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Journal articles on the topic 'Sesia'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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1

Yan, Jingyan, Daoxin Liu, Pengfei Song, Shou Feng, Wangyan Li, and Ying Li. "Complete mitochondrial genome of Sesia siningensis (Lepidoptera: Sesiidae)." Mitochondrial DNA Part B 5, no. 1 (2019): 317–18. http://dx.doi.org/10.1080/23802359.2019.1703583.

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2

Riyaz, Muzafar, and Suhaib Firdous Yatoo. "First record of Sesia ommatiaeformis (Moore, 1891) (Lepidoptera: Sesiidae) from India." Polish Journal of Entomology 90, no. 2 - Ahead of print (2021): 103–5. http://dx.doi.org/10.5604/01.3001.0014.9179.

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Sesia ommatiaeformis was first scientifically described by Moore in 1891. The newly recorded S. ommatiaeformis along with the photographs of a living individual are presented which constitutes the first evidence of its occurrence in India from North-western Himalayas, Kashmir

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3

Regis, Daniele, Guido Venturini, and Martin Engi. "Geology of the Scalaro valley – Sesia Zone (Italian Western Alps)." Journal of Maps 12, no. 4 (2015): 621–29. http://dx.doi.org/10.1080/17445647.2015.1060182.

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4

Pognante, Ugo. "Lawsonite, blueschist and eclogite formation in the southern Sesia zone (western Alps, Italy)." European Journal of Mineralogy 1, no. 1 (1989): 89–104. http://dx.doi.org/10.1127/ejm/01/1/0089.

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5

Pognante, Ugo. "Tectonic implications of lawsonite formation in the Sesia zone (Western Alps)." Tectonophysics 162, no. 3-4 (1989): 219–27. http://dx.doi.org/10.1016/0040-1951(89)90245-x.

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6

Benincasa, E., M. F. Brigatti, L. Medici, and L. Poppi. "K-rich rectorite from kaolinized micaschist of the Sesia-Lanzo Zone, Italy." Clay Minerals 36, no. 3 (2001): 421–33. http://dx.doi.org/10.1180/000985501750539508.

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AbstractRectorite crystals [[4](Si6.81Al1.19)[6](Al3.26Ti0.04Fe0.553+Mg0.18Mn0.01)[12](Na0.02K0.88 Mg0.16Ca0.01)O20(OH)4·0.75H2O] found in micaschist of the Sesia-Lanzo Zone (NW Italy) were studied using a variety of techniques including microprobe analysis, infrared spectroscopy, single crystal and powder X-ray diffraction, atomic force microscopy and thermal analysis. Chemical data and exchangeable cation determination indicate that K+ is the dominant non-exchangeable interlayer cation, and thus is believed to occupy the mica interlayer site; Mg2+ together with small amounts of Ca2+, Na+ and

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7

Babist, J., M. R. Handy, M. Konrad-Schmolke, and K. Hammerschmidt. "Precollisional, multistage exhumation of subducted continental crust: The Sesia Zone, western Alps." Tectonics 25, no. 6 (2006): n/a. http://dx.doi.org/10.1029/2005tc001927.

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8

Avigad, Dov. "Pre-collisional ductile extension in the internal western Alps (Sesia zone, Italy)." Earth and Planetary Science Letters 137, no. 1-4 (1996): 175–88. http://dx.doi.org/10.1016/0012-821x(95)00223-y.

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9

Perotti, Carraro, Giardino, De Luca, and Lasagna. "Geodiversity Evaluation and Water Resources in the Sesia Val Grande UNESCO Geopark (Italy)." Water 11, no. 10 (2019): 2102. http://dx.doi.org/10.3390/w11102102.

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This paper aims at systemizing knowledge related to geodiversity assessment for water resources and its evaluation. The novel aspect connected to geodiversity of this paper is the analysis of the components of hydrological system, both at the superficial and underground level, in the territory of the Sesia Val Grande United Nations educational, scientific, and cultural organization (UNESCO) Global Geopark (Northwest Italy). More specifically, the research establishes a conceptual model and a specific procedure for the evaluation of geodiversity connected to water resources on a regional scale,

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10

Robyr, M., B. Darbellay, and L. P. Baumgartner. "Matrix-dependent garnet growth in polymetamorphic rocks of the Sesia zone, Italian Alps." Journal of Metamorphic Geology 32, no. 1 (2013): 3–24. http://dx.doi.org/10.1111/jmg.12055.

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11

Francke, W., V. Karalius, E. Plass, et al. "New Type of Sesiidae Sex Pheromone Identified from the Hornet Moth Sesia apiformis." Journal of Chemical Ecology 30, no. 4 (2004): 805–17. http://dx.doi.org/10.1023/b:joec.0000028433.67396.93.

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12

Arundell, J. C., and N. A. Straw. "HORNET CLEARWING MOTH (SESIA APIFORMIS [CLERCK]) AND DIEBACK OF POPLARS IN EASTERN ENGLAND." Arboricultural Journal 25, no. 3 (2001): 235–53. http://dx.doi.org/10.1080/03071375.2001.9747308.

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13

Tavazzani, L., S. Peres, S. Sinigoi, G. Demarchi, and G. Musumeci. "Structure and petrography of the Valle Mosso pluton, Sesia Magmatic System, Southern Alps." Journal of Maps 13, no. 2 (2017): 684–97. http://dx.doi.org/10.1080/17445647.2017.1354787.

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14

Giustetto, R., and R. Compagnoni. "An unusual occurrence of palygorskite from Montestrutto, Sesia-Lanzo zone, internal Western Alps (Italy)." Clay Minerals 46, no. 3 (2011): 371–85. http://dx.doi.org/10.1180/claymin.2011.046.3.371.

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AbstractAn unusual occurrence of palygorskite was found near Montestrutto, lower Val d'Aosta (Italy), within an eclogite-facies leucogneiss of the Sesia-Lanzo zone. Under the optical microscope the mineral appears as a felt of fibres hundreds of μm long and a few μm thick. SEM observation proved each filament to be a bundle of smaller but remarkably long fibres (length mostly 15–20 μm and thickness <1 μm). EDS and TGA showed a water content [zeolitic H2O ( ≅ 6%) + structural OH2 (≅8%) + framework OH (≅2%) ≅l6 wt.%] lower than average (≅20 wt.%). Structure refinement by the Rietveld method c

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15

Martín-García, J., H. Jactel, and J. J. Diez. "Patterns and monitoring of Sesia apiformis infestations in poplar plantations at different spatial scales." Journal of Applied Entomology 135, no. 5 (2011): 382–92. http://dx.doi.org/10.1111/j.1439-0418.2010.01562.x.

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16

Dal Piaz, Giorgio Vittorio. "La Zona Sesia-Lanzo e l'evoluzione tettonico-metamorfica delle Alpi nordoccidentali interne: quarant'anni dopo." Rendiconti Online della Società Geologica Italiana 37 (November 2015): 24–27. http://dx.doi.org/10.3301/rol.2015.167.

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17

Giuntoli, Francesco, Pierre Lanari, Marco Burn, Barbara Eva Kunz, and Martin Engi. "Deeply subducted continental fragments – Part 2: Insight from petrochronology in the central Sesia Zone (western Italian Alps)." Solid Earth 9, no. 1 (2018): 191–222. http://dx.doi.org/10.5194/se-9-191-2018.

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Abstract. Subducted continental terranes commonly comprise an assembly of subunits that reflect the different tectono-metamorphic histories they experienced in the subduction zone. Our challenge is to unravel how, when, and in which part of the subduction zone these subunits were juxtaposed. Petrochronology offers powerful tools to decipher pressure–temperature–time (P–T–t) histories of metamorphic rocks that preserve a record of several stages of transformation. A major issue is that the driving forces for re-equilibration at high pressure are not well understood. For example, continental gra

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18

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 (2000): 147–66. http://dx.doi.org/10.1016/s0264-3707(99)00031-9.

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19

Angiboust, Samuel, Johannes Glodny, Onno Oncken, and Christian Chopin. "In search of transient subduction interfaces in the Dent Blanche–Sesia Tectonic System (W. Alps)." Lithos 205 (September 2014): 298–321. http://dx.doi.org/10.1016/j.lithos.2014.07.001.

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20

Delleani, Francesco, M. Iole Spalla, Daniele Castelli, and Guido Gosso. "A new petro-structural map of the Monte Mucrone metagranitoids (Sesia-Lanzo Zone, Western Alps)." Journal of Maps 9, no. 3 (2013): 410–24. http://dx.doi.org/10.1080/17445647.2013.800004.

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21

Manzotti, Paola, Michel Ballèvre, Michele Zucali, Martin Robyr, and Martin Engi. "The tectonometamorphic evolution of the Sesia–Dent Blanche nappes (internal Western Alps): review and synthesis." Swiss Journal of Geosciences 107, no. 2-3 (2014): 309–36. http://dx.doi.org/10.1007/s00015-014-0172-x.

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22

Inger, S., W. Ramsbotham, R. A. Cliff, and D. C. Rex. "Metamorphic evolution of the Sesia-Lanzo Zone, Western Alps: time constraints from multi-system geochronology." Contributions to Mineralogy and Petrology 126, no. 1-2 (1996): 152–68. http://dx.doi.org/10.1007/s004100050241.

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23

Buatier, M., H. L. M. van Roermund, M. R. Drury, and J. M. Lardeaux. "Deformation and recrystallization mechanisms in naturally deformed omphacites from the Sesia-Lanzo zone; geophysical consequences." Tectonophysics 195, no. 1 (1991): 11–27. http://dx.doi.org/10.1016/0040-1951(91)90141-e.

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24

Bąkowski, Marek, Rafał Celadyn, Marek Hołowiński, and Witold Zajda. "Clearwing moths (Lepidoptera: Sesiidae) of Małopolska Province." Polish Journal of Entomology / Polskie Pismo Entomologiczne 80, no. 2 (2011): 411–21. http://dx.doi.org/10.2478/v10200-011-0028-x.

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Clearwing moths (Lepidoptera: Sesiidae) of Małopolska Province Twenty-four species of the family Sesiidae have been recorded from the Province of Małopolska. This constitutes ca 78% of all the species of this family present in Poland. The species Paranthrene insolita, Synanthedon mesiaeformis, S. flaviventris, S. conopiformis, Chamaesphecia tenthrediniformis have been recorded for the first time in this region. Sesia bembeciformis and Synanthedon cephiformis have been recorded as new for the Pieniny Mts. The majority of adults were attracted with the use of synthetic sex pheromones.

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25

Rebay, Gisella, and Maria Iole Spalla. "Emplacement at granulite facies conditions of the Sesia–Lanzo metagabbros: an early record of Permian rifting?" Lithos 58, no. 3-4 (2001): 85–104. http://dx.doi.org/10.1016/s0024-4937(01)00046-9.

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26

KONRAD-SCHMOLKE, MATTHIAS, JOCHEN BABIST, MARK R. HANDY, and PATRICK J. O'BRIEN. "The Physico-Chemical Properties of a Subducted Slab from Garnet Zonation Patterns (Sesia Zone, Western Alps)." Journal of Petrology 47, no. 11 (2006): 2123–48. http://dx.doi.org/10.1093/petrology/egl039.

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27

Giuntoli, Francesco, and Martin Engi. "Internal geometry of the central Sesia Zone (Aosta Valley, Italy): HP tectonic assembly of continental slices." Swiss Journal of Geosciences 109, no. 3 (2016): 445–71. http://dx.doi.org/10.1007/s00015-016-0225-4.

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28

Koons, P. O. "Relative geobarometry from high-pressure rocks of quartzofeldspathic composition from the Sesia Zone, Western Alps, Italy." Contributions to Mineralogy and Petrology 93, no. 3 (1986): 322–34. http://dx.doi.org/10.1007/bf00389391.

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29

FRÜH-GREEN, G. L. "Interdependence of deformation, fluid infiltration and reaction progress recorded in eclogitic metagranitoids (Sesia Zone, Western Alps)." Journal of Metamorphic Geology 12, no. 3 (1994): 327–43. http://dx.doi.org/10.1111/j.1525-1314.1994.tb00026.x.

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30

Guo, W. W., H. Xia, G. De Roeck, and K. Liu. "Integral model for train-track-bridge interaction on the Sesia viaduct: Dynamic simulation and critical assessment." Computers & Structures 112-113 (December 2012): 205–16. http://dx.doi.org/10.1016/j.compstruc.2012.09.001.

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31

Lu, Gang, Maria Giuditta Fellin, Wilfried Winkler, et al. "Revealing exhumation of the central Alps during the Early Oligocene by detrital zircon U–Pb age and fission-track double dating in the Taveyannaz Formation." International Journal of Earth Sciences 109, no. 7 (2020): 2425–46. http://dx.doi.org/10.1007/s00531-020-01910-z.

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Abstract The late Eocene-to-early Oligocene Taveyannaz Formation is a turbidite series deposited in the Northern Alpine Foreland Basin (close to the Alpine orogenic front). Double dating of zircons with the fission-track and the U–Pb methods is applied on samples from the Taveyannaz Formation to reconstruct the exhumation history of the Central-Western Alps and to understand the syn-collisional magmatism along the Periadriatic lineament. Three samples from this unit show similar detrital zircon fission-track age populations that center at: 33–40 Ma (20%); 69–92 Ma (30–40%); and 138–239 Ma (40–

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32

Rebay, G., and B. Messiga. "Prograde metamorphic evolution and development of chloritoid-bearing eclogitic assemblages in subcontinental metagabbro (Sesia–Lanzo zone, Italy)." Lithos 98, no. 1-4 (2007): 275–91. http://dx.doi.org/10.1016/j.lithos.2007.04.002.

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33

Straw, N. A., G. Green, and D. T. Williams. "Dieback and recovery in poplar and attack by the hornet clearwing moth, Sesia apiformis (Clerck) (Lepidoptera: Sesiidae)." Bulletin of Entomological Research 97, no. 6 (2007): 555–67. http://dx.doi.org/10.1017/s0007485307005342.

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AbstractA survey of 801 poplar trees in central east England in 1999 demonstrated a correlation between crown dieback and infestation by hornet clearwing moth (Sesia apiformis), induced by a period of drought in 1995–1996. To determine whether trees colonised by S. apiformis would subsequently deteriorate and die or whether they could recover despite infestation and damage to the stem, all trees in the original survey were re-assessed in 2001, 2003 and 2005. The repeat surveys showed that trees with 70% or less crown dieback in 1999 replaced their canopy and generally improved by 2005, irrespe

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34

Rubatto, Daniela, Dieter Gebauer, and Roberto Compagnoni. "Dating of eclogite-facies zircons: the age of Alpine metamorphism in the Sesia–Lanzo Zone (Western Alps)." Earth and Planetary Science Letters 167, no. 3-4 (1999): 141–58. http://dx.doi.org/10.1016/s0012-821x(99)00031-x.

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35

Chellini, Giuseppe, Francesco Vittorio Lippi, and Walter Salvatore. "A multidisciplinary approach for fatigue assessment of a steel–concrete high-speed railway bridge on Sesia river." Structure and Infrastructure Engineering 10, no. 2 (2012): 189–212. http://dx.doi.org/10.1080/15732479.2012.719527.

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36

Corti, Luca, Gioele Alberelli, Davide Zanoni, and Michele Zucali. "Tectonometamorphic evolution of the Lago della Vecchia metaintrusive and its country rocks, Sesia-Lanzo Zone, Western Alps." Italian Journal of Geosciences 137, no. 2 (2018): 188–207. http://dx.doi.org/10.3301/ijg.2018.08.

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37

St�ckhert, B., E. J�ger, and G. Voll. "K ? Ar age determinations on phengites from the internal part of the Sesia Zone, Western Alps, Italy." Contributions to Mineralogy and Petrology 92, no. 4 (1986): 456–70. http://dx.doi.org/10.1007/bf00374428.

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38

Ramsbotham, W. "Time Constraints on the Metamorphic and Structural Evolution of the Southern Sesia-Lanzo Zone, Western Italian Alps." Mineralogical Magazine 58A, no. 2 (1994): 758–59. http://dx.doi.org/10.1180/minmag.1994.58a.2.131.

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39

Cantù, Michela, Luca Spaggiari, Michele Zucali, Davide Zanoni, and M. Iole Spalla. "Structural analysis of a subduction-related contact in southern Sesia-Lanzo Zone (Austroalpine Domain, Italian Western Alps)." Journal of Maps 12, sup1 (2016): 22–35. http://dx.doi.org/10.1080/17445647.2016.1155925.

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40

Rigaux, Dominique. "Le cycle de la vie de saint Benoît dans le cloître de l’abbaye de San Nazzaro Sesia." Revue Mabillon 23 (January 2012): 135–61. http://dx.doi.org/10.1484/j.rm.5.101008.

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41

Kapferer, Notburga, Ivan Mercolli, and Alfons Berger. "The composition and evolution of an Oligocene regolith on top of the Sesia–Lanzo Zone (Western Alps)." International Journal of Earth Sciences 100, no. 5 (2011): 1115–27. http://dx.doi.org/10.1007/s00531-010-0637-8.

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42

Chouinard, Gérald, Sylvie Bellerose, Michèle Roy, and Charles Vincent. "A note on the activity and species composition of sesiids [Lepidoptera: Sesiidae] as measured by pheromone traps and trunk sampling in apple orchards of southwestern Quebec." Communication brève 87, no. 3 (2007): 131–34. http://dx.doi.org/10.7202/015855ar.

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Abstract Adult males and larvae of sesiids were monitored in ten (1989–1991), five (2000) and two (2004) Quebec apple orchards. Multi Pher III traps baited with 99.1% Z, Z-3, 13-octadecadienyl acetate and 0.9% Z, E plus E, Z-3, 13-octadecadienyl acetate were used for adults, and trunk sampling was used for larvae. Synanthedon scitula, S. pyri, Podosesia syringae, S. acerrubri, S. fulvipes, S. exitiosa, S. acerni and Sesia tibialis males were captured between 1989 and 1991. Only 5 of the 347 adults of the S. scitula/pyri complex captured in 2000 belonged to S. pyri.

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43

van Roermund, H. L. M., and J. M. Lardeaux. "Modification of antiphase domain sizes in omphacite by dislocation glide and creep mechanisms and its petrological consequences." Mineralogical Magazine 55, no. 380 (1991): 397–407. http://dx.doi.org/10.1180/minmag.1991.055.380.09.

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AbstractA T.E.M. study of omphacites from the western Italian Alps (Sesia Lanzo Zone and Monviso eclogites) has revealed a bimodal size distribution of antiphase domains: (a) 250–350 Å, (b) ≥ 2500 Å. In addition observed dislocation substructures and ‘large-scale’ antiphase domains are intimately interconnected.A model is presented that can explain modification of the antiphase domain sizes by the interplay of cooling/growth and dislocation glide and/or creep mechanisms. Subsequent coarsening of the modified antiphase domains is inferred to be the result of surface free-energy processes. The m

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44

Assanelli, Matteo, Pietro Luoni, Gisella Rebay, Manuel Roda, and Maria Iole Spalla. "Tectono-Metamorphic Evolution of Serpentinites from Lanzo Valleys Subduction Complex (Piemonte—Sesia-Lanzo Zone Boundary, Western Italian Alps)." Minerals 10, no. 11 (2020): 985. http://dx.doi.org/10.3390/min10110985.

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In the upper Tesso Valley the folded contact between Piemonte Zone ophiolites and Sesia-Lanzo Zone continental crust is exposed. Here serpentinites, metabasites, calcschists and fine-grained gneisses are deformed by four ductile superposed groups of structures, associated with different mineral assemblages. Different serpentinite lithologies have been recognized and studied in detail. Mylonitic D2 structures are pervasive and mineral assemblages point to re-equilibration at T of 450 ± 50 ∘C and P of 0.8 ± 0.3 GPa, under blueschist/epidote amphibolite-facies conditions. Pre-D2 structures and mi

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45

Compagnoni, Roberto, Martin Engi, and Daniele Regis. "Valle d'Aosta section of the Sesia Zone: multi-stage HP metamorphism and assembly of a rifted continental margin." Geological Field Trips 6, no. 1.2 (2014): 1–44. http://dx.doi.org/10.3301/gft.2014.02.

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46

Perotti, Luigi, Irene Maria Bollati, Cristina Viani, et al. "Fieldtrips and Virtual Tours as Geotourism Resources: Examples from the Sesia Val Grande UNESCO Global Geopark (NW Italy)." Resources 9, no. 6 (2020): 63. http://dx.doi.org/10.3390/resources9060063.

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In the 20th anniversary year of the European Geopark Network, and 5 years on from the receipt of the UNESCO label for the geoparks, this research focuses on geotourism contents and solutions within one of the most recently designated geoparks, admitted for membership in 2013: the Sesia Val Grande UNESCO Global Geopark (Western Italian Alps). The main aim of this paper is to corroborate the use of fieldtrips and virtual tours as resources for geotourism. The analysis is developed according to: i) geodiversity and geoheritage of the geopark territory; ii) different approaches for planning fieldt

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47

Regis, D., D. Rubatto, J. Darling, B. Cenki-Tok, M. Zucali, and M. Engi. "Multiple Metamorphic Stages within an Eclogite-facies Terrane (Sesia Zone, Western Alps) Revealed by Th–U–Pb Petrochronology." Journal of Petrology 55, no. 7 (2014): 1429–56. http://dx.doi.org/10.1093/petrology/egu029.

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48

Gosso, Guido, Bruno Messiga, Gisella Rebay, and Maria Iole Spalla. "Interplay between deformation and metamorphism during eclogitization of amphibolites in the Sesia–Lanzo Zone of the Western Alps." International Geology Review 52, no. 10-12 (2010): 1193–219. http://dx.doi.org/10.1080/00206810903529646.

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49

Marco, Rubbo, Borghi Alessandro, and Compagnoni Roberto. "Thermodynamic analysis of garnet growth zoning in eclogite facies granodiorite from M. Mucrone, Sesia Zone, Western Italian Alps." Contributions to Mineralogy and Petrology 137, no. 4 (1999): 289–303. http://dx.doi.org/10.1007/s004100050551.

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50

CASTELLI, D. "Eclogitic metamorphism in carbonate rocks: the example of impure marbles from the Sesia-Lanzo Zone, Italian Western Alps." Journal of Metamorphic Geology 9, no. 1 (1991): 61–77. http://dx.doi.org/10.1111/j.1525-1314.1991.tb00504.x.

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