosmothermometry
12. 26Al in Semarkona ferromagnesian chondrules
13. Chemical analyses of thirty-eight iron meteorites
14. Chemical classification of iron meteorities-X. Multielement studies of 43 irons, resolution of group IIIE from IIIAB, and evaluation of Cu as a taxonomic parameter
15. Superior analyses of iron meteorites
16. Cooling rate variations of group IVA iron meteorites
17. Cooling rate of group IVA iron meteorites determined from a ternary Fe-Ni-P model
18. Trace element distribution between magnetic and non-magnetic portions of ordinary chondrites
19. The thermal evolution of IVA iron meteorites: Evidence from metallographic cooling rates
20. Phospohorus in meteoritic nickel-iron
21. Experimental studies of taenitee decomposition in ordinary Chondrites during continuous cooling (abstract)
22. Determination of the Fe-Ni and Fe-Ni-P phase diagram at low temperatures (700°C to 300°C)
23. Petrologic evidence for collisional heating of chondritic asteroids
24. An evaluation of the methods to determine the cooling rates of iron meteorites
25. The chemical classification of iron meteorites-VI. A reinvestigation of irons with Ge concentrations lower than 1 ppm
26. Chemical fractionation in iron meteorites and its interpretation
27. Geochemical relationships between some pallasites and iron meteorites
28. Core crystallization and silicate-metal mixing in the parent body of the IVA iron and stony-iron meteorites
29. Gallium, germanium, indium and iridium variations in a suite of L-group chondrites
30. Trapped melt in IIIAB irons; solid/liquid elemental partitioning during the fractionation of the IIIAB magma
31. Chemical classification of iron meteorites: XII. New members of the magmatic groups
32. Compositions of chondrites
33. Massive chromite in the Brenham pallasite and the fractionation of Cr during the crystallization of asteroidal cores
34. Composition and formation of metal nodules and veins in ordinary chondrules
35. Cooling rates of group IVA iron meteorites
36. A core origin for Group IVA iron meteorites: A reply to Moren and Goldstein
37. A new empirical cooling rate indicator for meteorites based on the size of the cloudy zone of the metallic phases