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<title>UTas ePrints - Neoproterozoic and Cambrian continental rifting, continent-arc collision and post-collisional magmatism</title>
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<meta content="Crawford, A.J." name="eprints.creators_name" />
<meta content="Cayley, R.A." name="eprints.creators_name" />
<meta content="Taylor, D.H." name="eprints.creators_name" />
<meta content="Morand, V.J." name="eprints.creators_name" />
<meta content="Gray, C.M." name="eprints.creators_name" />
<meta content="Kemp, A.I.S." name="eprints.creators_name" />
<meta content="Wohlt, K.E." name="eprints.creators_name" />
<meta content="VandenBerg, A.H.M." name="eprints.creators_name" />
<meta content="Moore, D.H." name="eprints.creators_name" />
<meta content="Maher, S." name="eprints.creators_name" />
<meta content="Direen, N.G." name="eprints.creators_name" />
<meta content="Edwards, J." name="eprints.creators_name" />
<meta content="Donaghy, A.G." name="eprints.creators_name" />
<meta content="Anderson, J.A." name="eprints.creators_name" />
<meta content="Black, L.P." name="eprints.creators_name" />
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<meta content="Neoproterozoic and Cambrian
continental rifting, continent-arc collision and post-collisional magmatism" name="eprints.title" />
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<meta content="Late Neoproterozoic, Cambrian, Geological Survey of Victoria" name="eprints.keywords" />
<meta content="Major advances have been made over the last decade in our understanding of the distribution, compositions, age and significance of Late Neoproterozoic and Cambrian rocks in Victoria.These advances have been driven mainly by the new generation of geological mapping carried out by the Geological Survey of Victoria, using detailed aeromagnetic, gravity and radiometric datasets covering much of the state. In addition, detailed work by universities over certain areas, particularly the Glenelg region in the far west and locally around Stawell, have made significant contributions to the knowledge of the Cambrian geology.
In western Victoria, Cambrian rocks comprise all the known
sedimentary and volcanic bedrock as well as numerous granites. Although there is some possibility of Proterozoic rocks occurring here, no dated rocks have returned ages older than Cambrian. The rock units and geological histories of the Glenelg, Grampians, Stavely and Stawell zones, which were poorly known until recently, are now much better understood. In central and eastern Victoria, the Cambrian rocks generally lie at deeper structural levels and are only exposed in the hanging walls of major faults. Important new information is available for the Glenelg River Complex in westernmost Victoria, the exposed and drilled volcanic belts in western Victoria, and the Cambrian greenstones around Pitfield and on Phillip Island." name="eprints.abstract" />
<meta content="2003" name="eprints.date" />
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<meta content="Crawford, A.J. and Cayley, R.A. and Taylor, D.H. and Morand, V.J. and Gray, C.M. and Kemp, A.I.S. and Wohlt, K.E. and VandenBerg, A.H.M. and Moore, D.H. and Maher, S. and Direen, N.G. and Edwards, J. and Donaghy, A.G. and Anderson, J.A. and Black, L.P. (2003) Neoproterozoic and Cambrian continental rifting, continent-arc collision and post-collisional magmatism. In: Evolution of the Palaeozoic Basement. . Geological Society of Australia, Sydney, Australia, pp. 73-93." name="eprints.citation" />
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continental rifting, continent-arc collision and post-collisional magmatism" name="DC.title" />
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<meta content="Major advances have been made over the last decade in our understanding of the distribution, compositions, age and significance of Late Neoproterozoic and Cambrian rocks in Victoria.These advances have been driven mainly by the new generation of geological mapping carried out by the Geological Survey of Victoria, using detailed aeromagnetic, gravity and radiometric datasets covering much of the state. In addition, detailed work by universities over certain areas, particularly the Glenelg region in the far west and locally around Stawell, have made significant contributions to the knowledge of the Cambrian geology.
In western Victoria, Cambrian rocks comprise all the known
sedimentary and volcanic bedrock as well as numerous granites. Although there is some possibility of Proterozoic rocks occurring here, no dated rocks have returned ages older than Cambrian. The rock units and geological histories of the Glenelg, Grampians, Stavely and Stawell zones, which were poorly known until recently, are now much better understood. In central and eastern Victoria, the Cambrian rocks generally lie at deeper structural levels and are only exposed in the hanging walls of major faults. Important new information is available for the Glenelg River Complex in westernmost Victoria, the exposed and drilled volcanic belts in western Victoria, and the Cambrian greenstones around Pitfield and on Phillip Island." name="DC.description" />
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<h1 class="ep_tm_pagetitle">Neoproterozoic and Cambrian continental rifting, continent-arc collision and post-collisional magmatism</h1>
<p style="margin-bottom: 1em" class="not_ep_block"><span class="person_name">Crawford, A.J.</span> and <span class="person_name">Cayley, R.A.</span> and <span class="person_name">Taylor, D.H.</span> and <span class="person_name">Morand, V.J.</span> and <span class="person_name">Gray, C.M.</span> and <span class="person_name">Kemp, A.I.S.</span> and <span class="person_name">Wohlt, K.E.</span> and <span class="person_name">VandenBerg, A.H.M.</span> and <span class="person_name">Moore, D.H.</span> and <span class="person_name">Maher, S.</span> and <span class="person_name">Direen, N.G.</span> and <span class="person_name">Edwards, J.</span> and <span class="person_name">Donaghy, A.G.</span> and <span class="person_name">Anderson, J.A.</span> and <span class="person_name">Black, L.P.</span> (2003) <xhtml:em>Neoproterozoic and Cambrian continental rifting, continent-arc collision and post-collisional magmatism.</xhtml:em> In: Evolution of the Palaeozoic Basement. . Geological Society of Australia, Sydney, Australia, pp. 73-93.</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 onmouseover="EPJS_ShowPreview( event, 'doc_preview_782' );" href="http://eprints.utas.edu.au/774/1/Crawford_-_Chapter_03.pdf" onmouseout="EPJS_HidePreview( event, 'doc_preview_782' );"><img alt="[img]" src="http://eprints.utas.edu.au/style/images/fileicons/application_pdf.png" class="ep_doc_icon" border="0" /></a><div class="ep_preview" id="doc_preview_782"><table><tr><td><img alt="" src="http://eprints.utas.edu.au/774/thumbnails/1/preview.png" class="ep_preview_image" border="0" /><div class="ep_preview_title">Preview</div></td></tr></table></div></td><td valign="top"><a href="http://eprints.utas.edu.au/774/1/Crawford_-_Chapter_03.pdf"><span class="ep_document_citation">PDF</span></a> - Requires a PDF viewer<br />5Mb</td></tr></table><div class="not_ep_block"><h2>Abstract</h2><p style="padding-bottom: 16px; text-align: left; margin: 1em auto 0em auto">Major advances have been made over the last decade in our understanding of the distribution, compositions, age and significance of Late Neoproterozoic and Cambrian rocks in Victoria.These advances have been driven mainly by the new generation of geological mapping carried out by the Geological Survey of Victoria, using detailed aeromagnetic, gravity and radiometric datasets covering much of the state. In addition, detailed work by universities over certain areas, particularly the Glenelg region in the far west and locally around Stawell, have made significant contributions to the knowledge of the Cambrian geology.
In western Victoria, Cambrian rocks comprise all the known
sedimentary and volcanic bedrock as well as numerous granites. Although there is some possibility of Proterozoic rocks occurring here, no dated rocks have returned ages older than Cambrian. The rock units and geological histories of the Glenelg, Grampians, Stavely and Stawell zones, which were poorly known until recently, are now much better understood. In central and eastern Victoria, the Cambrian rocks generally lie at deeper structural levels and are only exposed in the hanging walls of major faults. Important new information is available for the Glenelg River Complex in westernmost Victoria, the exposed and drilled volcanic belts in western Victoria, and the Cambrian greenstones around Pitfield and on Phillip Island.</p></div><table style="margin-bottom: 1em" cellpadding="3" class="not_ep_block" border="0"><tr><th valign="top" class="ep_row">Item Type:</th><td valign="top" class="ep_row">Book Chapter</td></tr><tr><th valign="top" class="ep_row">Keywords:</th><td valign="top" class="ep_row">Late Neoproterozoic, Cambrian, Geological Survey of Victoria</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">ID Code:</th><td valign="top" class="ep_row">774</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">26 Feb 2007</td></tr><tr><th valign="top" class="ep_row">Last Modified:</th><td valign="top" class="ep_row">09 Jan 2008 02:30</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=774;">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=774">item control page</a></p>
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