| Titolo | Clay mineral formation from mafic rocks in temperate climate, central Italy |
|---|---|
| Tipo di pubblicazione | Articolo su Rivista peer-reviewed |
| Anno di Pubblicazione | 1990 |
| Autori | Bini, C., Vaselli O., Coradossi N., Pancani M.G., and Angelone Massimo |
| Rivista | Sciences Geologiques - Bulletin |
| Volume | 43 |
| Paginazione | 129-138 |
| Parole chiave | clay 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 |
| URL | https://www.scopus.com/inward/record.uri?eid=2-s2.0-0025578114&partnerID=40&md5=a64f352b57f72817e3ff24addd360da2 |
| Citation Key | Bini1990129 |
