• Non ci sono risultati.

Blacic J. D., 1975. Plastic-deformation mechanism in quartz: the effect of water.

N/A
N/A
Protected

Academic year: 2021

Condividi " Blacic J. D., 1975. Plastic-deformation mechanism in quartz: the effect of water. "

Copied!
10
0
0

Testo completo

(1)

Grazie a

(2)

Bibliografia:

Barbey P., Cheilletz A., Laumonier B., 2000. The Canigou orthogneiss (eastern Pyrenees, France, Spain): an Early Ordovivian rapakivi granite laccolith and its contact aureole. C.R.Acad.Sci.Paris, Sciences de la Terre et des planètes 332 (2001) pp 129-136.

Blacic J. D., 1975. Plastic-deformation mechanism in quartz: the effect of water.

Tectonophysics, 27, pp. 271-294.

Blenkinsop T. G., Treloar P. J., 1995. Geometry, classification and kinematics of S- C fabrics. Journal of Structural Geololgy, 17,pp. 397-408.

Boschma D., 1963. Succession Hercynian structures in some areas of the Central Pyrenees, Leidse Geologische Mededelingen, 28, pp. 103-176.

Bouchez J. L., 1977. Le quartz et la cinematique des zones ductiles. Thesis Doctoral. Universitè de Nantes.

Bouchez J. L., Duval P., 1982. The fabric of polycrystalline ice deformed in simple shear: experiments in torsion, natural deformation and geometrical interpretation.

Textures and Microstructures, 5,pp. 171-190.

Carosi R., Lombardo B., Musumeci G., Pertusati P.C., 1999.Geology of the Higher Himalayan Criystalline in Khumbu Himal (Eastern Nepal). Journal of Asian Earth Sciences, vol 17, pp 785-803.

Carreras J., 1973. Petrologia y analisis estructural de las rocas metamorficas de la zona del Cabo de Creus (prov. Gerona). Umpubl. Thesis, Univ. Barcelona.

Carreras J., 1975. Las deformaciones tardi-hercinicas en el litoral septentrional de la peninsula del Cap de Creus (prov. Gerona, Espana): la genesis de las bandas miloniticas. Acta Geologica Hispanica, 10, pp. 109-115.

Carreras J., 1988. On the structural evolution of the Pyrenean segment of the Hercynian belt. In:Symposium on the geology of Pyrenees and Betics. pp. 38-39.

Carreras J., 1992. Zonas de cizalla en rocas foliadas: geometria y cinematica.

Simposios II Congreso Geologico de Espana, Salamanca, 2, pp. 355-364.

Carreras J., 1995. Métamorphisme Hercynien. Synthèse géologique et géophysique des Pyrénées, Tome 1 – Cycle Hercynien -1995. Edition BRGM – ITGE, pp 660-677 Carreras J., 1997. Shear zones in foliated rocks: geometry and kinematics. In:

Sengupta S. (ed.), Evolution of geologic structures in micro- to macro-scales. Chapm and Hall. London, pp. 185-201.

Carreras J., 2001. Zooming on Northern Cap de Creus shear zones. Journal of Stuctural Geology, 3, pp 1457-1486.

Carreras J., Capella I., 1994. Tectonics levels in the Paleozoic basement of the Pyrenees : a review and a new interpretation. Journal of Structural Geology, Vol.16, n°11, pp 1509-1524.

Carreras J., Debat P., Coordinateurs, 1995. Tectonique Hercynienne. Synthèse

géologique et géophysique des Pyrénées, Tome 1 – Cycle Hercynien -1995. Edition

(3)

Carreras J., Druguet E., 1994. Structural zonation as a result of inhomogeneous non-coaxial deformation and its control on a syntectonic plutonic intrusion: an example from the Cap de Creus area, eastern Pyrenees. Journal of Structural Geology, n° 16, pp 1525-1534.

Carreras J., Druguet E., Griera A., Soldevila J., 2004. Strain and deformation history in a syntetonic pluton. The case of the Roses granodiorite (Cap de Creus, Eastern Pyrenees). In: Transport and flow processes within shear zones. Special publication - Geological Society of London in press.

Carreras J., Druguet E. Guide to the Cap de Creus shear zones.

Carreras J., Garcìa-Celma A., 1982. Quartz c-axis fabric variation at the margins of a shear zone developped in schists from the Cap de Creus (Spain). . Acta geologica Hispanicà, t.17 , pp 137-149.

Carreras J., Julivert M., Santanach P. The Pyrenean basement: Hercynian structure and effect of alpine reworking. Project BP-88-0240 as a part of activity for IGCP Project 276.

Carreras J., Julivert M., Santanach P., 1980. Hercynian mylonite belts in the eastern Pyrenees : an example of shear zones associates with late folding. Journal of Structural Geology. Vol.2, n°1/2, pp 5-9.

Carreras J., Losantos M., 1982. Geological settings of the Roses granodiorite (E- Pyrenees, Spain). Acta Geològica Hispanicà, t.17 n°4, pp 211-217.

"Casas J. A., Espinosa J. R., Quirós M., 1996. Standard model stability bounds for new physics within LHC reach. Physics letter b, 382, 4.

Cavet P., 1957. Le Paleozoique de la zone axiale des Pyrenees orientales entre le Rousillon et l'Andorre. Bullettin Service Carte Geologique France, 254 (55), pp. 303- 518.

Choukroune P., ECORS Team, 1989. The ECORS Pyrenean deep seismic profile reflection data of the overall structure of an orogenic belt. Tectonics, 8 (1), pp. 23-29.

Choukroune P., Seguret M., 1973. Tectonics of the Pyrenees: role of compression and gravity. Gravity and Tectonics, K. De Jong and R. Scholten (eds.), Wiley, New York, pp. 141-156.

Choukroune P., Francheteau J., Hekinian R., Le Pichon Y., Needham H. D., 1976. Oceanic fracture zones do not provide deep sections in the crust. Canadian Journal of Earth Sciences, 13, pp. 1223-1235.

Coney P. J., Muñoz J. A., McClay K. R.,Evenchick C. A., 1996. Syntectonic burial and post-tectonic exhumation of the southern Pyrenees foreland fold–thrust belt.

Journal of the Geological Society, 153, pp. 9-16.

Daignieres M., Nicolas A., Achauer U., 1994. Rift initiation by lithospheric rupture.

Earth and Planetary Science Letters, 123, pp. 281-298.

Debat P., Soula J.C., 1995. Métamorphisme Hercynien. Synthèse géologique et

géophysique des Pyrénées, Tome 1 – Cycle Hercynien -1995. Edition BRGM – ITGE,

pp650-651.

(4)

Dennis J. A., Secor D. T., Hibbard P. J., Stoddard F. E., 2002. The Carolina Zone:

overview of Neoproterozoic to Early Paleozoic peri-Gondwanan terranes along the eastern Flank of the southern Appalachians. Earth-Science Reviews, 57, pp. 299- 339.

Druguet E., 2001. Development of high thermal gradients by coeval transpression and magmatism during the Variscan orogeny : insights from the Cap de Creus (Eastern Pyrenees). Tectonophysics 332 (2001) pp 275-293.

Duràn H., 1990. El paleozoico de les Guilleries. Acta Geologica Hispanicà, Vol.25 n°1-2, pp 83-103.

ECORS Team, 1988. The ECORS deep reflection seismic surve across the Pyrenees.

Nature, 331, pp. 508-511.

Etchecopar A., 1977. A lane kinematic model of progressive deformation in a polycrystalline aggregate. Tectonophysics, 39, pp. 121-139.

Etchecopar A., Vasseur G., 1987. A 3-D kinematic model of fabric development in polycrystalline aggregates: comparisons with experimental and natural examples.

Journal of Structural Geolology, 9,pp. 705-718.

Fitzgerald P. G., Muñoz J. A., Coney P. J., Baldwin S. L., 1999. Asymmetric exhumation across the Pyrenean orogen: implications for the tectonic evolution of a collisional orogen. Earth and Planetary Science Letters 173, pp. 157-170.

Flinn D., 1978. Construction and computation of three-dimensional progressive deformation. Journal of the Geological Society of London, n°135, pp 291-305.

Frassi C., 2006. Analisi di un settore della zona assiale della catena varisica sarda:

le zone di taglio Badesi - Li Paùlis e loro implicazione a scala regionale. Atti della società toscana di scienze naturali serie A, 111,tot. pp. 6,2006.

Garcìa-Celma A., 1982. Domainal and fabric heterogeneities in the Cap de Creus quartz mylonites. Journal of Structural Geology, vol 4, n° 4, pp 443-455.

Geyssant J., Guitard G., Laumonier B., 1980. Analyse Structurale des gneiss oeilles blastomylonitiques du versant nord du Canigou (P.O.). Comptes Rendus de l'Academie des Sciences, ser. D. 290: pp. 1103-1106.

Ghosh S. K., Ramberg H., 1976. Reorientation of inclusions by combination of pure shear and simple shear. Tectonophysics, 34,pp. 1-70.

Gliezes G., Leblanc D., Bouchez J. L., 1998b. The main phase of the Hercynian orogeny in the Pyrenees is a dextral transpression. Continental transpression and transtensional tectonics, Holdsworth R. E., Strachan R. A., Dewey J. F. (eds.).

Geological Society Special Publications, 135, pp. 267-273.

Green H. W., Griggs D. T., Christie J. M., 1970. Syntectonic and annealing recrystallization of fine-grained quartz aggregates. In: Paulitsch P (ed) Experimental and natural rock deformation. Springer, Berlin Heidelberg New York, pp. 272-335.

Guitard G., 1970. Le metamorphisme hercynien mesozonal et le gneiss oeilles du

massif du Camigou, (Pyrennees Orientales). Memoires du Bureau de Recherches

Geologiques et Minieres, 63, pp. 353.

(5)

Guitard G., 1976. Aspect des relations entre le tectonique et metamorphism.

Memoires du Bureau de Recherches Geologiques et Minieres (2e ser.), 1 (4), pp. 129- 164.

Guitard G., Geyssant J., Laumonier B., 1984.Les plissements hercyniens tardifs dans le Paleozoique inferieur du versant nord du Canigou. 1ere partie: analysi geometrique e chronologie des phases superposees. Relation avec le granite de Montluis et le metamorphism regional. Geologie de France, 4, pp. 9-125.

Guitard G., Vielzeuf D., Martinez F., Coordinateurs, 1995. Métamorphisme Hercynien. Synthèse géologique et géophysique des Pyrénées, Tome 1 – Cycle Hercynien -1995. Edition BRGM – ITGE, pp 501-402.

Hartevelt J. J. A., 1970. Geology of the Upper Segre and Valira valleys, Central Pyrenees, Andorra-Spain. Leidse Geologische Mededelingen A109, 45, pp.167-236 Hirth G., Tullis J., 1991. Dislocation creep regimes in aggregates. Journal of

Structural Geology, vol 14, n°2, 145-159.

Hobbs B. E., 1985. The geological significance of microfabric analysis. In: Wenk H.

R. (ed.). Preferred orientation in deformed metals and rocks: an introduction to modern texture analysis. Academic Press, Orlando, pp. 463-484.

Hobbs B. E., McLaren A. C., Paterson M. S., 1972. Plasticity of single crystals of synthetic quartz. In: Heard H. C., Borg I. Y., Carter N. L., Raleigh C. B. (eds). Flow and fracture of rocks. Geophysical Monograph, 16, pp. 29-53.

Jeffrey G., 1922. The motion of ellipsoidal particles immersed in a viscous fluid.

Proc R Soc Lond, A122,pp. 161-179.

Julivert M., Duràn H., 1990. Paleozoic stratigraphy of the central and northern part of the Catalonian coastal ranges. Acta Geològica Hispanicà, Vol.25 n°1-2, pp 3-12.

Julivert M., Duràn H., 1990. The hercynian structure of the Catalonian coastal ranges. Acta Geològica Hispanicà, Vol.25 n°1-2, pp 13-21.

Julivert M., Martinez F.J., 1980. The paleozoic of the Catalonian coastal ranges (NW Mediterranean). F.P. Sassi an G. Zirpoli eds, IGCP Project n°5, Newsletter, pp 124-128.

Kleinsmiede W. F. J., 1960. Geology ofthe Valle d'Aran (Centrale Pyrenees). Leidse Geologische Mededelingen, 18, pp. 129-245.

Kruhl J. H., 1996. Prism-and basal-plane parallel subgrain boundaries in quartz: a micro-structural geothermo-barometer. Journal of Metamorphic Geology, 14, pp.

581-589.

Kruhl J. H., 1998. Reply: Prism- and basal-plane parallel subgrain boundaries in quartz: a microstructural geothermobarometer. Journal of Metamorphic Geology, 16, pp. 142-146.

Labaume P., Mutti E., Seguret M., 1985. Megaturbidites: A depositional model from the eocene of the SW-Pyrenean Foreland basin, Spain. Geo-Marine Letters, pp.91-101

Lamouroux Ch., Soula J.C., Deramond J., Debat P., 1980a. Shear zone in

granodiorite massif in the Central Pyrenees and the behaviour of these massif during

the Alpine Orogenesis. Journal of Structural Geology, 2, pp. 49-53.

(6)

Laumonier B., Geyssant J., Guitard G., 1984. Les plissement hercyniens tardifs dans le Paleozoique du versant nord du Cnigou. 2eme partie:essai de restitution retrotectonique et cartographique des megastructures. Geologie France, 4, pp. 127- 147.

Laumonier B., Guitard G., 1978. Contribution a l'etude de la tectonique superposee hercynienne des Pyrenees Orientales: le probleme des plissements precoces dans le paleozoique inferieur epizonale (serie de Jujols) du synclinal de Villefranche de Conflent. Revue de Geographie Phisique et Geologie Dynamique S2, 20, pp.177-211.

Law R. D., 1987. Heterogeneous deformation and quartz crystallographic fabric transition: natural examples from the Moine Thrust zone of Stack of Glencoul, northern Assynt. Journal of Structural Geology, 9, pp. 819-834.

Law R. D., 1990. Crystallographic fabrics: a selective review of their application in research in structural geology. In: Deformation mechanism, rehology and tectonics, edited by Knipe R. and Rutter E., Geological Society Special Publication, 54, pp. 335- 352.

Law R. D., Casey M., Knipe R. J., 1986. Kinematic and tectonic significance of microstructures and crystallographic fabrics within quartz mylonites from the Asynt and Eriboll regions of the Moine Thrust zone, NW Scotland. Trans R Society Edimburg Earth Sciences, 76,pp. 99-125.

Law R. D., Knipe R. J., Dayan H., 1984. Strain path partitioning within thrust sheets: microsctructural and petrofabric evidence from the Moine Thrust zone at Loch Eriboll, north west Scotland. Journal of Structural Geololgy, 6,pp. 477-497.

Law R. D., Schmid S. M., Wheeler J., 1990. Simple shear deformation and quartz crystallographic fabrics: a possible natural example from the Torridon area of NW Scotland. Journal of Structural Geology, 12, pp. 29-45.

Law R. D., Searle M. P., Simpson R. L., 2004. Strain, deformation temperatures and vorticity of flow at the top of Greater Himalayan Slab, Everest Massif, Tibet.

Journal of the Geological Society of London, vol 161, pp 305-320.

Le Pichon X., Sibuet J. C., 1971. Western extension of boundary between European and Iberian plates during the Pyrenean opening. Earth Planet Soc. Lett., 12, pp.83-88.

Liesa M., Carreras J., 1989. On the Structure and metamorphism of the Roc de Fraussa Massif (Eastern Pyrenees). Geodinamica Acta (Paris) 1989, 3,2, pp 149-161.

Lister G. S., 1974. The theory of deformation fabrics. Unpublished Ph.D. thesis, Australian National University, Canberra.

Lister G. S., 1977. Crossed-girdle c-axis fabric in quartzites plastically deformed by plane strain and progressive simple shear. Tectonophysics, 39, pp. 51-54.

Lister G. S., 1979. Fabric transitions in plastically deformed quartzites: competition between basal, plastic deformation of quartzite. Journal of Structural Geology, 3, pp.

67-76.

Lister G. S., Hobbs B. E., 1980. The simulation of fabric development during plastic deformation and its application to quartzite: fabric transitions. Journal of Structural Geology, 1, pp. 99-115.

Lister G. S., Paterson M. S., 1979. The simulation of fabric development during

plastic deformation and its application to quartzite: fabric transitions. Journal of

(7)

Lister G. S., Paterson M. S., Hobbs B. E., 1978. The simulation of fabric development in plastic deformation and its application to quartzite: the model.

Tectonophysics, 45, pp. 107-158.

Lister G. S., Williams P. F., 1979. Fabric development in shear zones: theoretical controls and observed phenomena. Journal of Structural Geology, 1, pp. 283-297.

Lister G. S., Williams P. F., 1983. The partitioning of deformation in flowing rock mases. Tectonophysics, 92, pp. 1-33.

Malasoma A., Marroni M., 2007. HP/LT metamorphism in Volparone Breccia (Northern Corsica, France): Evidence for involvement of the Europe/ Corsica continental margin in the Alpin Subdution zone. Journal of Structural Geology,2007, 25, pp 529-547.

Malvern L., 1969. Introduction to the Mechanics of a continuous medium. Prentice- Hall, Englewood Cliffs, New Jersey

.

Mancketow N. S., Arbaret L., Pennacchioni G., 2002. Experimental observations on the effect of interference slip on rotation and stabilisation of rigid particles in simple shear and a comparison with natural mylonites. Journal of Structural Geology, 24, pp. 567-585.

Marjoribanks R. W., 1976. The relation between microfabric and strain in a progressively deformed quartzite sequence from central Australia. Tectonophysics, 32, pp. 269-293.

Mattauer M., 2004. Orthogneiss in the deepest levels of the variscan belt are not a Precambrian basement but Ordovician granites : tectonics consequences. Geoscience 336, 2004, pp 480-489.

Mattauer M., Henry J., 1974. the Pyrenees in Mesozoic/Cenozoic orogenic belts:

data for orogenic studies. Spencer A.M. (ed.), Geological Society of London Special Publication, 4, pp. 3-21.

Matte P., 1986. Tectonics and plate tectonics model for the variscan belt of Europe.

Tectonophysics 126, pp 329-374.

McCaig A. M., 1986. Thick and thin-skinned tectonics in the Pyrenees.

Tectonophysics, 129, pp. 319- 342.

Means W. D., Hobbs B., Lister G. S., Williams P. F., 1980. Vorticity and non- coaxiality in progressive deformation. Journal of Structural Geology, 2, pp. 371-378.

Means W. D.1994. Rotational quantities in homogeneous folw and the development of small-scale structures. Journal of Structural Geology, 16, pp. 437-445.

Muller J., Rogers P., 1987. L'evolution structurale des Pyrenees (Domaine central et occidental). Le segment Hercynien, la chaine de fond alpine. Geologie Alpine, 53, pp.

149-191.

Muñoz J. A., 1992. Evolution of a continental collision belt ECORS-Pyrenees crustal balanced cross section. In: Thrusts Tectonics, McClay K. R. (ed.), Chapman and Hall, pp. 235-246.

Muñoz J. A., Martinez A., Verges J., 1986. Thrust sequences in the spanish

eastern Pyrenees. Journal of Structural Geology, 8, pp. 399-405.

(8)

Nicolas A., Poirier J. P., 1976. Crystalline plasticity and solid state flow in metamorphic rocks. John Wiley & Sons, London, p. 444.

Oele J. A., 1966.The structural history of the Vall Ferrera Area, the transition between the Aston and the Salat Pallaresa anticlinorium, (Centrale Pyrenees, Spain).

Leidse Geologische Mededelingen, 38, pp. 129-164.

Olivet J. L., Bonnin J., Beuzart P., Auzende J. M. 1981. Cinematique de l' Atlantique Nord et Central.CNEXO, Paris.

Passchier C. W., 1987. Stable position of rigid objects in non-coaxial flow: a study in vorticity analysis. Journal of Structural Geology, 9, n° 5/6, pp 679-690.

Passchier C. W., 1991a. The classification of dilatant flow type. Journal of Structural Geology, 13, pp. 101-104.

Passchier C. W., 1991b. Geometric constraints on the development of shear bands in rocks. Geologie en Mijnbouw, 70, pp. 203-211.

Passchier C. W., 1998. Monoclinic model shear zones. Journal of Structural Geology, vol20,n°8, pp1121-1137.

Passchier C. W., Myers J. S., Kroner A., 1990. Field geology of high-grade geiss terranes. Springer. New York.

Passchier C. W., Throuw R. A. J., 1996. Microtectonics. Springer Verlag, Berlin- Heidelberg–New York .

Puigdefàbregas G., Souquet P., 1986. Tecto-sedimentary cycles and depositional sequences of the Mesozoic and Tertiary from the Pyrenees. Tectonophysics, 129, pp.

173-203.

Ramsay J. C., 1980. Shear zone geometry: a review. Journal of Structural Geology, n°8, pp 83-101.

Ramsay J. C., Allison I., 1979.Structural Analysisof shear zones in an Alpinised Hercynian granite. Schweizerische Mineralogische und Petrographische Mitteilungen, 59, pp. 251-279.

Ramsay J. C., Huber M., 1983. The techniques of modern Structural geology. Vol 1:

strain analysis. Academic Press London, pp 111-113.

Ramsay J. C., Graham R. H., 1970. Strain variationin shear belts. Canadian Journal of Earth Sciences, 7, pp. 786-813.

Reche J., Carreras J., Druguet E., 1995. Métamorphisme Hercynien. Synthèse géologique et géophysique des Pyrénées, Tome 1 – Cycle Hercynien -1995. Edition BRGM – ITGE, pp 524-555.

Robin P. Y. F., Cruden A. R., 1994. Strain and vorticity pattern in ideally ductile transpression zones. Journal of Structural Geology, 16, pp. 447-466.

Roure F., Choukroune P., Berastegui X., Muñoz J. A., Villien A.,Matheron P., Bareyt M., Seguret M., Camara P., Deramond J., 1989. ECORS deep seismic data and balanced cross section: geometric constrains on the evolution of the Pyrenees.

Tectonics, 8, pp. 41-50.

Saillant J. P., 1982. La faille de Merens (Pyrenees Orientales) microstructures and

(9)

Schimd S. M., Casey M., 1986. Complete fabric analysis of some commonly observed quartz c-axis patterns. In: Hobbs B. E., Heard H. C. (eds). Mineral and rock deformation: laboratory studies. Geophysical Monograph, 36, pp. 263-286.

Sebastian A., Reche J., Duràn H., 1990. Hercynian metamorphism in catalonian coastal ranges. Acta Geològica Hispanicà, Vol.25 n°1-2, pp 31-38.

Simpson C., 1981. Ductile shear zones: a mechanism of rock deformation in the ortogneiss of the Maggia Nappe, Ticino, Switzerland. Unpubl. Ph.D. Thesis, ETH Zurich, Switzerland.

Simpsons C., Carreras J., Losantos M., 1982. Inhomogeneous deformation in Roses granodiorite, N.E. Spain. Acta geològica Hispanicà, t.17 n°4, pp 219-226.

Soula J. C., 1982. Characteristics and mode of emplacement of gneiss domes and plutonics domes in central eastern Pyrenees, Journal of Structural Geology, 4, pp.

313-342.

Soula J. C., Deabt P., Deramond J., Pouguet P., 1986. A dynamic model of the structural evolution of the hercynian Pyrenees. Tectonophysics 129, pp 29-51.

Soula J. C., Debat P., Deramond J., Guchereau J. Y., Lamouroux Ch., Pouget P., Roux L., 1986a. Evolution structurale des ensembles metamorphiques des gneiss et des granitides dans les Pyrenees Centrales. Bullettin de la Societe Geologique de France (8emem ser.), 2 (1), pp. 79-93.

Soula J. C., Debat P., Deramond J., Guchereau J. Y., Pouget P., Roux L., 1986b.

A dynamic model of the structural evolution of the Hercynian Pyrenees.

Tectonophysics, 129, pp. 115-147.

Souriau A., Granet M., 1995. A tomographic study of the lithosphere beneath the Pyrenees from local and teleseismic data. Journal of Goephysical Research, 100, pp.

117-18.

Stipp M., Stunitz H., Heilbronner R., Schmid S. M, 2002a. Dynamic recrystallizazion of quartz: correlation between natural and experimental conditions (from: De Meer S., Drury M. R., De Bresser J. H. P., Pennock G. M.. 2002.

Deformation mechanisms,rheology and tectonics:current status and future perspective. Geological society, london, special publications, 200, pp171-190.).

Stipp M., Stunitz H., Heilbronner R., Schmid S. M., 2002b. The eastern Tonale fault zone: a “natural laboratory” for cristal plastic deformation of quartz over a temperature range from 250 to 700°C. Journal of Structural Geology 24, pp 1861- 1884.

Teixell A., 1996. The Anso transect of the Pyrenees: basement and cover thrust geometries. Journal of the Geological Society London, 153, pp. 301-310.

Teixell A., 1998. Custal structure and orogenic material budget in the west central Pyrenees. Tectonics, 17, pp. 395-406.

Tikoff B., Fossen H., 1995. The limitation of three-dimensional kinematic vorticity analysis. Journal of Structural Geology, 17, pp. 1771-1784.

Tullis J., Christie J. M., Griggs D. T., 1973. Microstructures and preferred

orientations of experimentally deformed quartzites. Bullettin of Geologic Society of

America, 84, pp. 297-314.

(10)

Twiss R. J., Moore E. S., 1992. Structural geology. W. H. Freeman and company, New York.A101.

Vergés J., Millán H., Roca E., Muñoz J. A., Marzo M., Cirés J., Den Bezemer T., Zoetemeijer R., Cloetingh S., 1995. Eastern Pyrenees and related foreland basins:

pre-, syn- and post-collisional crustal-scale cross-sections. Marine and Petroleum Geology, 12, pp. 903-915.

Verhoeff P. N. W., Vissers R. L. M., Zwart H. J., 1984. A new interpretation of the structural and meamorphic history of the western Aston massif (Centrale Pyrenees, France). Geologie en Mijnbow, 63, pp.399-410.

Wallis S. R., 1992. Vorticity analysis in a metachert from the Sambagawa Belt, SW Japan. Journal of Structural Geology, 14, pp 271-280.

Wallis S. R., Platt J. P., Knott S. D., 1993. Recognition of syn-convergence extension in accretionary wedges with examples from Calabrian arc and the Eastern Alps. American Journal of Sciences ,293, pp. 463-495.

Wauschkuhn B., 2003. The evolution of central Asia (The Himalayas: when the continent collide...). In the scope of the geologic graduate seminar 2003.

White S. H., Burrows S., Carreras J., Shaw N. D., Humphreys F. J., 1980. On the mylonites in ductile shear zones. Journal of Structural Geology, 2, pp. 175-188.

Wickham S. M., Oxburgh E. R., 1985. Continental rifts as a setting for regional metamorphism. Nature, 318, pp. 330-333.

Wickham S. M., Oxburgh E. R., 1986. A rifted tectonic setting for Hercynian high- termal gradient metemorphism in the Pyrenees. Tectonophysics, 129 (1-4), pp. 53- 59.

Williams G. D., 1985. Thrust tectonics in the south central Pyrenees. Journal of Structural Geology, 7, 1, pp. 11-17.

Zwart H. J., 1962. On the determination of polymetamorphic mineral association and its application to the Bossot area (Central Pyrenees). Geologische Rundschau, 52, pp. 38-65.

Zwart H. J., 1963. The structural evolution of the Paleozoic of the Pyrenees.

Geologische Rundschau, 53, pp. 170-205.

Zwart H. J., 1968. The Paleozoic crystalline Rocks of the Pyrenees in their structural setting. Kristalinikum, 6, pp. 125-140.

Zwart H. J., 1979.The geology of the Central Pyrenees. Leidse Geologische Mededelingen, 50, pp. 1-74.

Zwart H. J., 1986. The Variscan geology of the Pyrenees. In E. Banda and S.M.

Wickham (Editors), The geological evolution of the Pyrenees, Tectonophysics, 129, pp 9-27.

Zwart H. J.,1960. Relations between folding and metamorphism in the Central

Pyrenees, and their chronological succession. Geologie en Minjbow, 22, pp. 38-65.

Riferimenti

Documenti correlati

The analysis of the selected proxies outlined a pronounced sensitivity of Lake Ledro to hydrological variability throughout the whole time span considered, but

Despite different sizes and operating regions, the businesses of the consortium affiliates were relatively homogeneous: revenues were generated by new unit sales, by revamping old

POTENTIAL VALORISATION STRATEGIES Resource based Market based Policy based..

“yes” responses to script-consistent distracters (i.e., False alarms Consistent), “yes” re­ sponses to script-inconsistent distracters (i.e., False alarms Inconsistent),

This study reported data from the REPOSI registry on 2631 older subjects dis- charged home from internal medicine wards, exploring the association of several pharmacotherapy

The capability to synthesize phytochelatins and the presence of constitutive and functional phytochelatin synthases are ancestral (plesiomorphic) characters for basal

come in Face value di Johan van der keuken, ho avuto l’impressione che il tentativo di anda- re al di là della maschera che tutti noi indossiamo nella vita di ogni giorno sia

It does not investigate either condition required to support the emergence of a new technological paradigm and radical innovation or the preferred strategic and