Zobrazeno 1 - 10
of 125
pro vyhledávání: '"L[, 4"'
Autor:
Turci F.[1, Avataneo C.[3], Botta S.[3], Marcelli I.[3], Barale L.[4], Tomatis M.[1, Cossio R.[5, Tallone S.[4], Compagnoni R.[5, Piana F.[4]
Publikováno v:
Environmental & engineering geoscience
26 (2020): 113–120. doi:10.2113/EEG-2272
info:cnr-pdr/source/autori:Turci F.[1,2], Avataneo C.[3], Botta S.[3], Marcelli I.[3], Barale L.[4], Tomatis M.[1,2], Cossio R.[5,2], Tallone S.[4], Compagnoni R.[5,2], Piana F.[4]/titolo:New Tools for the Evaluation of Asbestos-Related Risk during Excavation in an NOA-Rich Geological Setting/doi:10.2113%2FEEG-2272/rivista:Environmental & engineering geoscience (Print)/anno:2020/pagina_da:113/pagina_a:120/intervallo_pagine:113–120/volume:26
26 (2020): 113–120. doi:10.2113/EEG-2272
info:cnr-pdr/source/autori:Turci F.[1,2], Avataneo C.[3], Botta S.[3], Marcelli I.[3], Barale L.[4], Tomatis M.[1,2], Cossio R.[5,2], Tallone S.[4], Compagnoni R.[5,2], Piana F.[4]/titolo:New Tools for the Evaluation of Asbestos-Related Risk during Excavation in an NOA-Rich Geological Setting/doi:10.2113%2FEEG-2272/rivista:Environmental & engineering geoscience (Print)/anno:2020/pagina_da:113/pagina_a:120/intervallo_pagine:113–120/volume:26
The presence of naturally occurring asbestos (NOA) in many areas worldwide requires an enhanced geological risk evaluation to ensure workplace safety from asbestos during large construction projects. Due to the complexity of the geological risk defin
Autor:
Russo Ermolli E.[1], Masi A.[2, Vignola C.[2], Di Lorenzo H.[1], Masci L.[2], Bona F.[4], Forti L.[4, Lembo G.[6], Mazzini I.[7], Mecozzi B.[8], Muttillo B.[6], Pieruccini P.[9], Sardella R.[8], Sadori L.[2]
Publikováno v:
Review of palaeobotany and palynology 297 (2022). doi:10.1016/j.revpalbo.2021.104577
info:cnr-pdr/source/autori:Russo Ermolli E.[1], Masi A.[2,3], Vignola C.[2], Di Lorenzo H.[1], Masci L.[2], Bona F.[4], Forti L.[4,5], Lembo G.[6], Mazzini I.[7], Mecozzi B.[8], Muttillo B.[6], Pieruccini P.[9], Sardella R.[8], Sadori L.[2]/titolo:The pollen record from Grotta Romanelli (Apulia, Italy): New insight for the Late Pleistocene Mediterranean vegetation and plant use/doi:10.1016%2Fj.revpalbo.2021.104577/rivista:Review of palaeobotany and palynology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:297
info:cnr-pdr/source/autori:Russo Ermolli E.[1], Masi A.[2,3], Vignola C.[2], Di Lorenzo H.[1], Masci L.[2], Bona F.[4], Forti L.[4,5], Lembo G.[6], Mazzini I.[7], Mecozzi B.[8], Muttillo B.[6], Pieruccini P.[9], Sardella R.[8], Sadori L.[2]/titolo:The pollen record from Grotta Romanelli (Apulia, Italy): New insight for the Late Pleistocene Mediterranean vegetation and plant use/doi:10.1016%2Fj.revpalbo.2021.104577/rivista:Review of palaeobotany and palynology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:297
Pollen analyses have been carried out on the infilling deposits of Grotta Romanelli (Apulia, Italy), a reference site for the Middle and Upper Palaeolithic of Italy. The analysis focused on Terre rosse, a fine unit till now ascribed to an interstadia
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8fc671bec531855e2afc8d98dc0b060a
https://hdl.handle.net/11365/1223782
https://hdl.handle.net/11365/1223782
Autor:
Sanfilippo A.[1, Borghini G.[3], Guarnieri L.[4], Nakamura E.[5], Piccardo G.B.[4], Vannucci R.[1, Zanetti A.[2]
Publikováno v:
Chemical geology 588 (2022). doi:10.1016/j.chemgeo.2021.120643
info:cnr-pdr/source/autori:Sanfilippo A.[1,2], Borghini G.[3], Guarnieri L.[4], Nakamura E.[5], Piccardo G.B.[4], Vannucci R.[1,2], Zanetti A.[2]/titolo:A 400 Ma-long Nd-Hf isotopic evolution of melt-modified garnet-pyroxenites in an ancient subcontinental lithosphere (Lanzo North ophiolite, Western Alps)/doi:10.1016%2Fj.chemgeo.2021.120643/rivista:Chemical geology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:588
info:cnr-pdr/source/autori:Sanfilippo A.[1,2], Borghini G.[3], Guarnieri L.[4], Nakamura E.[5], Piccardo G.B.[4], Vannucci R.[1,2], Zanetti A.[2]/titolo:A 400 Ma-long Nd-Hf isotopic evolution of melt-modified garnet-pyroxenites in an ancient subcontinental lithosphere (Lanzo North ophiolite, Western Alps)/doi:10.1016%2Fj.chemgeo.2021.120643/rivista:Chemical geology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:588
Pyroxenite veining is widely preserved in peridotite massifs, and used to derive information on the origin and evolution of upper mantle domains. These lithospheric mantle sections can be isolated from the convecting mantle for >1 Ga or more, sufferi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8faa5c82d8caa39eaf9eff08ed64c5b0
https://publications.cnr.it/doc/462365
https://publications.cnr.it/doc/462365
Autor:
Calahorra,M.A., Defea,B., Foieri,A., Abud,G., Tolocka,P. , Ladux, J. ., Otero,L. , Haelterman,R., Roca, M.E., Paradell, S., Calahorra,M.A.1, Defea,B.2, Foieri,A.3, Abud,G., Tolocka,P. 4, Ladux, J. 1., Otero,L. 4, Haelterman,R.4, Roca, M.E.4, Paradell, S.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aac22bd8280ec677ade3ddbfad67fca9
Publikováno v:
Journal of petrology
62 (2021): 1–31. doi:10.1093/petrology/egab058
info:cnr-pdr/source/autori:Lustrino M.[1,2], Salari G.[1], Rahimzadeh B.[3], Fedele L.[4], Masoudi F.[3], Agostini S.[5]/titolo:Quaternary Melanephelinites and Melilitites from Nowbaran (NW Urumieh-Dokhtar Magmatic Arc, Iran): Origin of Ultrabasic-Ultracalcic Melts in a Post-Collisional Setting/doi:10.1093%2Fpetrology%2Fegab058/rivista:Journal of petrology (Print)/anno:2021/pagina_da:1/pagina_a:31/intervallo_pagine:1–31/volume:62
62 (2021): 1–31. doi:10.1093/petrology/egab058
info:cnr-pdr/source/autori:Lustrino M.[1,2], Salari G.[1], Rahimzadeh B.[3], Fedele L.[4], Masoudi F.[3], Agostini S.[5]/titolo:Quaternary Melanephelinites and Melilitites from Nowbaran (NW Urumieh-Dokhtar Magmatic Arc, Iran): Origin of Ultrabasic-Ultracalcic Melts in a Post-Collisional Setting/doi:10.1093%2Fpetrology%2Fegab058/rivista:Journal of petrology (Print)/anno:2021/pagina_da:1/pagina_a:31/intervallo_pagine:1–31/volume:62
The small Quaternary volcanic district of Nowbaran (NW Iran) belongs to the Urumieh-Dokhtar Magmatic Arc, a ~1800 km long NW-SE striking Cenozoic belt characterized by the irregular but abundant presence of subduction-related igneous products. Nowbar
Autor:
Maritan L.[1], Ganzarolli G.[2, Antonelli F.[4], Rigo M.[1, 2, 3, 4, Kapatza A.[6], Bajnok K.[7], Coletti C.[1], Mazzoli C.[1], Lazzarini L.[4], Vedovetto P.[3], Chavarría Arnau A.[3]
Publikováno v:
Journal of Archaeological Science
Journal of Archaeological Science, 2021, 129, pp.105358. ⟨10.1016/j.jas.2021.105358⟩
Journal of Archaeological Science, Elsevier, 2021, 129, pp.105358. ⟨10.1016/j.jas.2021.105358⟩
Journal of archaeological science 129 (2021): 1–13. doi:10.1016/j.jas.2021.105358
info:cnr-pdr/source/autori:Maritan L.[1], Ganzarolli G.[2,3], Antonelli F.[4], Rigo M.[1,2,3,4,5], Kapatza A.[6], Bajnok K.[7], Coletti C.[1], Mazzoli C.[1], Lazzarini L.[4], Vedovetto P.[3], Chavarría Arnau A.[3]/titolo:What kind of calcite? Disclosing the origin of sparry calcite temper in ancient ceramics/doi:10.1016%2Fj.jas.2021.105358/rivista:Journal of archaeological science/anno:2021/pagina_da:1/pagina_a:13/intervallo_pagine:1–13/volume:129
Journal of Archaeological Science, 2021, 129, pp.105358. ⟨10.1016/j.jas.2021.105358⟩
Journal of Archaeological Science, Elsevier, 2021, 129, pp.105358. ⟨10.1016/j.jas.2021.105358⟩
Journal of archaeological science 129 (2021): 1–13. doi:10.1016/j.jas.2021.105358
info:cnr-pdr/source/autori:Maritan L.[1], Ganzarolli G.[2,3], Antonelli F.[4], Rigo M.[1,2,3,4,5], Kapatza A.[6], Bajnok K.[7], Coletti C.[1], Mazzoli C.[1], Lazzarini L.[4], Vedovetto P.[3], Chavarría Arnau A.[3]/titolo:What kind of calcite? Disclosing the origin of sparry calcite temper in ancient ceramics/doi:10.1016%2Fj.jas.2021.105358/rivista:Journal of archaeological science/anno:2021/pagina_da:1/pagina_a:13/intervallo_pagine:1–13/volume:129
The addition of temper in the pottery manufacturing process is attested since Prehistoric Times and is still a production choice adopted in the ceramic industry. When the temper is composed of minerals and rocks which outcrop in regions distant from
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::29902a3c3dcc8f8612043333cc9f1c01
https://hal.science/hal-03601284
https://hal.science/hal-03601284
Autor:
Bonacina G.[1, Sanfilippo A.[1, Zana S.[1], Bosino A.[1], Massara E.P.[2], Viaggi P.[2], Sabato L.[4], Gallicchio S.[4], Scotti P.[2]
Publikováno v:
Ofioliti (Bologna) 46 (2021): 43–62. doi:10.4454/ofioliti.v46i1.537
info:cnr-pdr/source/autori:Bonacina G.[1,2], Sanfilippo A.[1,3], Zana S.[1], Bosino A.[1], Massara E.P.[2], Viaggi P.[2], Sabato L.[4], Gallicchio S.[4], Scotti P.[2]/titolo:Geochemical evidence for local variability in redox and depositional conditions in a deep-water Bonarelli equivalent section from Southern Tethys (Fontana Valloneto Section, Southern Italy)/doi:10.4454%2Fofioliti.v46i1.537/rivista:Ofioliti (Bologna)/anno:2021/pagina_da:43/pagina_a:62/intervallo_pagine:43–62/volume:46
info:cnr-pdr/source/autori:Bonacina G.[1,2], Sanfilippo A.[1,3], Zana S.[1], Bosino A.[1], Massara E.P.[2], Viaggi P.[2], Sabato L.[4], Gallicchio S.[4], Scotti P.[2]/titolo:Geochemical evidence for local variability in redox and depositional conditions in a deep-water Bonarelli equivalent section from Southern Tethys (Fontana Valloneto Section, Southern Italy)/doi:10.4454%2Fofioliti.v46i1.537/rivista:Ofioliti (Bologna)/anno:2021/pagina_da:43/pagina_a:62/intervallo_pagine:43–62/volume:46
Identifying the depositional redox conditions is useful to evaluate the interplay between climate changes, biological feedbacks and de-oxygenation processes in the oceans during the Oceanic Anoxic Events (OAEs). Here, we focus on the about 56 m-thick
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::8d06d0075db4ae8ff27937eb855d01ba
Autor:
Matera P.F.[1], Ventruti G.[1], Zucchi M.[1], Brogi A.[1, Capezzuoli E.[3], Liotta D.[1, Yu T.-L.[4, Shen C.-C.[4, Huntington K.W.[6], Rinyu L.[7], Kele S.[8]
Publikováno v:
Geofluids (Oxford. Online) 2021 (2021): 1–28. doi:10.1155/2021/8817487
info:cnr-pdr/source/autori:Matera P.F.[1], Ventruti G.[1], Zucchi M.[1], Brogi A.[1,2], Capezzuoli E.[3], Liotta D.[1,2], Yu T.-L.[4,5], Shen C.-C.[4,5], Huntington K.W.[6], Rinyu L.[7], Kele S.[8]/titolo:Geothermal Fluid Variation Recorded by Banded Ca-Carbonate Veins in a Fault-Related, Fissure Ridge-Type Travertine Depositional System (Iano, southern Tuscany, Italy)/doi:10.1155%2F2021%2F8817487/rivista:Geofluids (Oxford. Online)/anno:2021/pagina_da:1/pagina_a:28/intervallo_pagine:1–28/volume:2021
Geofluids, Vol 2021 (2021)
info:cnr-pdr/source/autori:Matera P.F.[1], Ventruti G.[1], Zucchi M.[1], Brogi A.[1,2], Capezzuoli E.[3], Liotta D.[1,2], Yu T.-L.[4,5], Shen C.-C.[4,5], Huntington K.W.[6], Rinyu L.[7], Kele S.[8]/titolo:Geothermal Fluid Variation Recorded by Banded Ca-Carbonate Veins in a Fault-Related, Fissure Ridge-Type Travertine Depositional System (Iano, southern Tuscany, Italy)/doi:10.1155%2F2021%2F8817487/rivista:Geofluids (Oxford. Online)/anno:2021/pagina_da:1/pagina_a:28/intervallo_pagine:1–28/volume:2021
Geofluids, Vol 2021 (2021)
Banded Ca-carbonate veins in travertine deposits are efficient recorders of the compositional fluctuations of geothermal fluids flowing (or flowed) from deep reservoirs up to the surface, within fault zones. In this view, these veins represent key to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::837b28161186819102f61aeb58b037e3
http://www.cnr.it/prodotto/i/446767
http://www.cnr.it/prodotto/i/446767
Autor:
Sigari D.[1, Mazzini I.[2], Conti J.[3, Forti L.[4, Lembo G.[5], Mecozzi B.[3, Muttillo B.[5], Sardella R.[3]
Publikováno v:
Antiquity 95 (2021): 1387–1404. doi:10.15184/aqy.2021.128
info:cnr-pdr/source/autori:Sigari D.[1,6], Mazzini I.[2], Conti J.[3,7], Forti L.[4,8], Lembo G.[5], Mecozzi B.[3,9], Muttillo B.[5], Sardella R.[3]/titolo:Birds and bovids: new parietal engravings at the Romanelli Cave, Apulia/doi:10.15184%2Faqy.2021.128/rivista:Antiquity/anno:2021/pagina_da:1387/pagina_a:1404/intervallo_pagine:1387–1404/volume:95
info:cnr-pdr/source/autori:Sigari D.[1,6], Mazzini I.[2], Conti J.[3,7], Forti L.[4,8], Lembo G.[5], Mecozzi B.[3,9], Muttillo B.[5], Sardella R.[3]/titolo:Birds and bovids: new parietal engravings at the Romanelli Cave, Apulia/doi:10.15184%2Faqy.2021.128/rivista:Antiquity/anno:2021/pagina_da:1387/pagina_a:1404/intervallo_pagine:1387–1404/volume:95
The Romanelli Cave in south-east Italy is an important reference point for the so-called ‘Mediterranean province’ of European Upper Palaeolithic art. Yet, the site has only recently been subject to a systematic investigation of its parietal and p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5c0769fd95b410956e420ed31963352b
http://hdl.handle.net/11392/2494755
http://hdl.handle.net/11392/2494755