Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Langone A. [2]"'
Autor:
Spiess R.[1], Langone A.[2], Caggianelli A.[3], Stuart F.M.[4], Zucchi M.[3], Bianco C.[3], Brogi A.[3, Liotta D.[3
Publikováno v:
Journal of structural geology 155 (2022). doi:10.1016/j.jsg.2021.104498
info:cnr-pdr/source/autori:Spiess R.[1], Langone A.[2], Caggianelli A.[3], Stuart F.M.[4], Zucchi M.[3], Bianco C.[3], Brogi A.[3,5], Liotta D.[3,5]/titolo:Reply to Mazzarini et al. comment on 'Unveiling ductile deformation during fast exhumation of a granitic pluton in a transfer zone'/doi:10.1016%2Fj.jsg.2021.104498/rivista:Journal of structural geology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:155
info:cnr-pdr/source/autori:Spiess R.[1], Langone A.[2], Caggianelli A.[3], Stuart F.M.[4], Zucchi M.[3], Bianco C.[3], Brogi A.[3,5], Liotta D.[3,5]/titolo:Reply to Mazzarini et al. comment on 'Unveiling ductile deformation during fast exhumation of a granitic pluton in a transfer zone'/doi:10.1016%2Fj.jsg.2021.104498/rivista:Journal of structural geology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:155
In our reply we demonstrate the inconsistency of the comment we received from Mazzarini et al. Our data, models and conclusions are solid and framed in the regional evolution of the Northern Apennines, typified by eastward migration of coeval extensi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::09194aebc1b3c1c36214d39bbcca81b9
https://www.sciencedirect.com/journal/journal-of-structural-geology
https://www.sciencedirect.com/journal/journal-of-structural-geology
Autor:
Spiess R.[1], Langone A.[2], Caggianelli A.[3], Stuart F.M.[4], Zucchi M.[3], Bianco C.[3], Brogi A.[3, Liotta D.[3
Publikováno v:
Journal of structural geology 147 (2021): 1–24. doi:10.1016/j.jsg.2021.104326
info:cnr-pdr/source/autori:Spiess R.[1], Langone A.[2], Caggianelli A.[3], Stuart F.M.[4], Zucchi M.[3], Bianco C.[3], Brogi A.[3,5], Liotta D.[3,5]/titolo:Unveiling ductile deformation during fast exhumation of a granitic pluton in a transfer zone/doi:10.1016%2Fj.jsg.2021.104326/rivista:Journal of structural geology/anno:2021/pagina_da:1/pagina_a:24/intervallo_pagine:1–24/volume:147
info:cnr-pdr/source/autori:Spiess R.[1], Langone A.[2], Caggianelli A.[3], Stuart F.M.[4], Zucchi M.[3], Bianco C.[3], Brogi A.[3,5], Liotta D.[3,5]/titolo:Unveiling ductile deformation during fast exhumation of a granitic pluton in a transfer zone/doi:10.1016%2Fj.jsg.2021.104326/rivista:Journal of structural geology/anno:2021/pagina_da:1/pagina_a:24/intervallo_pagine:1–24/volume:147
Exhumation and cooling of upper crustal plutons is generally assumed to develop in the brittle domain, thus determining an abrupt passage from crystallization to faulting. To challenge this general statement, we have applied an integrated approach in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::77bf89a2c2ad38a4f07a1589a7eba5f3
https://doi.org/10.5194/egusphere-egu21-1316
https://doi.org/10.5194/egusphere-egu21-1316
Autor:
Corvò S.[1, Maino M.[1, Langone A.[2], Schenker F.L.[3], Piazolo S.[4], Casini L.[5], Seno S.[1
Publikováno v:
Lithos (Oslo. Print) 390-391 (2021): 1–25. doi:10.1016/j.lithos.2021.106126
info:cnr-pdr/source/autori:Corvò S.[1,2], Maino M.[1,2], Langone A.[2], Schenker F.L.[3], Piazolo S.[4], Casini L.[5], Seno S.[1,3]/titolo:Local variations of metamorphic record from compositionally heterogeneous rocks (Cima di Gagnone, Central Alps): Inferences on exhumation processes of (U)HP-HT rocks/doi:10.1016%2Fj.lithos.2021.106126/rivista:Lithos (Oslo. Print)/anno:2021/pagina_da:1/pagina_a:25/intervallo_pagine:1–25/volume:390-391
info:cnr-pdr/source/autori:Corvò S.[1,2], Maino M.[1,2], Langone A.[2], Schenker F.L.[3], Piazolo S.[4], Casini L.[5], Seno S.[1,3]/titolo:Local variations of metamorphic record from compositionally heterogeneous rocks (Cima di Gagnone, Central Alps): Inferences on exhumation processes of (U)HP-HT rocks/doi:10.1016%2Fj.lithos.2021.106126/rivista:Lithos (Oslo. Print)/anno:2021/pagina_da:1/pagina_a:25/intervallo_pagine:1–25/volume:390-391
The record of metamorphic conditions is commonly highly heterogeneous in spatially close rocks of different composition and rheology. The well-studied Cima di Gagnone area in the Central Alps represents such an example, as relatively small, 1– to 1
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4f8bce488539f23e5f25361240b26d11
http://www.cnr.it/prodotto/i/455988
http://www.cnr.it/prodotto/i/455988
Autor:
Carosi R.[1], Petroccia A.[1], Iaccarino S.[1], Simonetti M.[1], Langone A.[2], Montomoli C.[1
Publikováno v:
Geosciences, Vol 10, Iss 288, p 288 (2020)
Geosciences
Volume 10
Issue 8
Geosciences (Basel) 10 (2020): 1–29. doi:10.3390/geosciences10080288
info:cnr-pdr/source/autori:Carosi R.[1], Petroccia A.[1], Iaccarino S.[1], Simonetti M.[1], Langone A.[2], Montomoli C.[1,3]/titolo:Kinematics and timing constraints in a transpressive tectonic regime: The example of the posada-asinara shear zone (NE Sardinia, Italy)/doi:10.3390%2Fgeosciences10080288/rivista:Geosciences (Basel)/anno:2020/pagina_da:1/pagina_a:29/intervallo_pagine:1–29/volume:10
Geosciences
Volume 10
Issue 8
Geosciences (Basel) 10 (2020): 1–29. doi:10.3390/geosciences10080288
info:cnr-pdr/source/autori:Carosi R.[1], Petroccia A.[1], Iaccarino S.[1], Simonetti M.[1], Langone A.[2], Montomoli C.[1,3]/titolo:Kinematics and timing constraints in a transpressive tectonic regime: The example of the posada-asinara shear zone (NE Sardinia, Italy)/doi:10.3390%2Fgeosciences10080288/rivista:Geosciences (Basel)/anno:2020/pagina_da:1/pagina_a:29/intervallo_pagine:1–29/volume:10
Detailed geological field mapping, integrated with meso- and microstructural investigations, kinematic of the flow and finite strain analyses, combined with geochronology, are fundamental tools to obtain information on the temperature&ndash
defo
defo
Publikováno v:
Minerals (Basel) 10 (2020): 1–20.
info:cnr-pdr/source/autori:Ventruti G.[1], Caggianelli A. [1], Festa V. [1], Langone A.[2]/titolo:Crystal Chemistry of Barian Titanian Phlogopite from a Lamprophyre of the Gargano Promontory (Apulia, Southern Italy)./doi:/rivista:Minerals (Basel)/anno:2020/pagina_da:1/pagina_a:20/intervallo_pagine:1–20/volume:10
info:cnr-pdr/source/autori:Ventruti G.[1], Caggianelli A. [1], Festa V. [1], Langone A.[2]/titolo:Crystal Chemistry of Barian Titanian Phlogopite from a Lamprophyre of the Gargano Promontory (Apulia, Southern Italy)./doi:/rivista:Minerals (Basel)/anno:2020/pagina_da:1/pagina_a:20/intervallo_pagine:1–20/volume:10
This study is focused on a barian titanian phlogopite found in an alkaline ultramafic dyke transecting Mesozoic limestones of the Gargano Promontory (Apulia, Italy). The rock containing the barian titanian phlogopite, an olivine-clinopyroxene-rich la
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::c89537f2ed33351a86238c5a421da4ef
http://www.cnr.it/prodotto/i/431883
http://www.cnr.it/prodotto/i/431883
Autor:
Bonazzi M.[1, Langone A.[2], Tumiati S.[3], Dellarole E.[4], Mazzucchelli M.[2, Giovanardi T.[5], Zanetti A.[2]
Publikováno v:
Geosciences (Basel) 10 (2020): 1–31. doi:10.3390/geosciences10080281
info:cnr-pdr/source/autori:Bonazzi M.[1,2], Langone A.[2], Tumiati S.[3], Dellarole E.[4], Mazzucchelli M.[2,5], Giovanardi T.[5], Zanetti A.[2]/titolo:Mantle-derived corundum-bearing felsic dykes may survive only within the lower (Refractory%2Finert) crust: Evidence from zircon geochemistry and geochronology (Ivrea-Verbano zone, southern Alps, Italy)/doi:10.3390%2Fgeosciences10080281/rivista:Geosciences (Basel)/anno:2020/pagina_da:1/pagina_a:31/intervallo_pagine:1–31/volume:10
Geosciences, Vol 10, Iss 281, p 281 (2020)
Geosciences
Volume 10
Issue 8
info:cnr-pdr/source/autori:Bonazzi M.[1,2], Langone A.[2], Tumiati S.[3], Dellarole E.[4], Mazzucchelli M.[2,5], Giovanardi T.[5], Zanetti A.[2]/titolo:Mantle-derived corundum-bearing felsic dykes may survive only within the lower (Refractory%2Finert) crust: Evidence from zircon geochemistry and geochronology (Ivrea-Verbano zone, southern Alps, Italy)/doi:10.3390%2Fgeosciences10080281/rivista:Geosciences (Basel)/anno:2020/pagina_da:1/pagina_a:31/intervallo_pagine:1–31/volume:10
Geosciences, Vol 10, Iss 281, p 281 (2020)
Geosciences
Volume 10
Issue 8
Corundum-rich (up to 55 vol.%) felsic dykes formed with albite, ±
K-feldspar, ±
hercynite and ±
biotite-siderophyllite cut the lower crustal rocks exposed in the Ivrea&ndash
Verbano Zone (NW Italy). Zircon is an
K-feldspar, ±
hercynite and ±
biotite-siderophyllite cut the lower crustal rocks exposed in the Ivrea&ndash
Verbano Zone (NW Italy). Zircon is an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::76ff6c5b91c4100019cc29b0d0982bb9
http://www.cnr.it/prodotto/i/459606
http://www.cnr.it/prodotto/i/459606
Publikováno v:
Periodico di mineralogia (Testo stamp.) 88 (2019): 203–219. doi:10.2451/2019PM850
info:cnr-pdr/source/autori:Cruciani G.[1], Franceschelli M.[1], Langone A.[2], Puxeddu M.[3]/titolo:U-Pb zircon and Ar-Ar amphibole ages from Sardinian migmatites (Italy) and review of migmatite ages from the Variscan belt/doi:10.2451%2F2019PM850/rivista:Periodico di mineralogia (Testo stamp.)/anno:2019/pagina_da:203/pagina_a:219/intervallo_pagine:203–219/volume:88
info:cnr-pdr/source/autori:Cruciani G.[1], Franceschelli M.[1], Langone A.[2], Puxeddu M.[3]/titolo:U-Pb zircon and Ar-Ar amphibole ages from Sardinian migmatites (Italy) and review of migmatite ages from the Variscan belt/doi:10.2451%2F2019PM850/rivista:Periodico di mineralogia (Testo stamp.)/anno:2019/pagina_da:203/pagina_a:219/intervallo_pagine:203–219/volume:88
U-Pb zircon age determinations and Ar-Ar dating on biotite and amphibole were performed on amphibole-bearing migmatite of NE Sardinia Variscan chain. The mesosome zircons yielded a weighted average age of 461.3 ± 3.3 Ma (U-Pb concordant data). Leuco
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::199eb0a87b0e3d5e2760669aa62cb882
http://www.cnr.it/prodotto/i/407379
http://www.cnr.it/prodotto/i/407379
Publikováno v:
International journal of earth sciences (1999, Print) 103 (2014): 487–507. doi:10.1007/s00531-013-0971-8
info:cnr-pdr/source/autori:Fornelli A.[1], Langone A.[2], Micheletti F.[1], Pascazio A.[1], Piccarreta G.[1]/titolo:The role of trace element partitioning between garnet, zircon and orthopyroxene on the interpretation of zircon U-Pb ages: an example from high-.../doi:10.1007%2Fs00531-013-0971-8/rivista:International journal of earth sciences (1999, Print)/anno:2014/pagina_da:487/pagina_a:507/intervallo_pagine:487–507/volume:103
info:cnr-pdr/source/autori:Fornelli A.[1], Langone A.[2], Micheletti F.[1], Pascazio A.[1], Piccarreta G.[1]/titolo:The role of trace element partitioning between garnet, zircon and orthopyroxene on the interpretation of zircon U-Pb ages: an example from high-.../doi:10.1007%2Fs00531-013-0971-8/rivista:International journal of earth sciences (1999, Print)/anno:2014/pagina_da:487/pagina_a:507/intervallo_pagine:487–507/volume:103
The recognition of the coeval growth of zircon, orthopyroxene and garnet domains formed during the same metamorphic cycle has been attempted with detailed microanalyses coupled with textural analyses. A coronitic garnet-bearing granulite from the low
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::529f6d7b516396ac6fb0bfab2a7ff257
https://publications.cnr.it/doc/285997
https://publications.cnr.it/doc/285997
Publikováno v:
International journal of earth sciences (1999, Internet) 102 (2013): 1181–1202.
info:cnr-pdr/source/autori:Gretter N. [1], Ronchi A. [1], Langone A. [2], Perotti C. [1]/titolo:The transition between the two major Permian tectono-stratigraphic cycles in the central Southern Alps: results from facies analysis and U%2FPb geochronology./doi:/rivista:International journal of earth sciences (1999, Internet)/anno:2013/pagina_da:1181/pagina_a:1202/intervallo_pagine:1181–1202/volume:102
info:cnr-pdr/source/autori:Gretter N. [1], Ronchi A. [1], Langone A. [2], Perotti C. [1]/titolo:The transition between the two major Permian tectono-stratigraphic cycles in the central Southern Alps: results from facies analysis and U%2FPb geochronology./doi:/rivista:International journal of earth sciences (1999, Internet)/anno:2013/pagina_da:1181/pagina_a:1202/intervallo_pagine:1181–1202/volume:102
The Val Daone Conglomerate (VDC) is a continental clastic unit that crops out eastwards of the central Southern Alps, from the NE sector of the Collio Basin to the W as far as the Tione Basin to the E. This significant but as yet relatively unknown f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::64f57997e4265e13e58df2080d0c9367
http://www.cnr.it/prodotto/i/261432
http://www.cnr.it/prodotto/i/261432
Autor:
Boschi C. (1), Dallai L. (1), Dini A. (1), Baneschi I. (1), Langone A. (2), Cavallo A. (3), Ruggieri G. (4)
Publikováno v:
Goldschmidt 2012 Conference Abstracts, pp. 1494–1494, Montreal (Canada), 24-29 Giugno 2012
info:cnr-pdr/source/autori:Boschi C. (1), Dallai L. (1), Dini A. (1), Baneschi I. (1), Langone A. (2), Cavallo A. (3), Ruggieri G. (4),/congresso_nome:Goldschmidt 2012 Conference Abstracts/congresso_luogo:Montreal (Canada)/congresso_data:24-29 Giugno 2012/anno:2012/pagina_da:1494/pagina_a:1494/intervallo_pagine:1494–1494
info:cnr-pdr/source/autori:Boschi C. (1), Dallai L. (1), Dini A. (1), Baneschi I. (1), Langone A. (2), Cavallo A. (3), Ruggieri G. (4),/congresso_nome:Goldschmidt 2012 Conference Abstracts/congresso_luogo:Montreal (Canada)/congresso_data:24-29 Giugno 2012/anno:2012/pagina_da:1494/pagina_a:1494/intervallo_pagine:1494–1494
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::f2883b4d9d040431cbe1082b9b6c9f29
http://www.cnr.it/prodotto/i/224731
http://www.cnr.it/prodotto/i/224731