16 O enrichments in aluminum-rich chondrules from ordinary chondrites

[1]  N. Kita,et al.  A short duration of chondrule formation in the solar nebula: evidence from 26Al in Semarkona ferromagnesian chondrules , 2000 .

[2]  Y. Guan,et al.  Oxygen isotopes in calcium-aluminum-rich inclusions from enstatite chondrites: new evidence for a single CAI source in the solar nebula , 2000 .

[3]  K. McKeegan,et al.  Oxygen-Isotopic Compositions in Two Calcium-Aluminum-rich Inclusions from Unequilibrated Ordinary Chondrites , 2000 .

[4]  D. Ebel,et al.  Complexly zoned chromium‐aluminum spinel found in situ in the Allende meteorite , 2000 .

[5]  K. McKeegan,et al.  Oxygen Isotopes of CAIs from Unequilibrated Enstatite Chondrites: Characteristics and Implications , 2000 .

[6]  L. Leshin,et al.  Abundance of 26Al in Ferromagnesian Chondrules of Unequilibrated Ordinary Chondrites , 2000 .

[7]  J. Bridges,et al.  Mineralogical controls on the oxygen isotopic compositions of UOCs , 1999 .

[8]  J. Bridges,et al.  The Relative Effects of Mineralogy and Chondrule Size on Oxygen Isotopic Exchange in BO Xian (LL3.9) , 1999 .

[9]  Russell,et al.  Oxygen reservoirs in the early solar nebula inferred from an allende CAI , 1998, Science.

[10]  I. Lyon,et al.  Oxygen isotopes in forsterite grains from Julesburg and Allende: Oxygen‐16‐rich material in an ordinary chondrite , 1998 .

[11]  L. Leshin,et al.  Oxygen isotopic abundances in calcium- aluminum-rich inclusions from ordinary chondrites: implications for nebular heterogeneity. , 1998, Science.

[12]  L. Leshin,et al.  The oxygen isotopic composition of olivine and pyroxene from CI chondrites , 1997 .

[13]  G. Wasserburg,et al.  Evidence for Widespread 26Al in the Solar Nebula and Constraints for Nebula Time Scales , 1996, Science.

[14]  R. Clayton,et al.  Oxygen isotope studies of achondrites , 1996 .

[15]  R. Clayton,et al.  Experimental study of high temperature oxygen isotope exchange during chondrule formation , 1995 .

[16]  F. Ryerson,et al.  Determination of oxygen self-diffusion in åkermanite, anorthite, diopside, and spinel: Implications for oxygen isotopic anomalies and the thermal histories of Ca-Al-rich inclusions , 1994 .

[17]  R. Clayton Oxygen Isotopes in Meteorites , 2003 .

[18]  R. Clayton,et al.  Oxygen isotope studies of ordinary chondrites , 1991 .

[19]  G. Wasserburg,et al.  Origin of plagioclase-olivine inclusions in carbonaceous chondrites , 1991 .

[20]  W. Lanford,et al.  Oxygen diffusion in olivine: Effect of oxygen fugacity and implications for creep , 1989 .

[21]  R. Clayton High temperature isotope effects in the early solar system , 1986 .

[22]  H. Taylor,et al.  Stable isotopes in high temperature geological processes , 1986 .

[23]  R. Clayton,et al.  The oxygen isotope record in Murchison and other carbonaceous chondrites , 1984 .

[24]  R. Clayton,et al.  Oxygen isotopic compositions of chondrules in Allende and ordinary chondrites , 1983 .

[25]  R. Clayton,et al.  Genetic relations between iron and stony meteorites , 1978 .

[26]  R. Clayton,et al.  DISTRIBUTION OF THE PRE-SOLAR COMPONENT IN ALLENDE AND OTHER CARBONACEOUS CHONDRITES , 1977 .

[27]  J. Williamson,et al.  Least-squares fitting of a straight line , 1968 .

[28]  A. Albee,et al.  Empirical Correction Factors for the Electron Microanalysis of Silicates and Oxides , 1968, The Journal of Geology.