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  5.     <title>UTas ePrints - Facies architecture of the Lewis Ponds carbonate and volcanic-hosted massive sulfide deposits, central western New South Wales</title>
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  13.     <meta content="Agnew, M.W." name="eprints.creators_name" />
  14. <meta content="Bull, S.W." name="eprints.creators_name" />
  15. <meta content="Large, R.R." name="eprints.creators_name" />
  16. <meta content="mwagnew2004@yahoo.com.au" name="eprints.creators_id" />
  17. <meta content="Sbull@utas.edu.au" name="eprints.creators_id" />
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  23. <meta content="Facies architecture of the Lewis Ponds carbonate and
  24. volcanic-hosted massive sulfide deposits, central western
  25. New South Wales" name="eprints.title" />
  26. <meta content="pub" name="eprints.ispublished" />
  27. <meta content="260100" name="eprints.subjects" />
  28. <meta content="restricted" name="eprints.full_text_status" />
  29. <meta content="dacite, Hill End Trough, Lewis Ponds, limestone, lithofacies associations, Mumbil Group,
  30. volcanic-hosted massive sulfide" name="eprints.keywords" />
  31. <meta content="Copyright 2004 Taylor &amp; Francis. Reproduced in accordance with the publishers policy. The definitive published version is available online at: http://www.tandf.co.uk/journals/titles/08120099.asp" name="eprints.note" />
  32. <meta content="The Lewis Ponds carbonate and volcanic-hosted Zn–Pb–Cu–Ag–Au-rich massive sulfide deposits are
  33. located near the western margin of the Hill End Trough in the eastern Lachlan Fold Belt of New South
  34. Wales. Two stratabound massive sulfide zones, Main and Toms’ occur in a tightly folded Upper Silurian
  35. succession of marine felsic volcanic and sedimentary rocks. Siltstone, mudstone and quartz crystalrich
  36. sandstone overlie thick, tabular beds of poorly sorted mixed-provenance breccia, limestone-clast
  37. breccia and pebbly granular sandstone. The sedimentary rocks unconformably overlie a succession
  38. of strongly foliated, quartz–plagioclase–phyric dacite. Hydrothermal alteration and deformation have
  39. obscured primary textures and contact relationships in the footwall volcanic succession. However,
  40. three lithofacies associations were distinguished using phenocryst abundance, overall texture and
  41. immobile element compositions. Thick (up to 100 m) conformable or fault-bound units of poorly sorted
  42. limestone-clast breccia, megabreccia and massive limestone occur throughout the Lewis Ponds host
  43. sequence. Clasts vary in size from small pebbles to 10 m-long boulders and 90 m-thick lenses. Where
  44. primary textures are preserved, the bioclastic limestone contains crinoid fragments, brachiopods,
  45. bivalves, solitary corals, volcanic quartz and feldspar crystals and rare Silurian conodonts. Although
  46. originally deposited in shallower water, the allochthonous limestone occurs in a host sequence of
  47. predominantly siltstone and mudstone. The mixed-provenance breccia, limestone-clast breccia,
  48. pebbly granular sandstone and quartz crystal-rich sandstone were deposited on the flanks of a highlevel
  49. intrusive dacite centre in a moderately deep, below wave-base slope environment. Volcanic
  50. and sedimentary components originated from multiple source areas at the basin margin and in the
  51. adjacent hinterland. The Lewis Ponds host sequence records a transition from coarse-grained polymictic
  52. volcaniclastic breccia and sandstone, upwards into mudstone, siltstone and minor volcanogenic
  53. sandstone, indicating deposition in a deepening, more restricted environment as volcanism
  54. waned and the basin progressively subsided." name="eprints.abstract" />
  55. <meta content="2004-06" name="eprints.date" />
  56. <meta content="published" name="eprints.date_type" />
  57. <meta content="Australian Journal of Earth Sciences" name="eprints.publication" />
  58. <meta content="51" name="eprints.volume" />
  59. <meta content="3" name="eprints.number" />
  60. <meta content="349-368" name="eprints.pagerange" />
  61. <meta content="10.1111/j.1400-0952.2004.01062.x" name="eprints.id_number" />
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  63. <meta content="0812-0099" name="eprints.issn" />
  64. <meta content="http://dx.doi.org/10.1111/j.1400-0952.2004.01062.x" name="eprints.official_url" />
  65. <meta content="AGNEW M. W. 2003. Geology and genesis of the Lewis Ponds
  66. carbonate and volcanic-hosted massive sulfide deposits, New
  67. South Wales Australia. PhD thesis, University of Tasmania,
  68. Hobart (unpubl.).
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  77. ALLEN R. L., WEIHED P. &amp; SVENSON S-A. 1996b. Setting of Zn–Cu–Au–Ag
  78. massive sulfide deposits in the evolution and facies architecture
  79. of a 1.9 Ga marine volcanic arc, Skellefte District, Sweden.
  80. Economic Geology 91, 1022–1053.
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  326. <meta content="Agnew, M.W. and Bull, S.W. and Large, R.R. (2004) Facies architecture of the Lewis Ponds carbonate and volcanic-hosted massive sulfide deposits, central western New South Wales. Australian Journal of Earth Sciences, 51 (3). pp. 349-368. ISSN 0812-0099" name="eprints.citation" />
  327. <meta content="http://eprints.utas.edu.au/2043/2/Agnew.Bull.Large.AJES.2004.pdf" name="eprints.document_url" />
  328. <link rel="schema.DC" href="http://purl.org/DC/elements/1.0/" />
  329. <meta content="Facies architecture of the Lewis Ponds carbonate and
  330. volcanic-hosted massive sulfide deposits, central western
  331. New South Wales" name="DC.title" />
  332. <meta content="Agnew, M.W." name="DC.creator" />
  333. <meta content="Bull, S.W." name="DC.creator" />
  334. <meta content="Large, R.R." name="DC.creator" />
  335. <meta content="260100 Geology" name="DC.subject" />
  336. <meta content="The Lewis Ponds carbonate and volcanic-hosted Zn–Pb–Cu–Ag–Au-rich massive sulfide deposits are
  337. located near the western margin of the Hill End Trough in the eastern Lachlan Fold Belt of New South
  338. Wales. Two stratabound massive sulfide zones, Main and Toms’ occur in a tightly folded Upper Silurian
  339. succession of marine felsic volcanic and sedimentary rocks. Siltstone, mudstone and quartz crystalrich
  340. sandstone overlie thick, tabular beds of poorly sorted mixed-provenance breccia, limestone-clast
  341. breccia and pebbly granular sandstone. The sedimentary rocks unconformably overlie a succession
  342. of strongly foliated, quartz–plagioclase–phyric dacite. Hydrothermal alteration and deformation have
  343. obscured primary textures and contact relationships in the footwall volcanic succession. However,
  344. three lithofacies associations were distinguished using phenocryst abundance, overall texture and
  345. immobile element compositions. Thick (up to 100 m) conformable or fault-bound units of poorly sorted
  346. limestone-clast breccia, megabreccia and massive limestone occur throughout the Lewis Ponds host
  347. sequence. Clasts vary in size from small pebbles to 10 m-long boulders and 90 m-thick lenses. Where
  348. primary textures are preserved, the bioclastic limestone contains crinoid fragments, brachiopods,
  349. bivalves, solitary corals, volcanic quartz and feldspar crystals and rare Silurian conodonts. Although
  350. originally deposited in shallower water, the allochthonous limestone occurs in a host sequence of
  351. predominantly siltstone and mudstone. The mixed-provenance breccia, limestone-clast breccia,
  352. pebbly granular sandstone and quartz crystal-rich sandstone were deposited on the flanks of a highlevel
  353. intrusive dacite centre in a moderately deep, below wave-base slope environment. Volcanic
  354. and sedimentary components originated from multiple source areas at the basin margin and in the
  355. adjacent hinterland. The Lewis Ponds host sequence records a transition from coarse-grained polymictic
  356. volcaniclastic breccia and sandstone, upwards into mudstone, siltstone and minor volcanogenic
  357. sandstone, indicating deposition in a deepening, more restricted environment as volcanism
  358. waned and the basin progressively subsided." name="DC.description" />
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  472.     <h1 class="ep_tm_pagetitle">Facies architecture of the Lewis Ponds carbonate and volcanic-hosted massive sulfide deposits, central western New South Wales</h1>
  473.     <p style="margin-bottom: 1em" class="not_ep_block"><span class="person_name">Agnew, M.W.</span> and <span class="person_name">Bull, S.W.</span> and <span class="person_name">Large, R.R.</span> (2004) <xhtml:em>Facies architecture of the Lewis Ponds carbonate and volcanic-hosted massive sulfide deposits, central western New South Wales.</xhtml:em> Australian Journal of Earth Sciences, 51 (3). pp. 349-368. 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/2043/2/Agnew.Bull.Large.AJES.2004.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/2043/2/Agnew.Bull.Large.AJES.2004.pdf"><span class="ep_document_citation">PDF</span></a> - Full text restricted - Requires a PDF viewer<br />3688Kb</td><td><form method="get" accept-charset="utf-8" action="http://eprints.utas.edu.au/cgi/request_doc"><input value="2579" 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></table><p style="margin-bottom: 1em" class="not_ep_block">Official URL: <a href="http://dx.doi.org/10.1111/j.1400-0952.2004.01062.x">http://dx.doi.org/10.1111/j.1400-0952.2004.01062.x</a></p><div class="not_ep_block"><h2>Abstract</h2><p style="padding-bottom: 16px; text-align: left; margin: 1em auto 0em auto">The Lewis Ponds carbonate and volcanic-hosted Zn–Pb–Cu–Ag–Au-rich massive sulfide deposits are&#13;
  474. located near the western margin of the Hill End Trough in the eastern Lachlan Fold Belt of New South&#13;
  475. Wales. Two stratabound massive sulfide zones, Main and Toms’ occur in a tightly folded Upper Silurian&#13;
  476. succession of marine felsic volcanic and sedimentary rocks. Siltstone, mudstone and quartz crystalrich&#13;
  477. sandstone overlie thick, tabular beds of poorly sorted mixed-provenance breccia, limestone-clast&#13;
  478. breccia and pebbly granular sandstone. The sedimentary rocks unconformably overlie a succession&#13;
  479. of strongly foliated, quartz–plagioclase–phyric dacite. Hydrothermal alteration and deformation have&#13;
  480. obscured primary textures and contact relationships in the footwall volcanic succession. However,&#13;
  481. three lithofacies associations were distinguished using phenocryst abundance, overall texture and&#13;
  482. immobile element compositions. Thick (up to 100 m) conformable or fault-bound units of poorly sorted&#13;
  483. limestone-clast breccia, megabreccia and massive limestone occur throughout the Lewis Ponds host&#13;
  484. sequence. Clasts vary in size from small pebbles to 10 m-long boulders and 90 m-thick lenses. Where&#13;
  485. primary textures are preserved, the bioclastic limestone contains crinoid fragments, brachiopods,&#13;
  486. bivalves, solitary corals, volcanic quartz and feldspar crystals and rare Silurian conodonts. Although&#13;
  487. originally deposited in shallower water, the allochthonous limestone occurs in a host sequence of&#13;
  488. predominantly siltstone and mudstone. The mixed-provenance breccia, limestone-clast breccia,&#13;
  489. pebbly granular sandstone and quartz crystal-rich sandstone were deposited on the flanks of a highlevel&#13;
  490. intrusive dacite centre in a moderately deep, below wave-base slope environment. Volcanic&#13;
  491. and sedimentary components originated from multiple source areas at the basin margin and in the&#13;
  492. adjacent hinterland. The Lewis Ponds host sequence records a transition from coarse-grained polymictic&#13;
  493. volcaniclastic breccia and sandstone, upwards into mudstone, siltstone and minor volcanogenic&#13;
  494. sandstone, indicating deposition in a deepening, more restricted environment as volcanism&#13;
  495. waned and the basin progressively subsided.</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">Copyright 2004 Taylor &amp; Francis. Reproduced in accordance with the publishers policy. The definitive published version is available online at: http://www.tandf.co.uk/journals/titles/08120099.asp</td></tr><tr><th valign="top" class="ep_row">Keywords:</th><td valign="top" class="ep_row">dacite, Hill End Trough, Lewis Ponds, limestone, lithofacies associations, Mumbil Group,&#13;
  496. volcanic-hosted massive sulfide</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">2043</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">Mrs Katrina Keep</span></span></td></tr><tr><th valign="top" class="ep_row">Deposited On:</th><td valign="top" class="ep_row">04 Oct 2007 16:40</td></tr><tr><th valign="top" class="ep_row">Last Modified:</th><td valign="top" class="ep_row">23 Jan 2008 16:03</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=2043;">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=2043">item control page</a></p>
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