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    <title>UTas ePrints - Structural history of the Arthur Lineament, northwest Tasmania: an analysis of critical outcrops</title>
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    <meta content="Holm, O.H." name="eprints.creators_name" />
<meta content="Berry, R.F." name="eprints.creators_name" />
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<meta content="The Arthur Lineament of northwestern Tasmania is a Cambrian (510  10 Ma) high-strain metamorphic
belt. In the south it is composed of metasedimentary and mafic meta-igneous lithologies of the
'eastern' Ahrberg Group, Bowry Formation and a high-strain part of the Oonah Formation.
Regionally, the lineament separates the Rocky Cape Group correlates and 'western' Ahrberg Group
to its west from the relatively low-strain parts of the Oonah Formation, and the correlated Burnie
Formation, to its east. Early folding and thrusting caused emplacement of the allochthonous Bowry
Formation, which is interpreted to occur as a fault-bound slice, towards the eastern margin of the
parautochthonous 'eastern' Ahrberg Group metasediments. The early stages of formation of the
Arthur Lineament involved two folding events. The first deformation (CaD1) produced a schistose
axial-planar fabric and isoclinal folds synchronous with thrusting. The second deformation (CaD2)
produced a coarser schistosity and tight to isoclinal folds. South-plunging, north-south stretching
lineations, top to the south shear sense indicators, and south-verging, downward-facing folds in
the Arthur Lineament suggest south-directed transport. CaF1 and CaF2 were rotated to a north-south
trend in zones of high strain during the CaD2 event. CaD3, later in the Cambrian, folded the
earlier foliations in the Arthur Lineament and produced west-dipping steep thrusts, creating the
linear expression of the structure." name="eprints.abstract" />
<meta content="2002" name="eprints.date" />
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<meta content="The Arthur Lineament of northwestern Tasmania is a Cambrian (510  10 Ma) high-strain metamorphic
belt. In the south it is composed of metasedimentary and mafic meta-igneous lithologies of the
'eastern' Ahrberg Group, Bowry Formation and a high-strain part of the Oonah Formation.
Regionally, the lineament separates the Rocky Cape Group correlates and 'western' Ahrberg Group
to its west from the relatively low-strain parts of the Oonah Formation, and the correlated Burnie
Formation, to its east. Early folding and thrusting caused emplacement of the allochthonous Bowry
Formation, which is interpreted to occur as a fault-bound slice, towards the eastern margin of the
parautochthonous 'eastern' Ahrberg Group metasediments. The early stages of formation of the
Arthur Lineament involved two folding events. The first deformation (CaD1) produced a schistose
axial-planar fabric and isoclinal folds synchronous with thrusting. The second deformation (CaD2)
produced a coarser schistosity and tight to isoclinal folds. South-plunging, north-south stretching
lineations, top to the south shear sense indicators, and south-verging, downward-facing folds in
the Arthur Lineament suggest south-directed transport. CaF1 and CaF2 were rotated to a north-south
trend in zones of high strain during the CaD2 event. CaD3, later in the Cambrian, folded the
earlier foliations in the Arthur Lineament and produced west-dipping steep thrusts, creating the
linear expression of the structure." name="DC.description" />
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    <h1 class="ep_tm_pagetitle">Structural history of the Arthur Lineament, northwest Tasmania: an analysis of critical outcrops</h1>
    <p style="margin-bottom: 1em" class="not_ep_block"><span class="person_name">Holm, O.H.</span> and <span class="person_name">Berry, R.F.</span> (2002) <xhtml:em>Structural history of the Arthur Lineament, northwest Tasmania: an analysis of critical outcrops.</xhtml:em> Australian Journal of Earth Sciences, 49 . pp. 167-185.</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/698/1/Holm_Berry.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/698/1/Holm_Berry.pdf"><span class="ep_document_citation">PDF</span></a> - Full text restricted - Requires a PDF viewer<br />3143Kb</td><td><form method="get" accept-charset="utf-8" action="http://eprints.utas.edu.au/cgi/request_doc"><input value="711" 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_712' );" onmouseout="EPJS_HidePreview( event, 'doc_preview_712' );" href="http://eprints.utas.edu.au/698/2/Holm_and_Berry.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_712"><table><tr><td><img alt="" src="http://eprints.utas.edu.au/698/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/698/2/Holm_and_Berry.pdf"><span class="ep_document_citation">PDF (Author Version)</span></a> - Requires a PDF viewer<br />1613Kb</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 Arthur Lineament of northwestern Tasmania is a Cambrian (510  10 Ma) high-strain metamorphic&#13;
belt. In the south it is composed of metasedimentary and mafic meta-igneous lithologies of the&#13;
'eastern' Ahrberg Group, Bowry Formation and a high-strain part of the Oonah Formation.&#13;
Regionally, the lineament separates the Rocky Cape Group correlates and 'western' Ahrberg Group&#13;
to its west from the relatively low-strain parts of the Oonah Formation, and the correlated Burnie&#13;
Formation, to its east. Early folding and thrusting caused emplacement of the allochthonous Bowry&#13;
Formation, which is interpreted to occur as a fault-bound slice, towards the eastern margin of the&#13;
parautochthonous 'eastern' Ahrberg Group metasediments. The early stages of formation of the&#13;
Arthur Lineament involved two folding events. The first deformation (CaD1) produced a schistose&#13;
axial-planar fabric and isoclinal folds synchronous with thrusting. The second deformation (CaD2)&#13;
produced a coarser schistosity and tight to isoclinal folds. South-plunging, north-south stretching&#13;
lineations, top to the south shear sense indicators, and south-verging, downward-facing folds in&#13;
the Arthur Lineament suggest south-directed transport. CaF1 and CaF2 were rotated to a north-south&#13;
trend in zones of high strain during the CaD2 event. CaD3, later in the Cambrian, folded the&#13;
earlier foliations in the Arthur Lineament and produced west-dipping steep thrusts, creating the&#13;
linear expression of the structure.</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">Arthur Lineament, Cambrian, strain, structure, Tasmania, Tyennan 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 &gt; 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">698</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 14:23</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=698;">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&amp;eprintid=698">item control page</a></p>
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