19 results on '"Bloise, Andrea"'
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2. Characterization of Talcose Rocks Derived from Serpentinite—Pilot Study in the Ultramafic Complex of Cabo Ortegal (Spain) for Potential Use and Commercialization
3. Synthesis of Ni-Doped Tremolite Fibers to Help Clarify the Aetiology of the Cytotoxic Outcome of Asbestos
4. Anglesite, Cerussite, Gypsum, Langite, Malachite, and Posnjakite: New Occurrences in the Calabria Region (Southern Italy)
5. The Importance of Prevention When Working with Hazardous Materials in the Case of Serpentinite and Asbestos When Cleaning Monuments for Restoration
6. Hazardous Elements in Asbestos Tremolite from the Basilicata Region, Southern Italy: A First Step
7. Hydrothermal Alteration of Etna Ash and Implications for Mars
8. Provenance of White Marbles from the Roman City of Tauriana (Palmi, Reggio Calabria, Italy)
9. Mineralogical and Geochemical Characterization of Asbestiform Todorokite, Birnessite, and Ranciéite, and Their host Mn-Rich Deposits from Serra D’Aiello (Southern Italy)
10. Editorial for Special Issue “Mineral Fibres”
11. Assessment of Naturally Occurring Asbestos in the Area of Episcopia (Lucania, Southern Italy)
12. Multi-Analytical Approach for Asbestos Minerals and Their Non-Asbestiform Analogues: Inferences from Host Rock Textural Constraints
13. Archaeometric Approach for Studying Architectural Earthenwares from the Archaeological Site of S. Omobono (Rome-Italy)
14. Assessment of Serpentine Group Minerals in Soils: A Case Study from the Village of San Severino Lucano (Basilicata, Southern Italy)
15. The Effect of Grinding on Tremolite Asbestos and Anthophyllite Asbestos
16. Multi-Analytical Approach for Identifying Asbestos Minerals In Situ
17. Effect of Grinding on Chrysotile, Amosite and Crocidolite and Implications for Thermal Treatment
18. Non-Destructive Multi-Analytical Approach to Study the Pigments of Wall Painting Fragments Reused in Mortars from the Archaeological Site of Pompeii (Italy)
19. Thermal Stability of Woolly Erionite-K and Considerations about the Heat-Induced Behaviour of the Erionite Group
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