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Lunar and Planetary

S. R. Taylor, Planetary Science A. PunarPerspective, Lunar and Planetary Institute, Houston, Tex., 1982. [Pg.102]

E. Zinner, S. Dnst, J. Chaumont, and J. C. Dran. Proceeding of the Ninth Lunar and Planetary Sciences Conference. 1978, p. 1667. [Pg.548]

Tombrello, T. A., Proc. Lunar and Planetary Sciences Conference X, Part 3, 1233 (1979). [Pg.80]

Klingelhofer, G. et al. 2008. The Advanced Miniaturised Mossbauer Spectrometer MIMOS lla Increased Sensitivity and New Capability for Elemental Analysis. Lunar and Planetary Science, 39, 2379. [Pg.302]

Schroder, C. et al. 2009. Santorini, Another Meteorite on Mars and Third of a Kind. Lunar and Planetary Science, 40, 1665. [Pg.302]

Alexander CMOD (2003) Making CAIs and chondrules from Cl dust in a canonical nebula. Lunar and Planetary Science Conference XXXIV 1391... [Pg.229]

Norman M, McCulloch M, O Neill H, Brandon A (2004) Magnesium isotopes in the Earth, Moon, Mars, and Pallasite parent body high precision analysis of olivine by laser ablation multi-collector ICPMS. Lunar and Planetary Science Conference XXXV 1447... [Pg.230]

Collins A (2000) Diam Rel Mater 9 417-423 Correcher V, Garcia-Guinea J (2001) J Luminescence 93 303-312 Cremers D, Wiens R, Arp Z, Harris R, Maurice S (2003) Lunar and Planetary Science XXXIV... [Pg.334]

Hugh W, Hubble H, Ghosh M, Sharma S, Horton K, Lucey P, Angel M, Wiens R (2002) Lunar and Planetary Science XXXIII Ishii T, Ogasava K, Tanaka A, Adachi H (1999) Materials Transactions, JIM 40 416-419... [Pg.338]

Seydoux-Guillaume AM, Wirth R, Nasdala L, Gottschalk M, Montel JM, Heinrich W (2002b) Phys Chem Minerals 29 240-253 Sharma S, Angel M, Ghosh M, Hubble H, Lucey P (2001) In Lunar and Planetary Science XXXII... [Pg.342]

Wiens R, Maurice S, Cremers D, Chevrees S (2003) Lunar and Planetary Science XXXIV 1646-1647... [Pg.344]

Warren, P. H. and Wasson, J. T. (1977) Pristine nonmare rocks and the nature of the lunar crust. Proceedings of the 8th Lunar and Planetary Science Conference, 2215—2235. [Pg.191]

McKeegan, K. D., Jarzebinski, G. J. et al. (2008) A first look at oxygen in a Genesis concentrator sample (abstr.). Lunar and Planetary Science XXXIX, CD 2020. [Pg.228]

Bottke, W. F., Nesvomy, D., Vokrouhlicky, D. and Borbidelli, A. (2009) The Gefion family as the probable source of the L chondrite meteorites (abstr.). Lunar and Planetary Science XL, CD 1445. [Pg.348]

Hoppe, R, Macdougall, D. and Lugmair, G. W. (2004) High spatial resolution ion microprobe measurements refine chronology of Orgueil carbonate formation (abstr.). Lunar and Planetary Science XXXV, CD 1313. [Pg.350]

Hutcheon, I. D., Krot, A. N. and Ulyanov, A. A. (2000)26A1 in anorthite-rich chondrules in primitive carbonaceous chondrites evidence chondrules postdate CAI (abstr.). Lunar and Planetary Science XXXI, CD 1869. [Pg.350]

Flynn, G. J. and Sutton, S. R. (1992) Trace elements in chondritic stratospheric particles zinc depletion as a possible indicator of atmospheric entry heating. Proceedings of the Lunar and Planetary Science Conference, 22, 171-184. [Pg.442]

Hartmann, W. K. et al., editors (1986) Origin of the Moon. Lunar and Planetary Institute. [Pg.480]

Sims, K.W.W., Newsom, H.E. and Gladney, E.S. (1990) Chemical fractionation during formation of the Earth s core and continental crust clues from As, Sb, W, and Mo, in Origin of the Earth (eds H.E. Newson and J.H. Jones), Oxford University Press, New York Lunar and Planetary Institute, Houston, pp. 291-317. [Pg.228]

Bradley, J. R, Keller, L.,Thomas,K. L., Vander Wood,T. B., and Brownlee, D. E. (1993). Carbon analyses of IDPs sectioned in sulfur and supported on beryllium films. In 24th Lunar and Planetary Sciences Conference, Blanchard, D., and Black, D., eds., Houston, TX, pp. 173-174. [Pg.772]

Kargel JS, Head JW III, Hogenboom DL, Khurana KK, Marion GM (2001) The system sulfuric acid-magnesium sulfate-water Europa s ocean properties related to thermal state. Lunar and Planetary Science Conference XXXII, Houston TX. Abstract 2138... [Pg.232]

Lane M (2004) Thermal emission spectroscopy of sulfates Possible hydrous iron-sulfate in the soil at the MER-A Gusev Crater Landing site. Lunar and Planetary Science Conference XXXV. Houston, TX. Abstract 1858... [Pg.234]

Socki RA, Gibson EK Jr, Lauriol B, Clark ID, Romanek CS, Golden DC (2002) Stable isotope enriched carbonates from the karst permafrost region of Northern Yukon, Canada a Mars analog. In Lunar and Planetary Science Conference XXXIII. Houston, TX. Abstract 1801... [Pg.243]

Kothari, B. K., Marti, K., Niemeyer, S., Regnier, S., Stephens, J. R. (1979) Noble gas trapping during condensation A laboratory study (abstract). In Lunar and Planetary Science, vol. X, pp. 682 1. Houston Lunar Planetary Institute. [Pg.264]

Figure 8. Plot of CaO against Na20 for the chondrule mesostases in Semarkona and Krymka. The diagonal line is a regression line through the data for mesostases which luminesce and the broken lines refer to 2 a uncertainties on the intercepts of this line. The dotted line refers to the theoretical line for plagioclase. (Reprinted by permission from Ref. 11. Copyright 1987 Lunar and Planetary Institute.)... Figure 8. Plot of CaO against Na20 for the chondrule mesostases in Semarkona and Krymka. The diagonal line is a regression line through the data for mesostases which luminesce and the broken lines refer to 2 a uncertainties on the intercepts of this line. The dotted line refers to the theoretical line for plagioclase. (Reprinted by permission from Ref. 11. Copyright 1987 Lunar and Planetary Institute.)...
Figure 13. The difference in 20 angle for the 131 and 131 reflections in the X-ray diffraction patterns for the plagioclase oligoclase (-1.5° for the ordered and -2.0° for the disordered phases) plotted against TL peak temperature for samples annealed at the temperatures (°C) and the times indicated. (Reprinted with permission from Ref. 21. Copyright 1987 Lunar and Planetary Institute.)... Figure 13. The difference in 20 angle for the 131 and 131 reflections in the X-ray diffraction patterns for the plagioclase oligoclase (-1.5° for the ordered and -2.0° for the disordered phases) plotted against TL peak temperature for samples annealed at the temperatures (°C) and the times indicated. (Reprinted with permission from Ref. 21. Copyright 1987 Lunar and Planetary Institute.)...
Mar chal, C.N., Albarede, F., and Emmanuel, N. (1997) Natural variations in copper and zinc isotopic compositions. In Seventh Annual V.M. Goldschmidt Conference, 131-132, LPI Contribution No. 921, Lunar and Planetary Institute Houston. [Pg.326]

Keller, L. P. Messenger, S. 2007, in Proceedings of the Chronology of Meteorites and the Early Solar System, Kauai, Hawaii, November 5-7, Lunar and Planetary Institute Contribution No. 1374, 88. [Pg.25]

See other pages where Lunar and Planetary is mentioned: [Pg.140]    [Pg.301]    [Pg.118]    [Pg.228]    [Pg.231]    [Pg.242]    [Pg.223]    [Pg.223]    [Pg.223]    [Pg.224]    [Pg.224]    [Pg.224]    [Pg.25]    [Pg.26]    [Pg.63]   


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