Discussion and reply evaluation of petrogenetic models for lachlan fold belt granitoids: Implications for crustal architecture and tectonic models

Australian Journal of Earth Sciences

Volumn 46, Issue 5, 1999, Pages 827-836

  Chappell, B W ^a   White, A J R ^b   Williams, I S ^a   Wyborn, D ^a   Hergt, J M ^b   Woodhead, J D ^b   Collins, W J ^c  

^a AUSTRALIAN NATIONAL UNIVERSITY   (Australia)

^b UNIVERSITY OF MELBOURNE   (Australia)

^c UNIVERSITY OF NEWCASTLE   (Australia)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 85015487163     PISSN: 08120099     EISSN: 14400952     Source Type: Journal    
DOI: 10.1046/j.1440-0952.1999.00742.x     Document Type: Article

References (53)

1. BROWN M., AVERKIN A., MCLELLAN E. L. & SAWYER E. W. 1995. Melt segregation in migmatites. Journal of Geophysical Research 100, 15 655-679.
2. CAS R. A. F. 1983. A review of the palaeogeographic and tectonic development of the Palaeozoic Lachlan Fold Belt of southeastern Australia. Geological Society of Australia Special Publication 10.
3. CHAPPELL B. W. 1979. Granites as images of their source rocks. Geological Society of America, Abstracts with Programs 11, 400.
4. CHAPPELL B. W. 1984. Source rocks of S- and I-type granites in the Lachlan Fold Belt, southeastern Australia. Philosophical Transactions of the Royal Society of London A310, 693-707.
5. CHAPPELL B. W. 1994. Lachlan and New England: Fold belts of contrasting magmatic and tectonic development. Journal and Proceedings of the Royal Society of New South Wales 127, 47-59.
6. CHAPPELL B. W. 1996a. Magma mixing and the production of compositional variation within granite suites: evidence from the granites of southeastern Australia. Journal of Petrology 37, 449-470.
7. CHAPPELL B. W. 1996b. Compositional variation within granite suites of the Lachlan Fold Belt: its causes and implications for the physical state of granitoid magmas. Transactions of the Royal Society of Edinburgh: Earth Sciences 87, 159-170.
8. CHAPPELL B.W. 1998. Tectonic evolution of the eastern Australian fold belts from a granite-based perspective: 1998 Mawson Lecture. The Australian Geologist 109, 24-30.
9. CHAPPELL B. W., BRYANT C. J., WYBORN D., WHITE A. J. R. & WILLIAMS I. S. 1998. High- and low-temperature granites. Resource Geology 48, 225-236.
10. CHAPPELL B. W. & STEPHENS W. E. 1988. Origin of infracrustal (I-type) granite magmas. Transactions of the Royal Society of Edinburgh: Earth Sciences 79, 71-86.
11. CHAPPELL B. W. & WHITE A. J. R. 1992. I- and S-type granites in the Lachlan Fold Belt. Transactions of the Royal Society of Edinburgh: Earth Sciences 83, 1-26.
12. CHAPPELL B. W., WHITE A. J. R. & HINE R. 1988. Granite provinces and basement terranes in the Lachlan Fold Belt, southeastern Australia. Australian Journal of Earth Sciences 35, 505-521.
13. CHAPPELL B. W., WHITE A. J. R. & WYBORN D. 1987. The importance of residual source material (restite) in granite petrogenesis. Journal of Petrology 28, 1111-1138.
14. CHAPPELL B. W., BRYANT C. J., WYBORN D., WHITE A. J. R. & WILLIAMS I. S. 1998. High- and low-temperature I-type granites. Resource Geology 48, 225-235.
15. CHEN Y. D., PRICE R. C. & WHITE A. J. R. 1989. Inclusions in three S-type granites from southeastern Australia. Journal of Petrology 30, 1181-1218.
16. CLEMENS J. D. 1989. The importance of residual source material (restite) in granite petrogenesis: a comment. Journal of Petrology 30, 1313-1316.
17. COLLINSW, J. 1996. S- and I-type granitoids of the western Lachlan fold belt: products of three-component mixing. Transactions of the Royal Society of Edinburgh: Earth Sciences 87, 171-179.
18. COLLINSW, J. 1998. Evaluation of petrogenetic models for Lachlan Fold Belt granitoids: implications for crustal architecture and tectonic models. Australian Journal of Earth Sciences 45, 483-500.
19. COLLINS W. J. & VERNON R. H. 1994. A rift-drift-delamination model of crustal growth: Phanerozoic tectonic development of eastern Australia. Tectonophysics 235, 249-275.
20. DAVIDSON J. P. 1996. Deciphering mantle and crustal signatures in subduction zone magmatism. In: Bebout G. E., Scholl D.W., Kirby S. H. & Platt J. P. eds. Subduction: Top to Bottom, pp. 251-262. American Geophysical Union Monograph 96.
21. FERGUSSON C. L. & CONEY P. J. 1992. Convergence and intraplate deformation in the Lachlan fold Belt of southeastern Australia. Tectonophysics 214, 417-439.
22. GLEN R. A. 1992. Thrust, extensional and strike-slip tectonics in an evolving Palaeozoic orogen—a structural synthesis of the Lachlan Orogen of southeastern Australia. Tectonophysics 214, 341-380.
23. GRAY C. M. 1984. An isotopic mixing model for the origin of granitic rocks in southeastern Australia. Earth and Planetary Science Letters 70, 47-60.
24. GRIFFIN T. J., WHITE A. J. R. & CHAPPELL B. W. 1978. The Moruya Batholith and geochemical contrasts between the Moruya and Jindabyne suites. Journal of the Geological Society of Australia 25, 235-247.
25. HANSON R. B. 1996. Hydrodynamics of magmatic and meteoric fluids in the vicinity of granitic intrusions. Transactions of the Royal Society of Edinburgh: Earth Sciences 87, 251-260.
26. KEAY S., COLLINS W. J. & MC CULLOCH M. T. 1997. A three-component Sr-Nd isotopic mixing model for granitoid genesis, Lachlan fold belt, eastern Australia. Geology 25, 307-310.
27. MAAS R., NICHOLLS I. A. & LEGG C. 1997. Igneous and metamorphic enclaves in the S-type Deddick Granodiorite, Lachlan Fold Belt, SE Australia: petrographic, geochemical and Nd-Sr isotope evidence for crustal melting and magma mixing. Journal of Petrology 38, 815-841.
28. MASON P. R. D., DOWNES H., THIRLWELL M. F., SEGHEDI I., SZAKACS A., LOWRY D. & MATTEY D. 1996. Crustal assimilation as a major process in the East Carpathian Neogene and Quaternary continental margin. Journal of Petrology 37, 927-959.
29. MC CULLOCH M. T. & CHAPPELL B. W. 1982. Nd isotopic characteristics of S- and I-type granites. Earth and Planetary Science Letters 58, 51-64.
30. MC CULLOCH M. T. & WOODHEAD J. D. 1993. Lead isotopic evidence for deep crustal scale fluid transport during granite petrogenesis. Geochimica et Cosmochimica Acta 57, 659-674.
31. MEANS W. D. & PARK Y. 1994. New experimental approach to understanding igneous texture. Geology 22, 323-326.
32. PITCHER W. S. 1982. Granite type and tectonic environment. In: Hsu K. J. ed. Mountain Building Processes, pp. 19-40. Academic Press, London.
33. POLI G., TOMMASINI S. & HALLIDAY A. N. 1996. Trace element and isotopic exchange during acid-basic magma interaction processes. Transactions of the Royal Society of Edinburgh: Earth Sciences 87, 225-232.
34. RODRIGUEZ L. G. 1998. Systematic variation within the Tuross Head Tonalite: Product of magma mixing and fractional crystallisation. BSc (Hons) thesis, University of Newcastle, Newcastle (unpubl.).
35. ROSSITER A. G. & GRAY C. M. 1996. Magma mixing and the origin of S- and I-type granites. Geological Society of Australia Abstracts 41, 372.
36. SAWYER E. W. 1994. Melt segregation in the continental crust. Geology 22, 1019-1022.
37. SAWYER E. W. 1996. Melt-segregation and magma flow in migmatites: implications for the generation of granitic magmas. Transactions of the Royal Society of Edinburgh: Earth Sciences 87, 85-94.
38. SCHEIBNER E. 1989. The tectonics of New South Wales in the second decade of application of the plate tectonics paradigm. Journal and Proceedings of the Royal Society of New South Wales 122, 35-74.
39. SCHEIBNER E. 1992. Influence of detachment-related passive margin geometry on subsequent active margin dynamics: applied to the Tasman fold belt system. Tectonophysics 214, 401-416.
40. VERNON R. H. 1983. Restite, xenoliths and microgranitoid enclaves in granites. Journal and Proceedings of the Royal Society of New South Wales 116, 77-103.
41. VERNON R. H. 1990. Crystallization and hybridism in microgranitoid enclave magmas: microstructural evidence. Journal of Geophysical Research 95, 17849-17859.
42. WALL V. J., CLEMENS J. D. & CLARKE D. B. 1987. Models for granitoid evolution and source compositions. Journal of Geology 95, 731-749.
43. WATSON E. B. & HARRISON T. M. 1983. Zircon saturation revisited: temperature and composition effects in a variety of crustal magma types. Earth and Planetary Science Letters 64, 295-304.
44. WHITE A. J. R. & CHAPPELL B. W. 1977. Ultrametamorphism and granitoid genesis. Tectonophysics 43, 7-22.
45. WHITE A. J. R., WILLIAMS I. S. & CHAPPELL B. W. 1976. The Jindabyne Thrust and its tectonic, physiographic and petrogenetic significance. Journal of the Geological Society of Australia 23, 105-112.
46. WIEBE R. A. 1996. Mafic-silicic layered intrusions: the role of basaltic injections on magmatic processes and the evolution of silicic magma chambers. Transactions of the Royal Society of Edinburgh: Earth Sciences 87, 233-242.
47. WIEBE R. A. & COLLINS W. J. 1998. Depositional features and stratigraphic sections in granitic plutons: implications for the emplacement and crystallization of granitic magma chambers. Journal of Structural Geology 20, 1273-1289.
48. WILLIAMS I. S. 1995. Zircon analysis by ion microprobe: the case of the eastern Australian granites. In: Leon T. Silver 70th Birthday Symposium and Celebration, pp. 27-31. California Institute of Technology, Pasadena.
49. WILLIAMS I. S., CHAPPELL B. W., CHEN Y. D. & CROOK K. A. W. 1992. Inherited and detrital zircons—vital clues to the granite protoliths and early igneous history of southeastern Australia. Transactions of the Royal Society of Edinburgh: Earth Sciences 83, 503.
50. WILLIAMS I. S., CHEN Y., CHAPPELL B.W. & COMPSTON W. 1988. Dating the sources of Bega Batholith granites by ion microprobe. Geological Society of Australia Abstracts 21, 424.
51. WILLIAMS I. S., COMPSTON W., CHAPPELL B. W. & CROOK K. A. W. 1990. Untangling the sources of granites by dating inherited zircons. Geological Society of Australia Abstracts 27, 112.
52. WYBORN D. 1992. The tectonic significance of Ordovician magmatism in the eastern Lachlan Fold Belt. Tectonophysics 214, 177-192.
53. WYBORN L. A. I. & CHAPPELL B. W. 1983. Chemistry of the Ordovician and Silurian greywackes of the Snowy Mountains, southeastern Australia: an example of chemical evolution of sediments with time. Chemical Geology 39, 81-92.