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13 Bibliografia AERDEN (1994). Porphyroblast non-rotation during crustal extention in the Varisican Lys-Caillaouas Massif, Pyrenees

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13 Bibliografia

AERDEN (1994). Porphyroblast non-rotation during crustal extention in the Varisican Lys-Caillaouas Massif, Pyrenees. Journal of Structural

Geology, 17: 709-725.

AERDEN (2004). Correlating deformation in Variscan NW-Iberia using porphyroblasts; implications for the Ibero-Armorican Arc. Journal of

Structural Geology, 26: 177-196.

T. H. BELL (1985). Deformatinion partitioning and porphyroblasts rotation in metamorphic rocks: a radical reinterpretation. J. metamorphic Geol. 3: 109-118.

T. H. BELL and S.E. JOHNSON (1992). Shear sense: a new approach that resolves conflicts between criteria in metamorphic rocks. J. metamorphic

Geol. 10: 99-124.

J. CARRERAS, M. JULIVERT, P. SANTANACH. The Pyrenean Basement: Hercinian structure and effects of Alpine Reworking. Pag.: 275-293.

J. CARRERAS, M. JULIVERT, P.SANTANACH (1980). Hercinian mylonite belts in the eastern Pyrenees: an example of shear zones associated with late folding. Journal of Structural Geology, 2: 5-9.

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J. CARRERAS, F. ORTUNO (1990). Fondamento geométrico y cinematico de la modelizacion teorica y experimental de deformaciones no-coaxiales. Acta Geologica Hispanica 25: 237-259.

J. CARRERAS, I. CAPELLA (1994). Tectonic levels in the Paleozoic basement of Pyrenees: a review and a new interpretation. Journal of

Structural Geology, 16: 1509-1524.

J. CARRERAS (2001). Zooming on Northern Cap de Creus shear zone. J.

Struct. Geol. 23: 1457-1486.

E. DRUGUET, C.W. PASSCHIER, J. CARRERAS, P. VICTOR, S. DEN BROK (1997). Analysis of a complex high-strain zone at Cap de Creus, Spain. Tectonophysics 280:31-45.

E. DRUGUET (1997). The structure of NE Cap de Creus Peninsula. Relationships with metamorphism and magmatism. Tesi di dottorato. Pag.: 3-78.

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

E. DRUGUET, J. CARRERAS (2006).Analogue modelling of syntectonic leucosomes in migmatitic schists. Journal of Structural Geology 28: 1734-1747.

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A. GRIERA I ARTIGAS (2005). Estructures tectnòniques i la seva relaciò amb la vorticitàt cinematica: casos reales i models. Tesi di dottorato. Pag.: 3-14.

E. GÓMEZ-RIVAS, A. GRIERA, J. CARRERAS Y E. DRUGUET (2006). Influencia de la orientación de la anisotropía en el desarrollo de shear bands: estudio experimental. Geogaceta, 40: 47-50.

N. HAYWARD (1992). Microstructural analysisof the classical spiral garnet porphyroblasts of Southeast Vermont: evidence for non-rotation.

Journal of Metamorphic Geology, 10: 567-587.

HOLCOMB AND LITTLE (2001). A sensitive vorticity gauge using rotated porphyroblasts, and its applications to rocks adjacent to the Alpine Fault, New Zeland. Journal of Structural Geology, 23: 979-989.

D. IACOPINI R. CAROSI, C. MONTOMOLI, C.W. PASSCHIER (2008). Strain analysis and vorticity of flow in the Northern Sardinian Variscan Belt: Recognition of a partitioned oblique deformation event.

Tectonophysics, 446: 77-96.

ILG and KARLSTROM (2000). Porphyroblast inclusion trail geometries in the Grand Canyon: evidence for non-rotation and rotation? Journal of

Structural Geology, 22: 231-243.

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D. JIANG AND J. CLANCY WHITE (1995). Kinematics of rock flow and interpretation of geological structures, with particular reference to shear zone. Journal of Structural Geology, 17: 1249-1265.

M. J. JESSUP, R. D. LAW, C. FRASSI (2007). The Rigid Grain Net (RGN): an alternative method for estimating mean kinematic vorticity number (Wm). Journal of Structural Geology 29: 411-421.

S.E. JOHNSON (1990a). Lack of porphyroblast rotation in the Otago Schists, South Island, New Zeland: implication for crenulation cleavage development, folding and deformation partitioning. Journal of

Metamorphic Geology, 8: 13-30.

S.E. JOHNSON (1990b). Deformation history of the Ontago schists, New Zeland,from progressively developed porphyroblast-matrix microstructure: uplift-collapse orogenesis and its implications. Journal of Structural

Geology, 12: 727-746.

S.E. JOHNSON (1993). Testing models for the development of spiral shaped inclusion trails in garnet porphyroblasts: to rotate or non-rotate, that is the question. Journal of Metamorphic Geology, 11: 635-659.

S.E. JOHNSON, R.H. VERNON (1995a). Inferring the timing of porphyroblast growth in the absence of continuity between inclusion trails and matrix foliations: can it be reliably done? . Journal of Structural

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G.S. LISTER, P.F. WILLIAMS (1983). The partitioning of deformation in flowing rock masses . Tectonophysics, 92: 1-33.

C.W. PASSCHIER and C. SIMPSON (1986). Porphyroclast systems as kinematic indicators. Journal of Structural Geology, 8: 831-843.

C.W. PASSCHIER, P.J.H.R. SPECK (1994). The kinematic interpretation of obliquely-transected porphyroblasts: an example from the Trois Seigneurs Massif, France. Journal of Structural Geology, 16: 971-984.

J.G. RAMSAY (1962). The geometry and mechanics of formation of ‘similar’ type folds. Journal of Geology, 70: 309-327.

S. H. THREAGUS (1985).The relationship between foliation and strain: an experimental investigation: discussion. J. Struct. Geol. Vol. 7, No. 1, pp. 119-121.

S. H. THREAGUS, D. SOKOUTIS (1992). Laboratory modelling of strain variation across rheological boundaries. J. Struct. Geol. Vol. 14, No. 4, pp. 405-424.

S. H. TREAGUS (1999). Are the viscosity ratio of rocks mesurable from cleavage reflaction? Journal of Structural Geology, 21: 895-901.

R.H. VERNON et al. (1993). Growth and deformation of porphyroblasts in the foothills terrane, central Sierra Nevada, California: negotiating a microstructural minefield. Journal of Metamorphic Geology, 11: 203-222.

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