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Elemental levels and relationships in the endemic serpentine flora of the Great Dyke, Zimbabwe and their significance as controlling factors for the floraBROOKS, R. R; XING-HUA YANG.Taxon. 1984, Vol 33, Num 3, pp 392-399, issn 0040-0262Article

SUELOS DE LA ZONA HUMEDA ESPANOLA. X: SUELOS SOBRE SERPENTINAS. II: OLIGOELEMENTOS Y RELACION CA/MG EN SUELOS Y VEGETACION = LES SOLS DE LA ZONE HUMIDE ESPAGNOLE. X: SOLS SUR SERPENTINE. II. OLIGOELEMENTS ET RAPPORT CA/MG DU SOL ET DE LA VEGETATIONLOPEZ LOPEZ MI; GUITIAN OJEA F.1981; AN. EDAFOL. AGROBIOL.; ISSN 0365-1797; ESP; DA. 1981; VOL. 40; NO 1-2; PP. 1-10; ABS. ENG; BIBL. 17 REF.Article

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An essay: the stimulus of unusual geologies for plant speciationKRUCKEBERG, A. R.Systematic botany. 1986, Vol 11, Num 3, pp 455-463, issn 0363-6445Article

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Raznovidnost serpentina so strukturoj, perekhodnoj ot lizardita k klinokhrizotilu kak porodoobrazuyushchij mineral v al'pinotipnykh giperbazitakhVARLAKOV, A. S.Doklady Akademii nauk SSSR. 1984, Vol 278, Num 1, pp 189-193, issn 0002-3264Article

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PLANT COMMUNITIES ON SERPENTINA IN SCOTLANDBIRSE EL.1982; VEGETATIO; ISSN 0042-3106; NLD; DA. 1982; VOL. 49; NO 3; PP. 141-162; BIBL. 36 REF.Article

Différence entre les propriétés d'adsorption de deux échantillons de chrysotile en relation avec la modification de leur état de surface consécutive à un broyage et/ou un lessivageSUQUET, H.Réunion annuelle des sciences de la terre. 1992, Num 14, issn 0249-7557, p.145Conference Paper