Discussion Sequence and kinematics of multiple deformation around Taemas Bridge, Eastern Lachlan Fold Belt, New South Wales
2003; Taylor & Francis; Volume: 50; Issue: 5 Linguagem: Inglês
10.1111/j.1440-0952.2003.01025.x
ISSN1440-0952
Autores Tópico(s)earthquake and tectonic studies
ResumoAustralian Journal of Earth SciencesVolume 50, Issue 5 p. 827-833 Discussion Sequence and kinematics of multiple deformation around Taemas Bridge, Eastern Lachlan Fold Belt, New South Wales G. H. Packham, G. H. Packham School of Geosciences, University of Sydney, NSW 2006, Australia ( [email protected]).Search for more papers by this author G. H. Packham, G. H. Packham School of Geosciences, University of Sydney, NSW 2006, Australia ( [email protected]).Search for more papers by this author First published: 11 December 2003 https://doi.org/10.1111/j.1440-0952.2003.01025.xCitations: 4Read the full textAboutPDF ToolsRequest permissionExport citationAdd to favoritesTrack citation ShareShare Give accessShare full text accessShare full-text accessPlease review our Terms and Conditions of Use and check box below to share full-text version of article.I have read and accept the Wiley Online Library Terms and Conditions of UseShareable LinkUse the link below to share a full-text version of this article with your friends and colleagues. Learn more.Copy URL Share a linkShare onEmailFacebookTwitterLinkedInRedditWechat References Brunker R. L. & Offenberg A. C. 1970. Goulburn 1:250 000 Geological Sheet, SI/55–12. Geological Survey of New South Wales, Sydney. Conolly J. R. 1965. The stratigraphy of the Hervey Group in central New South Wales. Journal and Proceedings of the Royal Society of New South Wales 98, 37–83. Durney D. W. 2000. Background discussion for the Taemas and Murga stops. In: Scott M. M. ed. Heterogeneous Ductile to Brittle Structures in the Eastern Lachlan Fold Belt, 15th Australian Geological Convention Field Guide FA2, pp. 15–22. Geological Society of Australia, Sydney. Durney D. & Hood D. 2002. Relation of penetrative cleavage to the tectonic Y-axis in an area of non-coaxial shortening in the YZ-plane, Taemas, New South Wales. In: Lebit H., Luneburg C., Hudleston P. & Ramsay J. eds. Three-dimensional Flow, Fabric Development and Strain in Deformed Rocks and Significance for Mountain Building Processes: New Approaches, pp. 27–28. Geological Society of America Penrose Conference, Monte Verita, Abstract Volume. Durney D. W. & Kisch H. J. 1994. A field classification and intensity scale for first generation cleavages. AGSO Journal of Australian Geology & Geophysics 15, 257–295. Fleuty M. J. 1964. The description of folds. Proceedings of the Geologists Association 75, 461–492. Glen R. A., Korsch R. J., Direen N. G., Jones L. E. A., Johnstone D. W., Lawrie K. C., Finlayson D. M. & Shaw R. D. 2002. Crustal structure of the Ordovician Macquarie Arc, Eastern Lachlan Orogen, based on seismic-reflection profiling. Australian Journal of Earth Sciences 49, 323–348. Glen R. A. & Watkins J. J. 1999. Implications of Middle Devonian deformation of the eastern part of the Hill End Trough, Lachlan Orogen, New South Wales. Australian Journal of Earth Sciences 46, 35–52. Hood D. I. A. & Durney D. W. 2002. Sequence and kinematics of multiple deformation around Taemas Bridge, Eastern Lachlan Fold Belt, New South Wales. Australian Journal of Earth Sciences 49, 291–309. Johnston A. J., Pogson D. J., Thomas O. D., Watkins J. J. & Glen R. A. 2001. Boorowa 1:100 000 Geological Sheet 8629 (provisional 1st edition). Geological Survey of New South Wales, Orange. Lu J. & Seccombe P. K. 1993. Fluid evolution in a slate-belt gold deposit. Mineralium Deposita 28, 310–323. Lu J., Seccombe P. K. & Eldridge C. S. 1996a. SHRIMP S-isotope evidence for fluid mixing during gold mineralization in a slate-belt gold deposit (Hill, End, New South Wales, Australia). Chemical Geology 127, 229–240. Lu J., Seccombe P. K., Foster D. & Andrew A. S. 1996b. Timing of mineralization and source fluids in a slate-belt auriferous vein system, Hill End goldfield, NSW, Australia: evidence from 40Ar/39Ar dating and O- and H-isotopes. Lithos 38, 147–165. Lu J., Seccombe P. K. & Walshe J. L. 1996c. Conditions on chlorite growth in the Hill End Goldfield, New South Wales, Australia: some predictions and evaluations. Canadian Mineralogist 34, 9–21. Lyons P., Raymond O. L. & Duggan M. B. 2000. Forbes 1:250 000 Geological Sheet SI55-7 Explanatory Notes ( 2nd edition). Australian Geological Survey Organisation Record 2000/20. Mawson R. & Talent J. A. 2000. The Devonian of eastern Australia: stratigraphic alignments, stages and series boundaries and the transgression-regression patterns re-considered. Courier Forschungsinstitut Senckenberg 225, 243–270. Meakin N. S. & Morgan E. J. 1999. Dubbo 1:250 000 Geological Sheet SI/55–4 Explanatory Notes ( 2nd edition). Geological Survey of New South Wales, Sydney. Owen M. & Wyborn D. 1979. Geology and Geochemistry of the Tantangara and Brindabella 1:100 000 Sheet Areas. Bureau of Mineral Resources Bulletin204. Packham G. H. 1999. Radiometric evidence for Middle Devonian inversion of the Hill End Trough, northeast Lachlan Fold Belt. Australian Journal of Earth Sciences 46, 23–35. Pickett J. W. 1993. A Late Devonian xiphosuran from near Parkes, New South Wales. Association of Australasian Palaeontologists Memoir 15, 279–287. Powell C. McA & Edgecombe D. R. 1978. Mid-Devonian movements in the northeastern Lachlan Fold Belt. Journal of the Geological Society of Australia 25, 165–184. Powell C. McA, Edgecombe D. R., Henry N. M. & Jones J. G. 1976. Timing of regional deformation of the Hill End Trough: a reassessment. Journal of the Geological Society of Australia 23, 407–421. Powell C. McA, Fergusson C. L. & Williams A. J. 1980. Structural relationships across the Lambian Unconformity in the Hervey Range – Parkes area, N.S.W. Proceedings of the Linnean Society of New South Wales 104, 195–210. Price N. J. & Cosgrove J. W. 1990. Analysis of Geological Structures. Cambridge University Press, Cambridge. Raymond O. L., Duggan M. B., Lyons P., Scott M. M., Sherwin L., Wallace D. A., Krynen J. P., Young G. C., Wyborn D., Glen R. A., Percival I. G. & Leys M. 2001. Forbes 1:250 000 Geological Sheet Si55-7 ( 2nd edition). Australian Geological Survey Organisation Canberra and Geological Survey of New South Wales, Sydney. Raymond O. L. & Pogson D. J. 1998. Bathurst 1:250 000 Geological Sheet, SI/55–8 ( 2nd edition). Australian Geological Survey Organisation Canberra and Geological Survey of New South Wales, Sydney. Scheibner E. 1976. Explanatory Notes on the Tectonic Map of New South Wales. Geological Survey of New South Wales, Sydney. Scheibner E. & Basden H. eds. 1998. Geology of New South Wales—Synthesis, 2, Geological Evolution. Geological Survey of New South Wales Memoir Geology13 (2). Scott M. M. ed. 2000. Heterogeneous ductile to brittle structures in the Eastern Lachlan Fold Belt, 15th Australian Geological Convention Field Guide FA2. Geological Society of Australia, Sydney. Seccombe P. K. & Hicks M. N. 1989. The Hill End goldfield, NSW, Australia—early metamorphic deposition of auriferous quartz veins. Mineralogy and Petrology 40, 257–273. Seccombe P. K., Lu J., Andrew A. S., Gulson B. L. & Mizon K. J. 1993. Nature and evolution of metamorphic fluids associated with turbidite-hosted gold deposits: Hill End goldfield, NSW, Australia. Mineralogical Magazine 57, 423–436. Tucker R. D., Bradley D. C., Ver Straeten C. A., Harris A. G., Ebert J. R. & McCutcheon S. R. 1998. New U–Pb zircon ages and the duration and division of Devonian time. Earth and Planetary Science Letters 158, 175–186. Windh J. 1995. Saddle reef and related gold mineralization, Hill End gold field, Australia: evolution of an auriferous vein system during progressive deformation. Economic Geology 90, 1764–1775. Young G. C. & Turner S. 2001. Devonian microvertebrates and marine–nonmarine correlation in East Gondwanaland. Courier Forschungsinstitut Senckenberg 223, 453–470. Citing Literature Volume50, Issue5October 2003Pages 827-833 ReferencesRelatedInformation
Referência(s)