Crustal architecture during the early Mesoproterozoic Hiltaba-related mineralisation event: are the Gawler Range Volcanics a foreland basin fill?
暂无分享,去创建一个
B. Wade | M. Hand | N. Direen | J. Payne | K. Barovich | A. Reid | M. Szpunar
[1] B. Wade,et al. Temporal constraints on the timing of high-grade metamorphism in the northern Gawler Craton: implications for assembly of the Australian Proterozoic , 2008 .
[2] P. Betts,et al. 1600–1500 Ma hotspot track in eastern Australia: implications for Mesoproterozoic continental reconstructions , 2007 .
[3] A. Belperio,et al. Prominent Hill: A Hematite-Dominated, Iron Oxide Copper-Gold System , 2007 .
[4] M. Hand,et al. Tectonic Framework and Evolution of the Gawler Craton, Southern Australia , 2007 .
[5] N. Direen,et al. Regional Crustal Setting of Iron Oxide Cu-Au Mineral Systems of the Olympic Dam Region, South Australia: Insights from Potential-Field Modeling , 2007 .
[6] M. Hand,et al. Timing of Proterozoic metamorphism in the southern Curnamona Province: implications for tectonic models and continental reconstructions , 2007 .
[7] B. Wade,et al. Evidence for Early Mesoproterozoic Arc Magmatism in the Musgrave Block, Central Australia: Implications for Proterozoic Crustal Growth and Tectonic Reconstructions of Australia , 2006, The Journal of Geology.
[8] B. Stevens,et al. Correlation of Olary and Broken Hill Domains, Curnamona Province: Possible Relationship to Mount Isa and Other North Australian Pb-Zn-Ag-Bearing Successions , 2005 .
[9] R. Powell,et al. Spatially‐focussed melt formation in aluminous metapelites from Broken Hill, Australia , 2004 .
[10] Peter G. Betts,et al. Evolution of the Mount Woods Inlier, northern Gawler Craton, Southern Australia: an integrated structural and aeromagnetic analysis , 2003 .
[11] O. Oncken,et al. Growth of the Central Andean Plateau by Tectonic Segmentation Is Controlled by the Gradient in Crustal Shortening , 2003, The Journal of Geology.
[12] T. Jordan,et al. The structural and stratigraphic evolution of the La Rioja basin, Argentina , 2002 .
[13] R. Holdsworth,et al. Continental Reactivation and Reworking , 2001 .
[14] D. Foster,et al. Australia: Implications for Mesoproterozoic and Neoproterozoic tectonics of East Gondwana and Rodinia , 1998 .
[15] P. DeCelles,et al. Foreland basin systems , 1996 .
[16] R. Creaser. Neodymium isotopic constraints for the origin of Mesoproterozoic felsic magmatism, Gawler Craton, South Australia , 1995 .
[17] James P. Johnson. The geochronology and radiogenic isotope systematics of the Olympic Dam copper-uranium-gold-silver deposit, South Australia , 1993 .
[18] R. Powell,et al. Metamorphism in the Olary Block, South Australia: compression with cooling in a Proterozoic fold belt , 1987 .
[19] B. Stevens,et al. Post‐depositional history of the Willyama Supergroup in the Broken Hill Block, NSW , 1986 .
[20] C. Beaumont,et al. Geodynamic Models of Convergent Margin Tectonics: Transition from Rifted Margin to Overthrust Belt and Consequences for Foreland-Basin Development , 1986 .
[21] B. Wade,et al. Timing of Proterozoic high-grade metamorphism in the Barossa Complex, southern South Australia: exploring the extent of the 1590 Ma event Barossa Complex, 1590 Ma metamorphic event , 2007 .
[22] E. Bastrakov,et al. Metadata for Gawler Craton iron oxide Cu-Au (-U) potential map , 2006 .
[23] I. Buick,et al. Tectonic evolution of the Reynolds-Anmatjira Ranges: a case study in terrain reworking from the Arunta Inlier, central Australia , 2001, Geological Society, London, Special Publications.
[24] L. Cabrera,et al. Syntectonic intraformational unconformities in alluvial fan deposits, eastern Ebro Basin margins (NE Spain) , 1986 .