Ophiolite accretion in the Lachlan Orogen, Southeastern Australia

[1]  D. Gray,et al.  Evolution of the boundary between the western and central Lachlan Orogen: Implications for Tasmanide tectonics , 2003 .

[2]  D. Gray,et al.  Blueschist metamorphism during accretion in the Lachlan Orogen, south‐eastern Australia , 2002 .

[3]  D. Gray,et al.  Occurrence and significance of blueschist in the southern Lachlan Orogen , 2002 .

[4]  M. Gerbault.  At what stress level is the central Indian Ocean lithosphere buckling , 2000 .

[5]  D. Gray,et al.  Evolution and Structure of the Lachlan Fold Belt (Orogen) of Eastern Australia , 2000 .

[6]  D. Gray,et al.  Chronology of deformation within the turbidite‐dominated, Lachlan orogen: Implications for the tectonic evolution of eastern Australia and Gondwana , 1999 .

[7]  D. Gray,et al.  Character and kinematics of faults within the turbidite-dominated Lachlan Orogen: implications for tectonic evolution of eastern Australia: Reply , 1998 .

[8]  C. Fergusson.  Cambrian‐Silurian oceanic rocks, upper Howqua River, eastern Victoria: Tectonic implications , 1998 .

[9]  W. Collins.  Evaluation of petrogenetic models for Lachlan Fold Belt granitoids: Implications for crustal architecture and tectonic models , 1998 .

[10]  J. Royer,et al.  The Motion and Boundary Between the Capricorn and Australian Plates , 1997 .

[11]  E. Gnos,et al.  Rapid emplacement of the Oman ophiolite: Thermal and geochronologic constraints , 1996 .

[12]  G. Kimura,et al.  Peeling oceanic crust in subduction zones , 1995 .

[13]  P. Coney,et al.  Convergence and intraplate deformation in the Lachlan Fold Belt of Southeastern Australia , 1992 .

[14]  M. E. Mackay,et al.  Large‐scale duplexes within the New Britain Accretionary Wedge: A possible example of accreted ophiolitic slivers , 1992 .

[15]  D. Gray,et al.  Intracrustal detachments and implications for crustal evolution within the Lachlan fold belt, southeastern Australia , 1991 .

[16]  D. Gray,et al.  Deformation in the Ballarat Slate Belt, central Victoria, and implications for the crustal structure across southeast Australia , 1991 .

[17]  A. Crawford,et al.  Petrogenesis of Victorian Cambrian Tholeiites and Implications for the Origin of Associated Boninites , 1987 .

[18]  E. Honza,et al.  Incipient subduction and deduction along the eastern margin of the Japan Sea , 1985 .

[19]  A. Crawford,et al.  Petrology and geochemistry of Cambrian boninites and low-Ti andesites from Heathcote, Victoria , 1985 .

[20]  A. Crawford,et al.  Nd-Sr isotopic and geochemical systematics in Cambrian boninites and tholeiites from Victoria, Australia , 1984 .

[21]  S. Lippard,et al.  Ophiolites and Oceanic Lithosphere , 1984 .

[22]  A. Crawford,et al.  The association boninite low‐ti andesite‐tholeiite in the heathcote greenstone belt, Victoria; ensimatic setting for the early lachlan fold belt , 1984 .

[23]  E. Moores.  origin and emplacement of ophiolites , 1982 .

[24]  A. Vandenberg.  The Tasman Fold Belt System in Victoria , 1978 .

[25]  J. Dewey,et al.  Origin and Emplacement of the Ophiolite Suite: Appalachian Ophiolites in Newfoundland , 1971 .

[26]  R. Coleman.  Plate tectonic emplacement of upper mantle peridotites along continental edges , 1971 .

[27]  J. Brown,et al.  Geological Survey of Victoria , 1866, Nature.

[28]  D. Gray,et al.  Tethyan- and Cordilleran-type ophiolites of eastern Australia: implications for the evolution of the Tasmanides , 2003, Geological Society, London, Special Publications.

[29]  R. Coleman.  Prospecting for ophiolites along the California continental margin , 2000 .

[30]  L. Kellogg,et al.  Tethyan ophiolites, mantle convection, and tectonic "historical contingency": A resolution of the "ophiolite conundrum" , 2000 .

[31]  A. Nicolas,et al.  Ophiolites and Oceanic Crust: New Insights from Field Studies and the Ocean Drilling Program , 2000 .

[32]  M. Ford,et al.  Orogeny through time , 1997 .

[33]  D. Gray.  Tectonics of the southeastern Australian Lachlan Fold Belt: structural and thermal aspects , 1997, Geological Society, London, Special Publications.

[34]  Y. Isozaki,et al.  Well-preserved underplating structure of the jadeitized Franciscan complex, Pacheco Pass, California , 1996 .

[35]  P. Schmidt,et al.  Australian Palaeozoic palaeomagnetism and tectonics—II. A revised apparent polar wander path and palaeogeography , 1990 .

[36]  P. Coney,et al.  The regional tectonics of the Tasman orogenic system, eastern Australia , 1990 .

[37]  J. Sample,et al.  Structural style and kinematics of an underplated slate belt, Kodiak and adjacent islands, Alaska , 1987 .

[38]  N. Lundberg,et al.  Scaly fabrics from Deep Sea Drilling Project cores from forearcs , 1986 .

[39]  J. Moore,et al.  Cataclastic deformation in accretionary wedges: Deep Sea Drilling Project Leg 66, southern Mexico, and on-land examples from Barbados and Kodiak Islands , 1986 .

[40]  John F. Casey,et al.  Initiation of subduction zones along transform and accreting plate boundaries, triple-junction evolution, and forearc spreading centres—implications for ophiolitic geology and obduction , 1984, Geological Society, London, Special Publications.