Gas-melt interactions and their bearing on chondrule formation

Meteoritics and Planetary Science

Volumn 37, Issue 10, 2002, Pages 1377-1389

  Tissandier, Laurent ^a   Libourel, Guy ^a   Robert, François ^a  

^a CRPG CNRS   (France)

Author keywords

[No Author keywords available]

Indexed keywords

CHONDRULE; CRYSTALLIZATION; FRACTIONATION; GAS; MELT; SOLAR SYSTEM;

EID: 0036806507     PISSN: 10869379     EISSN: None     Source Type: Journal    
DOI: 10.1111/j.1945-5100.2002.tb01035.x     Document Type: Article

References (43)

1. Recycling and volatile loss in chondrule formation
2. Iron isotopes in chondrules: Implications for the role of evaporation during chondrule formation
3. The lack of potassium-isotopic fractionation in Bishunpur chondrules
4. Constraints on the evolution of chondrules based on the moderately volatile elements sulfur, sodium, and potassium
5. Numerical models of the primitive solar nebula
6. Diffusion in silicate melts
7. Isotopic variations in the rock-forming elements in meteorites
8. Evaporation in the young solar nebula as the origin of 'just-right' melting of chondrules
9. The flash melting of chondrules: An experimental investigation into the melting history and physical nature of chondrule precursors
10. 4
11. Condensation in dust-enriched systems
12. Elemental and isotopic fractionations produced through evaporation of the Allende CV chondrite: Implications for the origin of HAL-type hibonite inclusions
13. The formation of chondrules at high gas pressures in the solar nebula
14. Mass-dependent isotopic fractionation of Mg in chondrules: An experimental study
15. Experimental constraints on alkali condensation in chondrule formation
16. Modeling magmatic systems: Petrologic applications
17. Properties of chondrules
18. Temperature conditions for chondrule formation
19. Do nebular fractionations, evaporative losses, or both, influence chondrule compositions?
20. Chondrules: Their diversity and the role of open-system processes during their formation
21. Chemical analyses of meteorites: A compilation of stony and iron meteorite analyses
22. Petrology and mineralogy of type II, FeO-rich chondrules in Semarkona (LL3.0): Origin by closed-system fractional crystallization, with evidence for supercooling
23. Petrology of FeO-poor, porphyritic pyroxene chondrules in the Semarkona chondrite
24. FeO-rich, porphyritic pyroxene chondrules in unequilibrated ordinary chondrites
25. Petrology and thermal history of type IA chondrules in the Semarkona (LL3.0) chondrite
26. Chemical fractionations in meteorites-I. Condensation of the elements
27. The effect of Na vapor on the Na content of chondrules
28. Systematics of calcium partitioning between olivine and silicate melt: Implications for melt structure and calcium content of magmatic olivines
29. Olivine-melt partition coefficients of chondrules and their bearing on chondrule formation processes
30. Thermoluminescence and compositional zoning in the mesostasis of a Semarkona group Al chondrule and new insights into the chondrule-forming process
31. Condensation during chondrule formation: Elemental and Mg isotopic evidence
32. Mg isotope variation in bulk meteorites and chondrules
33. 3
34. Chondrules and other components in C, O, and E chondrites: Similarities in their properties and origins
35. Open-system behaviour during chondrule formation
36. X-rays and fluctuating X-winds from protostars
37. 2 condensation experiments and implications for protosolar materials
38. Chondrule formation: Energetics and length scales
39. Mineral equilibrium in fractionated nebular systems
40. 2 liquids from cosmic gases
41. Sodium and sulfur in chondrules: Heating time and cooling curves
42. Mass fractionation of K isotopes in chondrule evaporation experiments