Reply to comment by Brian Stevens on "Evidence and timing of crustal extension versus shortening in the early tectonothermal evolution of a Proterozoic continental rift sequence at Broken Hill, Australia"

Tectonics

Volumn 25, Issue 4, 2006, Pages

  Gibson, G M ^a   Peljo, M ^a   Chamberlain, T ^b  

^a GEOSCIENCE AUSTRALIA   (Australia)

^b Department of Natural Resources Mines and Energy Indooroopilly Science Centre ^*  (Australia)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 33845728068     PISSN: 02787407     EISSN: None     Source Type: Journal    
DOI: 10.1029/2005TC001934     Document Type: Note

References (27)

1. Abroad, R., and C. J. L. Wilson (1981), Uranium and boron distributions related to metamorphic microstructure evidence for metamorphic fluid activity, Contrib. Mineral. Petrol., 76, 24-32.
2. Barovich, K., and M. Hand (2004), A geochemical and isotopic perspective on the early development of the Willyama Supergroup, Cumamona Province, Geol. Soc. Anst. Abstr., 73, 144.
3. Barton, M. D., and R. B. Hanson (1989), Magmatism and the development of low-pressure metamorphic belts: Implications from the western United States and thermal modelling, Geol. Soc. Am. Bull., 101, 1051-1065.
4. Corbett, G. J. (1979), Structure, metamorphism and stratigraphy of part of the Willyama Complex near Yanco Glen, N. S. W., Ph.D. thesis, Univ. of N. S. W., Kensington, Australia.
5. Davis, G. A., and G. S. Lister (1988), Detachment faulting in continental extension; perspectives from the southwestern U.S. Cordillera, in Processes in Continental Lithosphere Deformation, edited by S. P. Clark, B. C. Burchfiel, and J. Suppe, Spec. Pap. Geol. Soc. of Am., 218, 133-139.
6. De Yoreo, J. J., D. R. Lux, and C. V. Guidotti (1991), Thermal modelling in low-pressure/high-temperature metamorphic belts, Tectonophysics, 188, 209-238.
7. Forbes, C. J., P. G. Betts, and G. S. Lister (2004), Synchronous development of type 2 and type 3 fold interference pattern: Evidence for recumbent sheath folds in the Allendale area, Broken Hill, NSW, Australia, J. Struct. Geol., 26, 113-126.
8. Frost, B. R., S. M. Swapp, and R. W. Gregory (2005), Prolonged existence of sulphide melt in the Broken Hill orebody, New South Wales, Australia, Can. Mineral., 43, 479-493.
9. Gibson, G. M., and A. P. Nutman (2004), Detachment faulting and bimodal magmatism in the Palaeoproterozoic Willyama Supergroup, south-central Australia: Keys to recognition of a multiply deformed Precambrian metamorphic core complex, J. Geol. Soc. London, 161, 55-66.
10. Gibson, G. M., and A. P. Nutman (2005), Reply to discussion of Detachment faulting and bimodal magmatism in the Palaeoproterozoic Willyama Supergroup, south-central Australia: Keys to recognition of a multiply-deformed Precambrian metamorphic core complex, J. Geol. Soc. London, 162, 411-416.
11. Gibson, G. M., M. Peljo, and T. Chamberlain (2004), Evidence and timing of crustal extension versus shortening in the early tectonothermal evolution of a Proterozoic continental rift sequence at Broken Hill, Australia, Tectonics, 23, TC5012, doi:10.1029/2003TC001552.
12. Hobbs, B. E., N. J. Archibald, M. A. Etheridge, and V. J. Wall (1984), Tectonic history of the Broken Hill Block, Australia, in Precambrian Tectonics Illustrated, edited by A. Kroner and R. Greiling, pp. 353-368, E. Scheizerbart'sche, Stuttgart, Germany.
13. Laing, W. P. (1996), Volcanic-related origin of the Broken Hill Pb+Zn+Ag deposit, Australia, in New Developments, in Broken Hill Type Deposits: CODES Key Center, Spec. Publ. 1, edited by J. Pongratz and G. J. Davidson, pp. 53-66, Univ. of Tasmania, Hobart.
14. Laing, W. P., R. W. Marjoribanks, and R. W. R. Rutland (1978), Structure of the Broken Hill mine area and its significance for the genesis of the orebodies, Econ. Geol., 73, 1112-1136.
15. Marjoribanks, R. W., R. W. R. Rutland, R. A. Glen, and W. P. Laing (1980), The structure and tectonic evolution of the Broken Hill region, Australia, Precambrian Res., 13, 209-240.
16. Nutman, A. P., and K. Ehlers (1998), Evidence for multiple Palaeoproterozoic thermal events and magmatism adjacent to the Broken Hill Pb-Zn-Ag orebody, Australia, Precambrian Res., 90, 203-238.
17. Page, R. W., B. P. J. Stevens, and G. M. Gibson (2005), Geochronology of the sequence hosting the Broken Hill Pb-Zn-Ag orebody, Australia, Econ. Geol., 100, 633-661.
18. Powell, R., and J. Downes (1990), Garnet porphyroblast-bearing leucosomes in metapelites: Mechanisms, phase diagrams and an example from Broken Hill, Australia, in High-Temperature Metamorphism and Crystal Anatexis, edited by J. R. Ashworth and M. Brown, pp. 105-123, CRC Press, Boca Raton, Fia.
19. Stevens, B. P. J. (1998), The origins of Broken Hill rock types and their relevance to mineralization (abstract), Broken Hill Exploration Initiative, October 1998, Rec. 1998/25, pp. 109-114, Aust. Geol. Surv. Org., Canberra.
20. Stevens, B. P. J. (2006), Comment on "Evidence and timing of crustal extension versus shortening in the early tectonothermal evolution of a Proterozoic continental rift sequence at Broken Hill, Australia" by G. M. Gibson, M. Peljo, and T. Chamberlain, Tectonics, 25, TC4009, doi:10.1029/2005TC001853.
21. Stevens, B. P. J., R. G. Barnes, R. E. Brown, W. J. Stroud, and I. L. Willis (1988), The Willyama Supergroup in the Broken Hill and Euriowie blocks, New South Wales, Precambrian Res., 40/41, 297-327.
22. Swapp, S. M., and B. R. Frost (2003), Evidence for high-pressure metamorphism in the granulites of the Broken Hill area, Rec. 2003/13, pp. 174-175, Geosci. Aust., Canberra.
23. Wernicke, B. (1985), Uniform-sense normal simple shear of the continental lithosphere, Can. J. Earth Sci., 22, 108-125.
24. White, S. H., E. Rothery, A. L. W. Lips, and J. R. Barclay (1995), Broken Hill area, Australia, as a Proterozoic thrust and fold belt: Implications for the Broken Hill base-metal deposit, Trans. Inst. Min. Metall., Sect. B, 104, B1-B17.
25. White, S. H., E. Rothery, A. L. W. Lips, and J. R. Barclay (1996), Reply to Stevens discussion of "Broken Hill area, Australia, as a Proterozoic thrust and fold belt: Implications for the Broken Hill basemetal deposit", Trans. Inst. Min. Metall., Sect. B, 105, B90-B98.
26. Willis, I. L., R. E. Brown, W. J. Stroud, and B. P. J. Stevens (1983), The Early Proterozoic Willyama Supergroup: Stratigraphic subdivisions and interpretation of high-to low-grade metamorphic rocks in the Broken Hill Block, New South Wales, Geol. Soc. Aust. J., 30, 195-224.
27. Wilson, C. J. L., and R. Powell (2001), Strain localisation and high-grade metamorphism at Broken Hill, Australia: A view from the Southern Cross area, Tectonophysics, 335, 193-210.