Formation of ordinary chondrites

Reviews of Geophysics

Volumn 10, Issue 3, 1972, Pages 711-759

  Wasson, John T ^a  

^a NONE

Author keywords

[No Author keywords available]

Indexed keywords

EID: 84995026922     PISSN: 87551209     EISSN: 19449208     Source Type: Journal    
DOI: 10.1029/RG010i003p00711     Document Type: Review

References (111)

1. Fractionation of some abundant lithophile element ratios in chondrites
2. Physical properties of stony meteorites and their interpretation in the light of the hypothesis of the origin of meteorites (in Russian)
3. Origin, age, and composition of meteorites
4. Chemical processes in the early solar system, as inferred from meteorites
5. Meteorites and the early solar system
6. Fractionation and condensation in space
7. Fractionation of iron in the solar system
8. Structure and evolution of non‐carbonaceous chondritic meteorites
9. Cognate xenoliths in chondritic meteorites: Examples in Mezö‐Madaras and Ghubara
10. Thermodynamic properties of orthypyroxenes and clinopyroxenes based on the ideal two‐side model
11. The origin of meteorites and the constrained equilibrium condensation theory
12. Condensation of primordial dust
13. Surface conditions of the Orgueil meteorite parent body as indicated by mineral associations
14. Mineralogy and petrology of silicate inclusions in iron meteorites, Contrib
15. The accumulation of chondritic material
16. A new table of abundances of the elements in the solar system
17. Lost City, Oklahoma, meteorite: An introduction to its laboratory investigation and a comparison with Pribram and Ucera
18. Petrological and compositional relationships in meteorites
19. Particle sizes and compositions of unequilibrated ordinary chondrites (abstract)
20. Recrystallized chondrules in the Sharps (H‐3) chondrite
21. Metamorphism of ordinary chondrites
22. The petrology of chondrules in the Sharps meteorite
23. Schmus, Significance of the unequilibrated ordinary chondrites
24. A survey of the unequilibrated ordinary chondrites
25. Meteorite classes and radiation ages
26. Further evidence on the origin of trapped gases in the meteorite Khor Temiki
27. Gold and iridium in meteorites and some selected rocks
28. The early evolution of the sun
29. A study of solar evolution
30. The record in the meteorites, 3, On the development of meteorites in asteroidal bodies
31. Chondrules and the meteorite parent bodies
32. The light‐dark structure in the Pantar and Kapoeta stone meteorites
33. The LL group chondrites
34. Sharps chondrite—New evidence on the origin of chondrules and chondrites
35. Rubidium‐strontium age of amphoterite (LL) chondrites
36. Rubidium‐strontium studies on black hypersthene chondrites: Effects of shock and reheating
37. Fractionation of iron in the solar system
38. Cosmogenic and radiogenic helium, neon, and argon in amphoteric chondrites
39. The origin of hypersthene chondrites: Ages and shock effects of black chondrites
40. St. Mesmin, a gas‐rich amphoteric chondrite
41. Noble gases in unequilibrated ordinary chondrites
42. Radiogene, spallogene und primordiale Edelgase in Steinmeteoriten
43. Über die Isotopenzusammensetzung und über den Sitz der leichten Uredelgase in Steinmeteoriten
44. Preservation of the iodine‐xenon record in meteorites
45. Xenon‐iodine dating: Sharp isochronism in chondrites
46. Chemical analyses of ten stony meteorites
47. Chemical analyses of seven stony meteorites and one iron with silicate inclusions
48. Chemical analyses with notes on one mesosiderite and seven chondrites
49. 87 age of bronzite (H group) chondrites
50. Chemical fractionations in meteorites, 4, Abundances of 14 trace elements in L chondrites: Implications for cosmothermometry
51. Possible correlation between classifications and potassium‐argon ages of chondrites
52. The iron, magnesium, and calcium distribution in coexisting olivines and rhombic pyroxenes of chondrites
53. The Chainpur meteorite
54. Stony meteorite Krähenberg: Its chemical composition and the Rb‐Sr age of the light and dark portions
55. Low‐temperature minerals from the fine‐grained matrix of some carbonaceous meteorites
56. Distribution of magnesium and iron between orthopyroxene and calcic pyroxene in natural mineral assemblages
57. Mass loss from T Tauri stars
58. Formation of chondrules
59. Der Meteorit von Siena
60. Chemical fractionations in meteorites, 1, Condensation of the elements
61. Experimental studies on the system Fe‐MgO‐SiO2‐O2 and their bearing on the petrology of chondritic meteorites
62. Chemical fractionations in meteorities, 2, Abundance patterns and their interpretation
63. Chemical fractionations in meteorites, 3, Major element fractionations in chondrites
64. Trapped xenon and the classification of chondrites
65. Calcium‐aluminum rich phases in the Allende meteorite
66. Olivine composition in chondrites
67. Xenon and krypton in the Bruderheim meteorite
68. Total carbon content of ordinary chondrites
69. Phase equilibration and the crystallization of chondritic meteorites
70. Relationship between siderophilic‐element content and oxidation state of ordinary chondrites
71. Oxygen isotope cosmothermometer
72. Oxygen isotope temperatures of ‘equilibrated’; ordinary chondrites
73. Physical conditions in gaseous spheres
74. Dating of meteorites by the high‐temperature release of iodine‐correlated Xe129
75. I‐Xe‐dating: Evidence for cold assembly of an unequilibrated chondrite
76. On the genetic relationship and classification of meteorites
77. Early heat generation in meteorites
78. Chondrules and chondrites
79. Determination of an internal 87Rb‐87Sr isochron for the Olivenza chondrite
80. Assam: A gas‐rich hypersthene chondrite
81. Rare gases in the sun in the atmosphere, and in meteorites
82. Electrical heating of meteorite parent bodies and planets by dynamo induction from a pre‐main sequence T Tauri ‘solar wind
83. The melting of asteroidal‐sized bodies by unipolar dynamo induction from a primordial T Tauri sun
84. Chemical evidence bearing on the origin of the solar system
85. Metamorphosis and equilibrium in chondrites
86. On the origin of gas‐rich meteorites
87. Gallium, germanium, indium and iridium variations in a suite of L‐group chondrites
88. The origin of the moon and its relationship to the origin of the solar system
89. The composition of the stone meteorites and the origin of the meteorites
90. Polymict structure of the Mezö‐Madaras chondrite
91. Mineralogy and petrology of chondritic meteorites
92. Equilibration temperatures of iron and magnesium in chondritic meteorites
93. A chemieal‐petrologic classification for the chondritic meteorites
94. Composition of stony meteorites, 1, Analytical techniques
95. Major‐element composition of individual chondrules of the Bjurböle meteorite
96. Der Sonnenwind als Quelle der Uredelgase in Steinmeteoriten
97. Meteoritenalter und verwandte Probleme der Kosmochemie
98. Initial strontium for a chondrite and the determination of a metamorphism or formation interval
99. Chondrules: Suggestions concerning their origin
100. On regular discontinuities in the composition of meteorites
101. Über die Hell‐Dunkel‐Struktur der urgashaltigen Chondrite Breitscheid und Pantar
102. On the formation of chondrules and metal particles by 'shock melting
103. Metamorphism in chondrites
104. Origin of chondrules and chondrites
105. Chondrites: Their metallic minerals, thermal histories, and parent planes
106. Criticism of paper by H. E. Suess and H. Wanke, ‘Metamorphosis and equilibration in chondrites
107. Primordial argon and the metamorphism of chondrites
108. The chronology of the chondrites on the basis of noble‐gas analyses (in Russian)