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Clay mineral formation from mafic rocks in temperate climate, central Italy

TitoloClay mineral formation from mafic rocks in temperate climate, central Italy
Tipo di pubblicazioneArticolo su Rivista peer-reviewed
Anno di Pubblicazione1990
AutoriBini, C., Vaselli O., Coradossi N., Pancani M.G., and Angelone Massimo
RivistaSciences Geologiques - Bulletin
Volume43
Paginazione129-138
Parole chiaveclay mineral formation, Italy, mafic rock, ophiolite, soil mineralogy, temperate climate, Tuscany, Weathering
Abstract

Soils developed over ophiolitic rocks of Tuscany (central Italy) were investigated in order to assess if the soil properties are related to the different parent materials, and to document what genetic processes are taking place in the mild temperate climate. Differences in clay mineral composition were recorded in several weathering stages of the rocks and related soils (transformation of primary minerals, synthesis of new minerals in the soil-water system). As a consequence, an actual soil sequence is proposed for each lithological type investigated. -Authors
Note

cited By 2
URLhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-0025578114&partnerID=40&md5=a64f352b57f72817e3ff24addd360da2
Citation KeyBini1990129