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Journal articles on the topic 'Italy Ivrea'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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1

Wasilewski, Peter, and Richard D. Warner. "Magnetic petrology of deep crustal rocks—Ivrea Zone, Italy." Earth and Planetary Science Letters 87, no. 3 (February 1988): 347–61. http://dx.doi.org/10.1016/0012-821x(88)90022-2.

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2

Pittarello, Lidia, Gerlinde Habler, Rainer Abart, and Dieter Rhede. "Garnet growth in frictional melts of the Ivrea Zone (Italy)." Italian Journal of Geosciences 134, no. 1 (February 2015): 149–61. http://dx.doi.org/10.3301/ijg.2014.53.

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3

Sinigoi, Silvano, James E. Quick, Adriano Mayer, and Gabriella Demarchi. "Density-controlled assimilation of underplated crust, Ivrea-Verbano zone, Italy." Earth and Planetary Science Letters 129, no. 1-4 (January 1995): 183–91. http://dx.doi.org/10.1016/0012-821x(94)00230-v.

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4

Pistone, Mattia, Othmar Müntener, Luca Ziberna, György Hetényi, and Alberto Zanetti. "Report on the ICDP workshop DIVE (Drilling the Ivrea–Verbano zonE)." Scientific Drilling 23 (November 30, 2017): 47–56. http://dx.doi.org/10.5194/sd-23-47-2017.

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Abstract. The Ivrea–Verbano Zone is the most complete, time-integrated crust–upper mantle archive in the world. It is a unique target for assembling data on the deep crust and the Moho transition zone and testing several hypotheses of formation, evolution, and modification of the continental crust through space and time across the Earth. The ICDP workshop Drilling the Ivrea–Verbano zonE (DIVE), held in Baveno, Italy, from 1 to 5 May 2017, focused on the scientific objectives and the technical aspects of drilling and sampling in the Ivrea–Verbano Zone at depth. A total of 47 participants from 9 countries with a wide variety of scientific and/or drilling expertise attended the meeting. Discussion on the proposed targets sharpened the main research lines and led to working groups and the necessary technical details to compile the full drilling proposal. The participants of the workshop concluded that four drilling operations in the Val Sesia and Val d'Ossola crustal sections represent the scientifically most promising solution to achieve the major goals within DIVE to unravel the physico-chemical properties and architecture of the lower continental crust towards the crust–mantle (Moho) transition zone.

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5

Kügle. "CODEX IVREA, BIBL. CAP. 115: A FRENCH SOURCE "MADE IN ITALY"." Revista de Musicología 13, no. 2 (1990): 527. http://dx.doi.org/10.2307/20795403.

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6

Obata, Masaaki, and Shun-ichiro Karato. "Ultramafic pseudotachylite from the Balmuccia peridotite, Ivrea-Verbano zone, northern Italy." Tectonophysics 242, no. 3-4 (February 1995): 313–28. http://dx.doi.org/10.1016/0040-1951(94)00228-2.

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7

Brodie, K. H., and E. H. Rutter. "Deep crustal extensional faulting in the Ivrea Zone of Northern Italy." Tectonophysics 140, no. 2-4 (September 1987): 193–212. http://dx.doi.org/10.1016/0040-1951(87)90229-0.

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8

Baker, A. J. "Stable isotopic constraints on fluidrock interactions in the Ivrea zone, Italy." Chemical Geology 71, no. 4 (December 1988): 365. http://dx.doi.org/10.1016/0009-2541(88)90061-7.

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9

Gianotti, Franco, Maria Gabriella Forno, Susan Ivy-Ochs, and Peter W. Kubik. "New chronological and stratigraphical data on the Ivrea amphitheatre (Piedmont, NW Italy)." Quaternary International 190, no. 1 (November 2008): 123–35. http://dx.doi.org/10.1016/j.quaint.2008.03.001.

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10

Pittarello, Lidia, Giorgio Pennacchioni, and Giulio Di Toro. "Amphibolite-facies pseudotachylytes in Premosello metagabbro and felsic mylonites (Ivrea Zone, Italy)." Tectonophysics 580 (December 2012): 43–57. http://dx.doi.org/10.1016/j.tecto.2012.08.001.

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11

BAKER, A. J. "Stable Isotopic Evidence for Fluid-Rock Interactions in the Ivrea Zone, Italy." Journal of Petrology 31, no. 1 (February 1, 1990): 243–60. http://dx.doi.org/10.1093/petrology/31.1.243.

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12

Alfani, Guido. "Wealth Inequalities and Population Dynamics in Early Modern Northern Italy." Journal of Interdisciplinary History 40, no. 4 (April 2010): 513–49. http://dx.doi.org/10.1162/jinh.2010.40.4.513.

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An analysis of the wealth and population of early modern Ivrea—based on the estimi, or property tax, records; the correzioni degli estimi, a continuous series of tax records rarely found elsewhere and hardly ever used before; the census of 1613, another unique and informative source; and other archival records—finds that the city's concentration and distribution of wealth was resilient even in face of acute demographical shocks (such as the plague of 1630) and that inequalities in property underwent a slow increase even in economically stagnant areas during the seventeenth century. The article places these findings in a European perspective, and it debates Jan van Zanden's hypothesis of a positive relationship between inequality in wealth and demographical/economic growth before the Industrial Revolution.

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13

Barboza, Scott A., and George W. Bergantz. "Dynamic model of dehydration melting motivated by a natural analogue: applications to the Ivrea–Verbano zone, northern Italy." Earth and Environmental Science Transactions of the Royal Society of Edinburgh 87, no. 1-2 (1996): 23–31. http://dx.doi.org/10.1017/s0263593300006441.

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ABSTRACT:Dehydration melting of crustal rocks may commonly occur in response to the intrusion of mafic magma in the mid- or lower crust. However, the relative importance of melt buoyancy, shear or dyking in melt generation and extraction under geologically relevant conditions is not well understood. A numerical model of the partial melting of a metapelite is presented and the model results are compared with the Ivrea-Verbano Zone in northern Italy. The numerical model uses the mixture theory approach to modelling simultaneous convection and phase change and includes special ramping and switching functions to accommodate the rheology of crystal-melt mixtures in accordance with the results of deformation experiments. The model explicitly includes both porous media flow and thermally and compositionally driven bulk convection of a restitecharged melt mass. A range of melt viscosity and critical melt fraction models is considered. General agreement was found between predicted positions of isopleths and those from the Ivrea-Verbano Zone. Maximum melt velocities in the region of porous flow are found to be 1 × 10−7 and 1 × 10−1m per year in the region of viscous flow. The results indicate that melt buoyancy alone may not be a sufficient agent for melt extraction and that extensive, vigorous convection of partially molten rocks above mafic bodies is unlikely, in accord with direct geological examples.

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14

Alfani, Guido. "The effects of plague on the distribution of property: Ivrea, Northern Italy 1630." Population Studies 64, no. 1 (March 2010): 61–75. http://dx.doi.org/10.1080/00324720903448712.

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15

BARBOZA, SCOTT A., and GEORGE W. BERGANTZ. "Metamorphism and Anatexis in the Mafic Complex Contact Aureole, Ivrea Zone, Northern Italy." Journal of Petrology 41, no. 8 (August 1, 2000): 1307–27. http://dx.doi.org/10.1093/petrology/41.8.1307.

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16

Kolodnyi, Anatolii M. "Chtristianity in its revelations and present problems (based on Ivan Ortynsky)." Ukrainian Religious Studies, no. 73 (January 13, 2015): 62–71. http://dx.doi.org/10.32420/2015.73.460.

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Ivan Ortinsky was born on January 20, 1922 in the village of Pogirtsi, Rudkivsky District. At the age of 17, having just got a certificate of maturity for a gymnasium, he departed from Lviv to Italy. Here in 1939-1943 young Ivan studied at the Salesian Small Seminary in Ivrea. In August 1942, in the city of Turin, he joined the novices of the Salesians fathers. Thanks to the good knowledge of different languages, in 1946 he was appointed guide in the catacombs of St. Kalista. In 1949-1963, Ortinsky served as coordinator of the catacombs excursion bureau.

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17

ALTENBERGER, U. "Local disequilibrium of plagioclase in high-temperature shear zones of the Ivrea Zone, Italy." Journal of Metamorphic Geology 13, no. 5 (September 1995): 553–58. http://dx.doi.org/10.1111/j.1525-1314.1995.tb00242.x.

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18

Kunz, Barbara E., Tim E. Johnson, Richard W. White, and Charlotte Redler. "Partial melting of metabasic rocks in Val Strona di Omegna, Ivrea Zone, northern Italy." Lithos 190-191 (March 2014): 1–12. http://dx.doi.org/10.1016/j.lithos.2013.11.015.

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19

Rutter, Ernest, Katharine Brodie, Tony James, and Luigi Burlini. "Large-scale folding in the upper part of the Ivrea-Verbano zone, NW Italy." Journal of Structural Geology 29, no. 1 (January 2007): 1–17. http://dx.doi.org/10.1016/j.jsg.2006.08.013.

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20

GARUTI, G. "Age, Geochemistry and Petrogenesis of the Ultramafic Pipes in the Ivrea Zone, NW Italy." Journal of Petrology 42, no. 2 (February 1, 2001): 433–57. http://dx.doi.org/10.1093/petrology/42.2.433.

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21

Quick, James E., Silvano Sinigoi, and Adriano Mayer. "Emplacement of mantle peridotite in the lower continental crust, Ivrea-Verbano zone, northwest Italy." Geology 23, no. 8 (1995): 739. http://dx.doi.org/10.1130/0091-7613(1995)023<0739:eompit>2.3.co;2.

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22

Lu, D. M. "Geochemistry of the Lower Crustal Mafic-Ultramafic Complex at Finero, Ivrea Zone, N. Italy." Mineralogical Magazine 58A, no. 2 (1994): 537–38. http://dx.doi.org/10.1180/minmag.1994.58a.2.17.

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23

Handy, M. R., L. Franz, F. Heller, B. Janott, and R. Zurbriggen. "Multistage accretion and exhumation of the continental crust (Ivrea crustal section, Italy and Switzerland)." Tectonics 18, no. 6 (December 1999): 1154–77. http://dx.doi.org/10.1029/1999tc900034.

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24

Brodie, K. H., E. H. Rutter, and D. Rex. "On the age of deep crustal extensional faulting in the Ivrea zone, northern Italy." Geological Society, London, Special Publications 45, no. 1 (1989): 203–10. http://dx.doi.org/10.1144/gsl.sp.1989.045.01.11.

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25

Voshage, H., J. C. Hunziker, A. W. Hofmann, and A. Zingg. "A Nd and Sr isotopic study of the Ivrea zone, Southern Alps, N-Italy." Contributions to Mineralogy and Petrology 97, no. 1 (September 1987): 31–42. http://dx.doi.org/10.1007/bf00375212.

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26

Rutter, E. H., and K. H. Brodie. "Some geophysical implications of the deformation and metamorphism of the Ivrea zone, northern Italy." Tectonophysics 182, no. 1-2 (October 1990): 147–60. http://dx.doi.org/10.1016/0040-1951(90)90347-b.

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27

Assumma, Bottero, and Monaco. "Landscape Economic Attractiveness: An Integrated Methodology for Exploring the Rural Landscapes in Piedmont (Italy)." Land 8, no. 7 (June 28, 2019): 105. http://dx.doi.org/10.3390/land8070105.

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The present paper focuses on an integrated evaluation methodology aimed at measuring the attractiveness of rural landscapes. The landscapes under observation are two exceptional contexts in Piedmont (Italy): The Moraine Amphitheatre of Ivrea and the vineyard landscape of Langhe, Roero and Monferrato, which have recently been included in the UNESCO World Heritage List. The proposed investigation tool consists of the use of a system of landscape indicators, from which a synthetic index called the landscape economic attractiveness index has been obtained, and the integration of the results in a dynamic model, considering the synthetic index as a factor of people mobility in a multi-pole system. This integrated approach aims at supporting the decision-making process in the definition and orientation of landscape and territorial transformation policies, respecting the landscape components.

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28

Förster, H. J., and D. E. Harlov. "Monazite-(Ce)-huttonite solid solutions in granulite-facies metabasites from the Ivrea-Verbano Zone, Italy." Mineralogical Magazine 63, no. 4 (August 1999): 587–94. http://dx.doi.org/10.1180/minmag.1999.063.4.11.

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AbstractComposite populations of monazite-group minerals of both metamorphic and metasomatic origin have been discovered in thin layers of granulite-facies metabasites interlayered with metapelites, located in the Val Strona di Omegna region of the Ivrea-Verbano Zone, Italy. In addition to monazite-(Ce), which is uncommonly poor in Th and is probably formed by incongruent dissolution of apatite, these populations include members of the monazite-huttonite series. The latter minerals contain between 13 and 30.1 mol.% ThSiO4 [= huttonitic monazite-(Ce)], and are known from only half a dozen other occurrences worldwide. We propose that breakdown of primary monazite-(Ce) in the metapelites during granulite-facies metamorphism mobilized Th and the REEs, which were then transported by high-grade metamorphic fluids into the metabasite layers to form the Th-rich minerals of the monazite-huttonite series.

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29

Gianotti, Franco. "Stratigraphical subdivision of the Middle Pleistocene glacigenic sequence of the Ivrea amphitheatre (Piedmont, NW Italy)." Quaternary International 279-280 (November 2012): 165. http://dx.doi.org/10.1016/j.quaint.2012.08.208.

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30

Hartmann, Gerald, and K. Hans Wedepohl. "The composition of peridotite tectonites from the Ivrea Complex, northern Italy: Residues from melt extraction." Geochimica et Cosmochimica Acta 57, no. 8 (April 1993): 1761–82. http://dx.doi.org/10.1016/0016-7037(93)90112-a.

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31

Mayer, Adriano, Klaus Mezger, and Silvano Sinigoi. "New Sm–Nd ages for the Ivrea–Verbano Zone, Sesia and Sessera valleys (Northern-Italy)." Journal of Geodynamics 30, no. 1-2 (February 2000): 147–66. http://dx.doi.org/10.1016/s0264-3707(99)00031-9.

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32

Oberti, Roberta, Massimo Boiocchi, Frank C. Hawthorne, Neil A. Ball, Fernando Cámara, Renato Pagano, and Adriana Pagano. "Ferro-ferri-hornblende from the Traversella mine (Ivrea, Italy): occurrence, mineral description and crystal-chemistry." Mineralogical Magazine 80, no. 7 (December 2016): 1233–42. http://dx.doi.org/10.1180/minmag.2016.080.060.

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AbstractFerro-ferri-hornblende is a new member of the amphibole supergroup (IMA-CNMNC 2015-054). It has been found in a rock specimen from the historical collection of Leandro De Magistris, which was collected at the Traversella mine (Val Chiusella, Ivrea, Piemonte, Italy). The specimen was catalogued as ‘speziaite', and contains a wide range of amphibole compositions from tremolite/actinolite to magnesio-hastingsite. The end-member formula of ferro-ferri-hornblende is A□BCa2c(Fe+Fe3+)T(Si7Al) O22W(OH)2 , which requires SiO2 43.41, Al2O3 5.26, FeO 29.66, Fe2O3 8.24 CaO 11.57, H2O 1.86, total 100.00 wt.%. The empirical formula derived from electron microprobe analysis and single-crystal structure refinement for the holotype crystal is A(Na0.10K0.13) Σ=0.23B(Ca 1.93Na0.07)Σ=2.00C(Mg1.16Fe2+3.21Mn0.O6Fe3+0.45 Al0.12Ti 0.01)Σ=5.01T(Si7.26Al0. 74)Σ=8.00 O22W(OH1.89F0.01C10.10)Σ=2.00- Ferro-ferri-hornblende is biaxial (-), with α = 1.697(2), P = 1 .722(5), γ = 1.726(5) and 2V (meas.) = 35.7(1.4)°, 2V (calc.) = 43.1°. The unit-cell parameters are a = 9.9307(5), b = 18.2232(10), c = 5.3190(3) Å, β = 104.857(1)°, V= 930.40 (9) Å3, Z= 2, space group C2/m. The a:b:c ratio is 0.545:1:0.292. The strongest eight reflections in the powder X-ray pattern [d values (in Å), I, (hkl)] are: 8.493, 100, (110); 2.728, 69, (151); 3.151, 47, (310); 2.555, 37, (); 2.615, 32, (061); 2.359, 28, (); 3.406, 26, (131); 2.180, 25, (261). Type material is deposited in the collections of the Museo di Mineralogia, Dipartimento di Scienze della Terra e dell'Ambiente, Università di Pavia, under the catalogue number 2015-01. Sample M/U15285 from the historical collection of Luigi Colomba, presently at the Museo Regionale di Scienze Naturali di Torino, was also checked, and the presence of ferro-ferri-hornblende was confirmed.

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33

Burlini, Luigi, and David M. Fountain. "Seismic anisotropy of metapelites from the Ivrea-Verbano zone and Serie dei Laghi (northern Italy)." Physics of the Earth and Planetary Interiors 78, no. 3-4 (July 1993): 301–17. http://dx.doi.org/10.1016/0031-9201(93)90162-3.

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34

Ferrsrio, A., and G. Garuti. "Platinum-group mineral inclusions in chromitites of the Finero mafic-ultramafic complex (Ivrea-Zone, Italy)." Mineralogy and Petrology 41, no. 2-4 (April 1990): 125–43. http://dx.doi.org/10.1007/bf01168491.

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35

Sinigoi, S., P. Antonini, G. Demarchi, A. Longinelli, M. Mazzucchelli, L. Negrini, and G. Rivalenti. "Intractions of mantle and crustal magmas in the southern part of the Ivrea Zone (Italy)." Contributions to Mineralogy and Petrology 108, no. 4 (October 1991): 385–95. http://dx.doi.org/10.1007/bf00303445.

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36

Garuti, Giorgio, Massimo Oddone, and José Torres-Ruiz. "Platinum-group-element distribution in subcontinental mantle: evidence from the Ivrea Zone (Italy) and the Betic – Rifean cordillera (Spain and Morocco)." Canadian Journal of Earth Sciences 34, no. 4 (April 1, 1997): 444–63. http://dx.doi.org/10.1139/e17-037.

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The six platinum-group elements (PGE's) Os, Ir, Ru, Rh, Pt, and Pd and Au were analyzed by instrumental neutron-activation analysis after nickel sulfide fire assay, in peridotites and dyke rocks from the orogenic ultramafic massifs of the Ivrea Zone in the Italian western Alps (Baldissero, Balmuccia, Finero) and the Betico–Rifean cordillera in southern Spain and northern Morocco (Ronda, Beni Bousera). The peridotites are considered as variably depleted, and reenriched low lithosphere, whereas the dyke rocks represent polybaric derivatives of basaltic melts (pyroxenites and gabbros), most coming from the underlying asthenosphere. The peridotites have total PGE content in the range 8.6–54.7 ppb, while mantle-normalized patterns generally grade from nearly flat and PGE rich, in less depleted lherzolites, to negative and PGE poor, in residual harzburgites and dunites. Dyke rocks have total PGE's in the range 5.4 – 250 ppb and positive mantle-normalized patterns. Negative anomalies of Ir – Pt are frequently observed in dykes, indicating that both metals were probably retained in the mantle source of these melts. Most of the peridotites display positive anomaly of Au, and in some case are enriched in Ru, Rh, and Pd, but exhibit the same negative anomalies in Ir and Pt as the dykes. These features are ascribed to reintroduction of noble metals into the residual mantle by reaction with the basaltic melts that generated the dykes, or alternatively by recycling of "dyke material" during further partial melting of the host mantle. The role of the sulfide phase as carrier of the recycled PGE is stressed by clear interelemental correlation in peridotites from the Ivrea Zone. Present data provide evidence that zones of PGE enrichment can origin; this way in the subcontinental mantle, and may constitute a potential reservoir for noble metal fertile volcanism in continental rift systems.

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37

Pros, Z., T. Lokajı́ček, R. Přikryl, and K. Klı́ma. "Direct measurement of 3D elastic anisotropy on rocks from the Ivrea zone (Southern Alps, NW Italy)." Tectonophysics 370, no. 1-4 (July 2003): 31–47. http://dx.doi.org/10.1016/s0040-1951(03)00176-8.

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38

Zhong, X., M. Frehner, K. Kunze, and A. S. Zappone. "A numerical and experimental investigation on seismic anisotropy of Finero peridotite, Ivrea-Verbano Zone, Northern Italy." IOP Conference Series: Materials Science and Engineering 82 (April 24, 2015): 012072. http://dx.doi.org/10.1088/1757-899x/82/1/012072.

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39

Baker, A. J. "Stable isotope evidence for limited fluid infiltration of deep crustal rocks from the Ivrea Zone, Italy." Geology 16, no. 6 (1988): 492. http://dx.doi.org/10.1130/0091-7613(1988)016<0492:sieflf>2.3.co;2.

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40

Magagnan, Alessandra, Mauro Palomba, Adriana Bovio, Elena Ferrero, Franco Gianotti, Marco Giardino, Lino Judica, Luigi Perotti, and Marco Davide Tonon. "GeoDidaLab: a laboratory for environmental education and research within the Ivrea Morainic Amphitheatre (Turin, NW Italy)." Rendiconti Online della Società Geologica Italiana 45 (July 2018): 68–76. http://dx.doi.org/10.3301/rol.2018.31.

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41

Rutter, Ernest H., Jalal Khazanehdari, Katharine H. Brodie, Derek J. Blundell, and David A. Waltham. "Synthetic seismic reflection profile through the Ivrea zone–Serie dei Laghi continental crustal section, northwestern Italy." Geology 27, no. 1 (1999): 79. http://dx.doi.org/10.1130/0091-7613(1999)027<0079:ssrptt>2.3.co;2.

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42

Quick, James E., Silvano Sinigoi, and Adriano Mayer. "Emplacement dynamics of a large mafic intrusion in the lower crust, Ivrea-Verbano Zone, northern Italy." Journal of Geophysical Research: Solid Earth 99, B11 (November 10, 1994): 21559–73. http://dx.doi.org/10.1029/94jb00113.

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43

Sinigoi, Silvano, James E. Quick, Diane Clemens-Knott, Adriano Mayer, Gabbriella Demarchi, Maurizio Mazzucchelli, Luisa Negrini, and Giorgio Rivalenti. "Chemical evolution of a large mafic intrusion in the lower crust, Ivrea-Verbano Zone, northern Italy." Journal of Geophysical Research: Solid Earth 99, B11 (November 10, 1994): 21575–90. http://dx.doi.org/10.1029/94jb00114.

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44

Rutter, E. H., K. H. Brodie, and P. J. Evans. "Structural geometry, lower crustal magmatic underplating and lithospheric stretching in the Ivrea-Verbano zone, northern Italy." Journal of Structural Geology 15, no. 3-5 (March 1993): 647–62. http://dx.doi.org/10.1016/0191-8141(93)90153-2.

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45

Altenberger, Uwe. "Stress-induced natural transformation of ortho- to clinohypersthene in metagabbros of the Ivrea Zone, Northern Italy." Mineralogy and Petrology 46, no. 1 (1992): 43–48. http://dx.doi.org/10.1007/bf01160700.

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46

Demarchi, Gabriella, James E. Quick, Silvano Sinigoi, and Adriano Mayer. "Pressure Gradient and Original Orientation of A Lower‐Crustal Intrusion in the Ivrea‐Verbano Zone, Northern Italy." Journal of Geology 106, no. 5 (September 1998): 609–22. http://dx.doi.org/10.1086/516045.

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47

KITAO, Yasunori. "A STUDY ON THE CONSERVATION METHOD FOR THE MODERN ARCHITECTURE BY THE DESIGN GUIDELINE IN IVREA, ITALY." Journal of Architecture and Planning (Transactions of AIJ) 79, no. 701 (2014): 1613–22. http://dx.doi.org/10.3130/aija.79.1613.

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48

Bigi, Simona, Maria Franca Brigatti, Maurizio Mazzuchelli, and Giorgio Rivalenti. "Crystal chemical variations in Ba-rich biotites from gabbroic rocks of lower crust (Ivrea Zone, NW Italy)." Contributions to Mineralogy and Petrology 113, no. 1 (January 1993): 87–99. http://dx.doi.org/10.1007/bf00320833.

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49

Abart, R., and R. Sperb. "Metasomatic coronas around hornblendite xenoliths in granulite facies marble, Ivrea zone, N Italy. II: Oxygen isotope patterns." Contributions to Mineralogy and Petrology 141, no. 4 (May 17, 2001): 494–504. http://dx.doi.org/10.1007/s004100100256.

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50

Qiu, Lin, Roberta L. Rudnick, William F. McDonough, and Fernando Bea. "The behavior of lithium in amphibolite- to granulite-facies rocks of the Ivrea–Verbano Zone, NW Italy." Chemical Geology 289, no. 1-2 (October 2011): 76–85. http://dx.doi.org/10.1016/j.chemgeo.2011.07.014.

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