Oxygen isotopic composition of fulgurites from the Egyptian Sahara and other locations

Rapid Communications in Mass Spectrometry

Volumn 26, Issue 17, 2012, Pages 1980-1984

  Longinelli, Antonio ^a   Serra, Romano ^b   Sighinolfi, Giampaolo ^c   Selmo, Enricomaria ^a   Sgavetti, Maria ^a  

^a UNIVERSITY OF PARMA   (Italy)

^b UNIVERSITY OF BOLOGNA   (Italy)

^c UNIVERSITY OF MODENA AND REGGIO EMILIA   (Italy)

Author keywords

[No Author keywords available]

Indexed keywords

BROMINE COMPOUNDS; FRACTIONATION; GLASS; ISOTOPES; OXYGEN;

EARTH'S SURFACE; EGYPTIANS; FUSION PROCESS; HIGH-TEMPERATURE REACTION; ISOTOPIC FRACTIONATIONS; ISOTOPIC VALUES; LIGHTNING STRIKES; MELTING PROCESS; OXYGEN ISOTOPIC COMPOSITION; TARGET MATERIALS;

LIGHTNING;

EID: 84864773450     PISSN: 09514198     EISSN: 10970231     Source Type: Journal    
DOI: 10.1002/rcm.6315     Document Type: Article

References (5)

1. C. Ege,. What are fulgurites and where can they be found? 2005. Available:.
2. W.M. Myers, A.B. Peck,. A fulgurite from South Amboy, New Jersey, Am. Miner. 1925, 10, 152.
3. H. P. Taylor, Jr, S. Epstein,. Comparison of oxygen isotope analyses of tektites, soils, and impactite glasses, in Isotopic and Cosmic Chemistry, (Eds:, H. Craig, S. L. Miller, G. J. Wasserburg,), North-Holland Publishing Co., Amsterdam, 1964, p. 181.
4. I. Friedman, J. R. O'Neil,. Data of Geochemistry, Chapter KK. Compilation of stable isotope fractionation factors of geochemical interest. Geol. Survey Prof. Paper 440-KK, 1977.
5. 18O and chemical composition of Libyan Desert Glass, country rocks, and sands: New considerations on target material. Meteoritics Planet. Sci. 2011, 46, 218.