Criteria for identifying structures related to true crustal extension in orogens

[1]  R. Butler,et al.  Evidence for extension in the western Alpine orogen: the contact between the oceanic Piemonte and overlying continental Sesia units , 1993 .

[2]  A. Michard,et al.  Compression versus extension in the exhumation of the Dora-Maira coesite-bearing unit, Western Alps, Italy , 1993 .

[3]  R. K. O’nions,et al.  Prograde and retrograde thermal histories from the central Swiss Alps , 1992 .

[4]  S. Getty,et al.  Geochronological constraints on ductile deformation, crustal extension, and doming about a basement-cover boundary, New England Appalachians , 1992 .

[5]  S. Getty,et al.  Evidence for extension at the Willimantic Dome, Connecticut; implications for the late Paleozoic tectonic evolution of the New England Appalachians , 1992 .

[6]  L. Jolivet,et al.  Alpine Corsica Metamorphic Core Complex , 1991 .

[7]  J. Dewey,et al.  Subduction and eduction of continental crust: major mechanisms during continent‐continent collision and orogenic extensional collapse, a model based on the south Norwegian Caledonides , 1991 .

[8]  Thomas Reinecke,et al.  Very-high-pressure metamorphism and uplift of coesite-bearing metasediments from the Zermatt-Saas zone, Western Alps , 1991 .

[9]  M. Coward,et al.  Metamorphism and crustal stacking in the North Indian Plate, North Pakistan , 1989 .

[10]  J. Selverstone,et al.  Evidence for east‐west crustal extension in the Eastern Alps: Implications for the unroofing history of the Tauern window , 1988 .

[11]  P. Hancock,et al.  Continental Extensional Tectonics , 1987 .

[12]  J. Platt.  Dynamics of orogenic wedges and the uplift of high-pressure metamorphic rocks , 1986 .

[13]  R. Wintsch,et al.  A Tectonic Model for the Late Paleozoic of Southeastern New England , 1986, The Journal of Geology.

[14]  J. Selverstone,et al.  Petrologic constraints on imbrication, metamorphism, and uplift in the SW Tauern Window, eastern Alps , 1985 .

[15]  R. Cliff.  Isotopic dating in metamorphic belts , 1985, Journal of the Geological Society.

[16]  Alan Bruce Thompson,et al.  Pressure—Temperature—Time Paths of Regional Metamorphism I. Heat Transfer during the Evolution of Regions of Thickened Continental Crust , 1984 .

[17]  W. Ernst,et al.  Mineral parageneses of eclogitic rocks and related mafic schists of the Piemonte ophiolite nappe, Breuil-St. Jacques area, Italian Western Alps , 1978 .

[18]  Martin H. Dodson,et al.  Closure temperature in cooling geochronological and petrological systems , 1973 .

[19]  C. Passchier,et al.  Shear-sense indicators: A review , 1991 .

[20]  G. Lister,et al.  The origin of metamorphic core complexes and detachment faults formed during Tertiary continental extension in the northern Colorado River region, U.S.A. , 1989 .

[21]  M. Séranne,et al.  The Devonian basins of western Norway: tectonics and kinematics of an extending crust , 1987, Geological Society, London, Special Publications.

[22]  B. Burchfiel,et al.  Thin-skinned N-S extension within the convergent Himalayan region: gravitational collapse of a Miocene topographic front , 1987, Geological Society, London, Special Publications.

[23]  J. Burg,et al.  Deformation of leucogranites of the crystalline Main Central Sheet in southern Tibet (China) , 1984 .