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<title>UTas ePrints - Chemical U - Th - Pb monazite dating and the Proterozoic history of King Island, southeast Australia</title>
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<meta content="Berry, R.F." name="eprints.creators_name" />
<meta content="Holm, O.H." name="eprints.creators_name" />
<meta content="Steele, D.A." name="eprints.creators_name" />
<meta content="Ron.Berry@utas.edu.au" name="eprints.creators_id" />
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<meta content="Chemical U - Th - Pb monazite dating and the
Proterozoic history of King Island, southeast Australia" name="eprints.title" />
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<meta content="geochronology, Grenville, King Island, metamorphism, monazite, Rodinia, Tasmania,
uranium, lead dating, Wickham Orogeny." name="eprints.keywords" />
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<meta content="The Proterozoic stratigraphy of Tasmania has some common aspects with South Australia but the
Wickham Orogeny (760 Ma) has been a major contrasting feature. We have used chemical U-Th-Pb
monazite dating to clarify the age relationships in western King Island, which is the key area for the
definition of the Wickham Orogeny. New monazite dates demonstrate that the major regional
deformation on King Island occurred at 1290 Ma. The Wickham Orogeny is reinterpreted as a local
deformation restricted to the contact aureole of the Cape Wickham granite. The Wickham Orogeny in
Tasmania may correlate with minor felsic volcanism in the Adelaide Fold Belt, and low-angle
unconformities in the Neoproterozoic of northwest Tasmania. The metamorphism on King Island is
synchronous with Grenville-age (1300 Ma) orogenic events recognised in central and western Australia.
The nearest known examples to Tasmania are in the Musgrave Ranges. Monazite dating of western King
Island provides the first direct evidence for Mesoproterozoic basement in southeastern Australia and
has major implications for Rodinia reconstructions." name="eprints.abstract" />
<meta content="2005" name="eprints.date" />
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<meta content="The Proterozoic stratigraphy of Tasmania has some common aspects with South Australia but the
Wickham Orogeny (760 Ma) has been a major contrasting feature. We have used chemical U-Th-Pb
monazite dating to clarify the age relationships in western King Island, which is the key area for the
definition of the Wickham Orogeny. New monazite dates demonstrate that the major regional
deformation on King Island occurred at 1290 Ma. The Wickham Orogeny is reinterpreted as a local
deformation restricted to the contact aureole of the Cape Wickham granite. The Wickham Orogeny in
Tasmania may correlate with minor felsic volcanism in the Adelaide Fold Belt, and low-angle
unconformities in the Neoproterozoic of northwest Tasmania. The metamorphism on King Island is
synchronous with Grenville-age (1300 Ma) orogenic events recognised in central and western Australia.
The nearest known examples to Tasmania are in the Musgrave Ranges. Monazite dating of western King
Island provides the first direct evidence for Mesoproterozoic basement in southeastern Australia and
has major implications for Rodinia reconstructions." name="DC.description" />
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<h1 class="ep_tm_pagetitle">Chemical U - Th - Pb monazite dating and the Proterozoic history of King Island, southeast Australia</h1>
<p style="margin-bottom: 1em" class="not_ep_block"><span class="person_name">Berry, R.F.</span> and <span class="person_name">Holm, O.H.</span> and <span class="person_name">Steele, D.A.</span> (2005) <xhtml:em>Chemical U - Th - Pb monazite dating and the Proterozoic history of King Island, southeast Australia.</xhtml:em> Australian Journal of Earth Sciences, 52 . pp. 461-471. ISSN 0812-0099</p><p style="margin-bottom: 1em" class="not_ep_block"></p><table style="margin-bottom: 1em" class="not_ep_block"><tr><td valign="top" style="text-align:center"><a href="http://eprints.utas.edu.au/696/1/berryetal_KingIsland.pdf"><img alt="[img]" src="http://eprints.utas.edu.au/style/images/fileicons/application_pdf.png" border="0" class="ep_doc_icon" /></a></td><td valign="top"><a href="http://eprints.utas.edu.au/696/1/berryetal_KingIsland.pdf"><span class="ep_document_citation">PDF</span></a> - Full text restricted - Requires a PDF viewer<br />1899Kb</td><td><form method="get" accept-charset="utf-8" action="http://eprints.utas.edu.au/cgi/request_doc"><input value="708" name="docid" accept-charset="utf-8" type="hidden" /><div class=""><input value="Request a copy" name="_action_null" class="ep_form_action_button" onclick="return EPJS_button_pushed( '_action_null' )" type="submit" /> </div></form></td></tr><tr><td valign="top" style="text-align:center"><a onmouseover="EPJS_ShowPreview( event, 'doc_preview_709' );" onmouseout="EPJS_HidePreview( event, 'doc_preview_709' );" href="http://eprints.utas.edu.au/696/2/Berry_KingIsland.pdf"><img alt="[img]" src="http://eprints.utas.edu.au/style/images/fileicons/application_pdf.png" border="0" class="ep_doc_icon" /></a><div class="ep_preview" id="doc_preview_709"><table><tr><td><img alt="" src="http://eprints.utas.edu.au/696/thumbnails/2/preview.png" border="0" class="ep_preview_image" /><div class="ep_preview_title">Preview</div></td></tr></table></div></td><td valign="top"><a href="http://eprints.utas.edu.au/696/2/Berry_KingIsland.pdf"><span class="ep_document_citation">PDF (Author Version)</span></a> - Requires a PDF viewer<br />860Kb</td></tr></table><p style="margin-bottom: 1em" class="not_ep_block">Official URL: <a href="http://www.blackwell-synergy.com">http://www.blackwell-synergy.com</a></p><div class="not_ep_block"><h2>Abstract</h2><p style="padding-bottom: 16px; text-align: left; margin: 1em auto 0em auto">The Proterozoic stratigraphy of Tasmania has some common aspects with South Australia but the
Wickham Orogeny (760 Ma) has been a major contrasting feature. We have used chemical U-Th-Pb
monazite dating to clarify the age relationships in western King Island, which is the key area for the
definition of the Wickham Orogeny. New monazite dates demonstrate that the major regional
deformation on King Island occurred at 1290 Ma. The Wickham Orogeny is reinterpreted as a local
deformation restricted to the contact aureole of the Cape Wickham granite. The Wickham Orogeny in
Tasmania may correlate with minor felsic volcanism in the Adelaide Fold Belt, and low-angle
unconformities in the Neoproterozoic of northwest Tasmania. The metamorphism on King Island is
synchronous with Grenville-age (1300 Ma) orogenic events recognised in central and western Australia.
The nearest known examples to Tasmania are in the Musgrave Ranges. Monazite dating of western King
Island provides the first direct evidence for Mesoproterozoic basement in southeastern Australia and
has major implications for Rodinia reconstructions.</p></div><table style="margin-bottom: 1em" border="0" cellpadding="3" class="not_ep_block"><tr><th valign="top" class="ep_row">Item Type:</th><td valign="top" class="ep_row">Article</td></tr><tr><th valign="top" class="ep_row">Additional Information:</th><td valign="top" class="ep_row">The definitive version is available at www.blackwell-synergy.com</td></tr><tr><th valign="top" class="ep_row">Keywords:</th><td valign="top" class="ep_row">geochronology, Grenville, King Island, metamorphism, monazite, Rodinia, Tasmania,
uranium, lead dating, Wickham Orogeny.</td></tr><tr><th valign="top" class="ep_row">Subjects:</th><td valign="top" class="ep_row"><a href="http://eprints.utas.edu.au/view/subjects/260100.html">260000 Earth Sciences > 260100 Geology</a></td></tr><tr><th valign="top" class="ep_row">Collections:</th><td valign="top" class="ep_row">UNSPECIFIED</td></tr><tr><th valign="top" class="ep_row">ID Code:</th><td valign="top" class="ep_row">696</td></tr><tr><th valign="top" class="ep_row">Deposited By:</th><td valign="top" class="ep_row"><span class="ep_name_citation"><span class="person_name">Mr Ruben Chan</span></span></td></tr><tr><th valign="top" class="ep_row">Deposited On:</th><td valign="top" class="ep_row">05 Feb 2007</td></tr><tr><th valign="top" class="ep_row">Last Modified:</th><td valign="top" class="ep_row">23 Jan 2008 14:17</td></tr><tr><th valign="top" class="ep_row">ePrint Statistics:</th><td valign="top" class="ep_row"><a target="ePrintStats" href="/es/index.php?action=show_detail_eprint;id=696;">View statistics for this ePrint</a></td></tr></table><p align="right">Repository Staff Only: <a href="http://eprints.utas.edu.au/cgi/users/home?screen=EPrint::View&eprintid=696">item control page</a></p>
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