Structures, interference patterns, and strain regime during midcrustal deformation in the Alpi Apuane (Northern Apennines, Italy)
暂无分享,去创建一个
G. Molli | G. Molli | L. Vaselli | L. Vaselli
[1] L. Skjernaa. Rotation and deformation of randomly oriented planar and linear structures in progressive simple shear , 1980 .
[2] N. D’Agostino,et al. Midcrustal shear zones in postorogenic extension: Example from the northern Tyrrhenian Sea , 1998 .
[3] J. Malavieille,et al. Transverse lineation and large-scale structures related to Alpine obduction in Corsica , 1981 .
[4] R. Butler,et al. Can crustal extension be distinguished from thrusting in the internal parts of mountain belts? A case history of the Entrelor shear zone, Western Alps , 1996 .
[5] S. Seno,et al. From finite strain data to strain history: a model for a sector of the Ligurian Alps, Italy , 1998 .
[6] Jonathan W. Mies. Structural analysis of sheath folds in the Sylacauga Marble Group, Talladega slate belt, southern Appalachians , 1993 .
[7] F. Storti. Tectonics of the Punta Bianca promontory: Insights for the evolution of the Northern Apennines‐Northern Tyrrhenian Sea basin , 1995 .
[8] M. Orozco,et al. Internal structure of a collapsed terrain: The Lújar syncline and its significance for the fold- and sheet-structure of the Alborán Domain (Betic Cordilleras, Spain) , 2004 .
[9] R. Holdsworth,et al. The geometry and topology of natural sheath folds: a new tool for structural analysis , 2004 .
[10] T. Bell. Progressive deformation and reorientation of fold axes in a ductile mylonite zone: the woodroffe thrust , 1978 .
[11] W. Owens,et al. Strain analysis of a Northern Apennine shear zone using deformed marble breccias , 1981 .
[12] Luigi Carmignani,et al. Tertiary extensional tectonics in Tuscany (Northern Apennines, Italy) , 1994 .
[13] S. Schmid,et al. Geophysical‐geological transect and tectonic evolution of the Swiss‐Italian Alps , 1996 .
[14] J. Watterson,et al. Stretching fabrics, folds and crustal shortening , 1974 .
[15] J. Burg,et al. Structural evidence for back sliding of the Kohistan arc in the collisional system of northwest Pakistan , 1996 .
[16] D. Flinn. ON FOLDING DURING THREE-DIMENSIONAL PROGRESSIVE DEFORMATION , 1962, Quarterly Journal of the Geological Society of London.
[17] J. Platt. Dynamics of orogenic wedges and the uplift of high-pressure metamorphic rocks , 1986 .
[18] P. Elter,et al. Introduction a la geologie de l'Apennin septentrional , 1975 .
[19] L. Carmignani,et al. Structural Evolution of the Apuane Alps: An Example of Continental Margin Deformation in the Northern Apennines, Italy , 1978, The Journal of Geology.
[20] R. Lacassin,et al. Kilometre-scale sheath fold at Mattmark and implications for transport direction in the Alps , 1985, Nature.
[21] Bernd Leiss,et al. Fabric anisotropy and its influence on physical weathering of different types of Carrara marbles , 2000 .
[22] M. Brandon,et al. Contribution of ductile flow to exhumation of low-temperature, high-pressure metamorphic rocks: San Juan-Cascade nappes, NW Washington State , 1999 .
[23] J. Ramsay. Shear zone geometry: A review , 1980 .
[24] P. R. Cobbold,et al. Development of sheath folds in shear regimes , 1980 .
[25] G. Williams,et al. The geometrical classification of noncylindrical folds , 1979 .
[26] Federico Sani,et al. Cover thrust reactivations related to internal basement involvement during Neogene‐Quaternary evolution of the northern Apennines , 1998 .
[27] L. Skjernaa. Tubular folds and sheath folds: definitions and conceptual models for their development, with examples from the Grapesvare area, northern Sweden , 1989 .
[28] R. D. Dallmeyer,et al. Dating of deformation phases using K-Ar and 40Ar/39Ar techniques: results from the northern apennines , 1986 .
[29] V. Ez. When shearing is a cause of folding , 2000 .
[30] S. Ghosh,et al. Buckling experiments on intersecting fold patterns , 1968 .
[31] D. Grujic,et al. Folds with axes parallel to the extension direction: an experimental study , 1995 .
[32] D. Sanderson. The development of fold axes oblique to the regional trend , 1973 .
[33] R. Holdsworth,et al. The geometry and kinematics of flow perturbation folds , 2002 .
[34] C. Beaumont,et al. Formation, burial and exhumation of basement nappes at crustal scale: a geometric model based on the Western Swiss-Italian Alps , 1997 .
[35] J. Vogl. Late-orogenic backfolding and extension in the Brooks Range collisional orogen, northern Alaska , 2002 .
[36] D. Liotta. D 2 asymmetric folds and their vergence meaning in the Montagnola Senese metamorphic rocks (inner northern Apennines, central Italy) , 2002 .
[37] P. Conti,et al. Microfabric study on the deformational and thermal history of the Alpi Apuane marbles (Carrara marbles), Italy , 2000 .
[38] Luigi Carmignani,et al. Crustal extension in the northern Apennines: The transition from compression to extension in the Alpi Apuane Core Complex , 1990 .
[39] J. Malavieille,et al. Origin of a large-scale fold nappe in the Montagne Noire, Variscan belt, France , 1999 .
[40] B. Leiss,et al. ‘High-temperature’ texture in naturally deformed Carrara marble from the Alpi Apuane, Italy , 2003 .
[41] N. Froitzheim. Formation of recumbent folds during synorogenic crustal extension (Austroalpine nappes, Switzerland) , 1992 .
[42] R. Holdsworth,et al. Early curvilinear fold structures and strain in the Moine of the Glen Garry region, Inverness-shire , 1984, Journal of the Geological Society.
[43] S. Mazzoli,et al. Extensional processes driven by large-scale duplexing in collisional regimes , 1996 .
[44] J. Treagus,et al. Folds and the strain ellipsoid: a general model , 1981 .
[45] V. Picotti,et al. Pliocene and Pleistocene exhumation and uplift of two key areas of the Northern Apennines , 2003 .
[46] G. Giorgetti,et al. Structural and petrological constraints on the tectono‐metamorphic evolution of the Massa Unit (Alpi Apuane, NW Tuscany, Italy) , 2000 .