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Comet dust as a source of amino acids at the Cretaceous/Tertiary boundary = De la poussière de comète en tant que source d'acides aminés à la limite Crétacé/TertiaireZAHNLE, K; GRINSPOON, D.Nature (London). 1990, Vol 348, Num 6297, pp 157-160, issn 0028-0836, 4 p.Article

Strontium-isotope anomaly in strangelove-oceanMULLER, D.W; HSU, K.J.International geological congress. 1992, p.1000Conference Paper

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Ni-rich spinel at the Cretaceous-Tertiary boundary of El Kef, TunisiaROBIN, E; ROCCHIA, R.Bulletin de la Société géologique de France. 1998, Vol 169, Num 3, pp 365-372, issn 0037-9409Article

Are periodicities in crater formations and mass extinctions related?YABUSHITA, S.Earth, moon and planets. 1994, Vol 64, Num 3, pp 207-216, issn 0167-9295Article

Mindset, standards and style in the mass extinction debatesGLEN, W.International geological congress. 1992, 2Vol, p. 66Conference Paper

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The history of the current impact/volcanism/mass-extinction debatesGLEN, W.International geological congress. 1992, 2Vol, p. 67Conference Paper

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K-T boundary scenario in IndiaPHANSALKAR, V. G.International geological congress. 1992, 2Vol, p. 67Conference Paper

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