Zobrazeno 1 - 10
of 184
pro vyhledávání: '"H[, 1"'
Autor:
Hejazi, SMH (Hejazi, S. M. H. ) (1), Restaino, OF (Restaino, O. F. ) (2), Giosafatto, CVL (Giosafatto, C. V. L. ) (1), D'Ambrosio, S (D'Ambrosio, S. ) (2), Schiraldi, C (Schiraldi, C. ) (2), Zannini, D (Zannini, D. ) (3), Santagata, G (Santagata, G. ) (3), Porta, R (Porta, R. )
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3730::3a047b7eb3459d915428ea801ad687ef
http://hdl.handle.net/11588/893602
http://hdl.handle.net/11588/893602
Publikováno v:
Review of Palaeobotany and Palynology, 296, 1. Elsevier Saunders
Review of palaeobotany and palynology 296 (2022). doi:10.1016/j.revpalbo.2021.104544
info:cnr-pdr/source/autori:Nowak H.[1], Kustatscher E.[1,2,3], Roghi G.[4], Van Konijnenburg-van Cittert J.H.A.[5,6]/titolo:Variability of in situ spores in some leptosporangiate ferns from the Triassic in Italy and Austria/doi:10.1016%2Fj.revpalbo.2021.104544/rivista:Review of palaeobotany and palynology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:296
Review of palaeobotany and palynology 296 (2022). doi:10.1016/j.revpalbo.2021.104544
info:cnr-pdr/source/autori:Nowak H.[1], Kustatscher E.[1,2,3], Roghi G.[4], Van Konijnenburg-van Cittert J.H.A.[5,6]/titolo:Variability of in situ spores in some leptosporangiate ferns from the Triassic in Italy and Austria/doi:10.1016%2Fj.revpalbo.2021.104544/rivista:Review of palaeobotany and palynology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:296
Spores or pollen from a single species or even an individual plant or sporangium may vary in morphology and size to a point that equivalent forms found dispersed in the sediment have been described as different species or even genera. In addition, no
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e6d1eafbf8ae922e02f547a627ed5906
https://dspace.library.uu.nl/handle/1874/414240
https://dspace.library.uu.nl/handle/1874/414240
Autor:
Hummel H.[1, Kalle V.[1], Bienfait L.[1], Boyer Y.[3], Heurich M.[5], Svajda J.[6], Adamescu M.[7], Cazacu C.[7], Medina F.M.[8], Mork?n? R.[9], Razinkovas-Baziukas A.[9], Poursanidis D.[10], Tasevska O.[11], Al Malla A.[12], Stritih A.[13, 14], Rossi C.[15], Arenas-Castro S.[16], Carvalho-Santos C.[16, 17], Smit I.P.J.[18, 19], Valentini E.[20, 21], Xuan A.N.[21], Orenstein D.[22], Provenzale A.[23], de Wit R.[3], Hummel C.[1
Publikováno v:
Environmental and sustainability indicators, Amsterdam : Elsevier, 2022, vol. 14, art. no. 100179, p. 1-14
Environmental and Sustainability Indicators, 14
Environmental and Sustainability Indicators
Environmental and Sustainability Indicators, 2022, 14, ⟨10.1016/j.indic.2022.100179⟩
Environmental and sustainability indicators 14 (2022). doi:10.1016/j.indic.2022.100179
info:cnr-pdr/source/autori:Hummel H.[1,2], Kalle V.[1], Bienfait L.[1], Boyer Y.[3], Heurich M.[5], Svajda J.[6], Adamescu M.[7], Cazacu C.[7], Medina F.M.[8], Mork?n? R.[9], Razinkovas-Baziukas A.[9], Poursanidis D.[10], Tasevska O.[11], Al Malla A.[12], Stritih A.[13,14], Rossi C.[15], Arenas-Castro S.[16], Carvalho-Santos C.[16,17], Smit I.P.J.[18,19], Valentini E.[20,21], Xuan A.N.[21], Orenstein D.[22], Provenzale A.[23], de Wit R.[3], Hummel C.[1,4]/titolo:A bottom-up practitioner-derived set of Essential Variables for Protected Area management/doi:10.1016%2Fj.indic.2022.100179/rivista:Environmental and sustainability indicators/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:14
Environmental And Sustainability Indicators (2665-9727) (Elsevier), 2022-06, Vol. 14, P. 100179 (14p.)
Environmental and Sustainability Indicators, 14
Environmental and Sustainability Indicators
Environmental and Sustainability Indicators, 2022, 14, ⟨10.1016/j.indic.2022.100179⟩
Environmental and sustainability indicators 14 (2022). doi:10.1016/j.indic.2022.100179
info:cnr-pdr/source/autori:Hummel H.[1,2], Kalle V.[1], Bienfait L.[1], Boyer Y.[3], Heurich M.[5], Svajda J.[6], Adamescu M.[7], Cazacu C.[7], Medina F.M.[8], Mork?n? R.[9], Razinkovas-Baziukas A.[9], Poursanidis D.[10], Tasevska O.[11], Al Malla A.[12], Stritih A.[13,14], Rossi C.[15], Arenas-Castro S.[16], Carvalho-Santos C.[16,17], Smit I.P.J.[18,19], Valentini E.[20,21], Xuan A.N.[21], Orenstein D.[22], Provenzale A.[23], de Wit R.[3], Hummel C.[1,4]/titolo:A bottom-up practitioner-derived set of Essential Variables for Protected Area management/doi:10.1016%2Fj.indic.2022.100179/rivista:Environmental and sustainability indicators/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:14
Environmental And Sustainability Indicators (2665-9727) (Elsevier), 2022-06, Vol. 14, P. 100179 (14p.)
Assessing the environmental status of Protected Areas (PAs) is a challenging issue. To indicate that status, the identification of a common set of variables that are scientifically sound, and easy to assess and monitor by the PA practitioners, is par
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4e3407be444763b9e6bf94ecc2e62639
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:
Allen, S. (1, Frey, H. (1), Haeberli, W. (1), Huggel, C. (1), Chiarle, M. (3), Geertsema, M. (4)
Publikováno v:
Natural Hazard Science. Oxford: Oxford University Press, 2022
info:cnr-pdr/source/autori:Allen, S. (1, 2), Frey, H. (1), Haeberli, W. (1), Huggel, C. (1), Chiarle, M. (3), & Geertsema, M. (4)/titolo:Assessment Principles for Glacier and Permafrost Hazards in Mountain Regions/titolo_volume:Natural Hazard Science/curatori_volume:/editore: /anno:2022
info:cnr-pdr/source/autori:Allen, S. (1, 2), Frey, H. (1), Haeberli, W. (1), Huggel, C. (1), Chiarle, M. (3), & Geertsema, M. (4)/titolo:Assessment Principles for Glacier and Permafrost Hazards in Mountain Regions/titolo_volume:Natural Hazard Science/curatori_volume:/editore: /anno:2022
Glacier and permafrost hazards in cold mountain regions encompass various flood and mass movement processes that are strongly affected by rapid and cumulative climate-induced changes in the alpine cryosphere. These processes are characterized by a ra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e7c28eef1ffda32d0544500d31aeca7e
http://www.cnr.it/prodotto/i/463420
http://www.cnr.it/prodotto/i/463420
Autor:
Wu S.[1, Yang Y.[1, Jochum K.P.[3], Romer R.L.[4], Glodny J.[4], Savov I.P.[5], Agostini S.[6], De Hoog J.C.M.[7], Peters S.T.M.[8], Kronz A.[8], Zhang C.[9, 10], Bao Z.[9], Wang X.[9], Li Y.[1, Tang G.[1, Feng L.[1, Yu H.[11], Li Z.[11], Zhang L.[12], Lin J.[13], Zeng Y.[14], Xu C.[15], Wang Y.[15], Cui Z.[16], Deng L.[17], Xiao J.[17], Liu Y.[1, Xue D.[1, Zhang D.[1, Jia L.[1, Wang H.[1, Xu L.[1, Huang C.[1, Xie L.[1, Pack A.[8], Wörner G.[8], He M.[17], Li C.[1, Yuan H.[9], Huang F.[11], Li Q.[1, Yang J.[1, Li X.[1, Wu F.[1
Publikováno v:
Wu, S, Yang, Y, Jochum, K P, Romer, R L, Glodny, J, Savov, I P, Agostini, S, De Hoog, J C M, Peters, S T M, Kronz, A, Zhang, C, Bao, Z, Wang, X, Li, Y, Tang, G, Feng, L, Yu, H, Li, Z, Zhang, L, Lin, J, Zeng, Y, Xu, C, Wang, Y, Cui, Z, Deng, L, Xiao, J, Liu, Y, Xue, D, Zhang, D, Jia, L, Wang, H, Xu, L, Huang, C, Xie, L, Pack, A, Wörner, G, He, M, Li, C, Yuan, H, Huang, F, Li, Q, Yang, J, Li, X & Wu, F 2021, ' Isotopic Compositions (Li-B-Si-O-Mg-Sr-Nd-Hf-Pb) and Fe 2+ /ΣFe Ratios of Three Synthetic Andesite Glass Reference Materials (ARM-1, ARM-2, ARM-3) ', Geostandards and Geoanalytical Research . https://doi.org/10.1111/ggr.12399
Geostandards and geoanalytical research 45 (2021): 719–745. doi:10.1111/ggr.12399
info:cnr-pdr/source/autori:Wu S.[1,2], Yang Y.[1,2], Jochum K.P.[3], Romer R.L.[4], Glodny J.[4], Savov I.P.[5], Agostini S.[6], De Hoog J.C.M.[7], Peters S.T.M.[8], Kronz A.[8], Zhang C.[9,10], Bao Z.[9], Wang X.[9], Li Y.[1,2], Tang G.[1,2], Feng L.[1,2], Yu H.[11], Li Z.[11], Zhang L.[12], Lin J.[13], Zeng Y.[14], Xu C.[15], Wang Y.[15], Cui Z.[16], Deng L.[17], Xiao J.[17], Liu Y.[1,2], Xue D.[1,2], Zhang D.[1,2], Jia L.[1,2], Wang H.[1,2], Xu L.[1,2], Huang C.[1,2], Xie L.[1,2], Pack A.[8], Wörner G.[8], He M.[17], Li C.[1,2], Yuan H.[9], Huang F.[11], Li Q.[1,2], Yang J.[1,2], Li X.[1,2], Wu F.[1,2]/titolo:Isotopic Compositions (Li-B-Si-O-Mg-Sr-Nd-Hf-Pb) and Fe2+%2F?Fe Ratios of Three Synthetic Andesite Glass Reference Materials (ARM-1, ARM-2, ARM-3)/doi:10.1111%2Fggr.12399/rivista:Geostandards and geoanalytical research/anno:2021/pagina_da:719/pagina_a:745/intervallo_pagine:719–745/volume:45
Geostandards and Geoanalytical Research
Geostandards and geoanalytical research 45 (2021): 719–745. doi:10.1111/ggr.12399
info:cnr-pdr/source/autori:Wu S.[1,2], Yang Y.[1,2], Jochum K.P.[3], Romer R.L.[4], Glodny J.[4], Savov I.P.[5], Agostini S.[6], De Hoog J.C.M.[7], Peters S.T.M.[8], Kronz A.[8], Zhang C.[9,10], Bao Z.[9], Wang X.[9], Li Y.[1,2], Tang G.[1,2], Feng L.[1,2], Yu H.[11], Li Z.[11], Zhang L.[12], Lin J.[13], Zeng Y.[14], Xu C.[15], Wang Y.[15], Cui Z.[16], Deng L.[17], Xiao J.[17], Liu Y.[1,2], Xue D.[1,2], Zhang D.[1,2], Jia L.[1,2], Wang H.[1,2], Xu L.[1,2], Huang C.[1,2], Xie L.[1,2], Pack A.[8], Wörner G.[8], He M.[17], Li C.[1,2], Yuan H.[9], Huang F.[11], Li Q.[1,2], Yang J.[1,2], Li X.[1,2], Wu F.[1,2]/titolo:Isotopic Compositions (Li-B-Si-O-Mg-Sr-Nd-Hf-Pb) and Fe2+%2F?Fe Ratios of Three Synthetic Andesite Glass Reference Materials (ARM-1, ARM-2, ARM-3)/doi:10.1111%2Fggr.12399/rivista:Geostandards and geoanalytical research/anno:2021/pagina_da:719/pagina_a:745/intervallo_pagine:719–745/volume:45
Geostandards and Geoanalytical Research
To expand the newly developed ARM glasses as reference materials for in situ microanalysis of isotope ratios and iron oxidation state by a variety of techniques such as SIMS, LA-MC-ICP-MS and EPMA, we report Li-B-Si-O-Mg-Sr-Nd-Hf-Pb isotope data and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d26a1dd8431fc8a07dbd9bada1125c0e
https://hdl.handle.net/20.500.11820/23a47175-987d-4992-9c76-4a64ec67786e
https://hdl.handle.net/20.500.11820/23a47175-987d-4992-9c76-4a64ec67786e
Autor:
Yizhaq H.[1], Bel G.[1, Silvestro S.[3, Elperin T.[5], Kok J. F.[6], Cardinale, M.[7], Provenzale A.[8], Katra I. [9]
Publikováno v:
Earth and planetary science letters 512 (2019): 59–70. doi:10.1016/j.epsl.2019.01.025
info:cnr-pdr/source/autori:Yizhaq H.[1], Bel G.[1,2], Silvestro S.[3,4], Elperin T.[5], Kok J. F.[6], Cardinale, M.[7], Provenzale A.[8], Katra I. [9]/titolo:The origin of the transverse instability of aeolian megaripples/doi:10.1016%2Fj.epsl.2019.01.025/rivista:Earth and planetary science letters/anno:2019/pagina_da:59/pagina_a:70/intervallo_pagine:59–70/volume:512
info:cnr-pdr/source/autori:Yizhaq H.[1], Bel G.[1,2], Silvestro S.[3,4], Elperin T.[5], Kok J. F.[6], Cardinale, M.[7], Provenzale A.[8], Katra I. [9]/titolo:The origin of the transverse instability of aeolian megaripples/doi:10.1016%2Fj.epsl.2019.01.025/rivista:Earth and planetary science letters/anno:2019/pagina_da:59/pagina_a:70/intervallo_pagine:59–70/volume:512
Flat sand beds subjected to wind stress are unstable, and the wind action results in two types of aeolian sand ripples: normal ripples and megaripples. The distinction between the two types is based on two characteristics: i) the normal ripple patter
Publikováno v:
Renewable energy 177 (2021): 1102–1115. doi:10.1016/j.renene.2021.06.059
info:cnr-pdr/source/autori:Yu H.[1,2], Xu T.[1,2], Yuan Y.[1,2,3], Gherardi F.[1,4], Feng B.[1,2], Jiang Z. [1,2], Hu Z.[1,2]/titolo:Enhanced heat extraction for deep borehole heat exchanger through the jet grouting method using high thermal conductivity material/doi:10.1016%2Fj.renene.2021.06.059/rivista:Renewable energy/anno:2021/pagina_da:1102/pagina_a:1115/intervallo_pagine:1102–1115/volume:177
info:cnr-pdr/source/autori:Yu H.[1,2], Xu T.[1,2], Yuan Y.[1,2,3], Gherardi F.[1,4], Feng B.[1,2], Jiang Z. [1,2], Hu Z.[1,2]/titolo:Enhanced heat extraction for deep borehole heat exchanger through the jet grouting method using high thermal conductivity material/doi:10.1016%2Fj.renene.2021.06.059/rivista:Renewable energy/anno:2021/pagina_da:1102/pagina_a:1115/intervallo_pagine:1102–1115/volume:177
In this work, a novel enhanced deep borehole heat exchanger (EDBHE) was proposed to improve heat extraction efficiency based on the jet grouting method. By means of this technology, a soilcrete zone with high thermal conductivity was built near the w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::646e3ac1df22fe9e28f87fe00435ba20
Publikováno v:
Chemical geology 586 (2021): 1–20. doi:10.1016/j.chemgeo.2021.120506
info:cnr-pdr/source/autori:Sato H.[1], Ishikawa A.[2,3], Onoue T.[4], Tomimatsu Y.[4], Rigo M.[1,5]/titolo:Sedimentary record of Upper Triassic impact in the Lagonegro Basin, southern Italy: Insights from highly siderophile elements and Re-Os isotope stratigraphy across the Norian%2FRhaetian boundary/doi:10.1016%2Fj.chemgeo.2021.120506/rivista:Chemical geology/anno:2021/pagina_da:1/pagina_a:20/intervallo_pagine:1–20/volume:586
info:cnr-pdr/source/autori:Sato H.[1], Ishikawa A.[2,3], Onoue T.[4], Tomimatsu Y.[4], Rigo M.[1,5]/titolo:Sedimentary record of Upper Triassic impact in the Lagonegro Basin, southern Italy: Insights from highly siderophile elements and Re-Os isotope stratigraphy across the Norian%2FRhaetian boundary/doi:10.1016%2Fj.chemgeo.2021.120506/rivista:Chemical geology/anno:2021/pagina_da:1/pagina_a:20/intervallo_pagine:1–20/volume:586
The Norian and Rhaetian transition (Late Triassic) is characterized by a faunal turnover in major pelagic groups, such as radiolarians, conodonts, and ammonoids. Although catastrophic events such as emplacements of large igneous provinces and/or extr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fbcba7acea68232abc83bda3a764bba7
Autor:
Sunde Ø.[1], Friis H.[1], Andersen T.[2], Trumbull R.B.[3], Wiedenbeck M.[3], Lyckberg P.[4], Agostini S.[5], Casey W.H.[6, Yu P.[7]
Publikováno v:
Lithos (Oslo. Print) 352-353 (2020): 1–15. doi:10.1016/j.lithos.2019.105293
info:cnr-pdr/source/autori:Sunde Ø.[1], Friis H.[1], Andersen T.[2], Trumbull R.B.[3], Wiedenbeck M.[3], Lyckberg P.[4], Agostini S.[5], Casey W.H.[6,8], Yu P.[7]/titolo:Boron isotope composition of coexisting tourmaline and hambergite in alkaline and granitic pegmatites/doi:10.1016%2Fj.lithos.2019.105293/rivista:Lithos (Oslo. Print)/anno:2020/pagina_da:1/pagina_a:15/intervallo_pagine:1–15/volume:352-353
Lithos
info:cnr-pdr/source/autori:Sunde Ø.[1], Friis H.[1], Andersen T.[2], Trumbull R.B.[3], Wiedenbeck M.[3], Lyckberg P.[4], Agostini S.[5], Casey W.H.[6,8], Yu P.[7]/titolo:Boron isotope composition of coexisting tourmaline and hambergite in alkaline and granitic pegmatites/doi:10.1016%2Fj.lithos.2019.105293/rivista:Lithos (Oslo. Print)/anno:2020/pagina_da:1/pagina_a:15/intervallo_pagine:1–15/volume:352-353
Lithos
The boron isotopic composition of tourmaline and hambergite (Be2BO3[OH,F]) from peraluminous (n = 12), peralkaline (n = 1), and peralkaline nepheline syenite (n = 16) pegmatites has been measured by secondary ion mass spectrometry, for which a new ha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::73e1ff34d32337be1a6b6cf90b7a188d
https://escholarship.org/uc/item/21c0z4cz
https://escholarship.org/uc/item/21c0z4cz