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  5.     <title>UTas ePrints - Facies architecture and Late Pliocene-Pleistocene evolution of a felsic volcanic island, Milos, Greece</title>
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  25. <meta content="Volcanic facies architecture . Shallow marine
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  29. <meta content="The volcanic island of Milos, Greece, comprises
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  31. compositionally and texturally diverse succession of calcalkaline, volcanic, and sedimentary rocks that record a
  32. transition from a relatively shallow but dominantly belowwave-base submarine setting to a subaerial one. The volcanic activity began at 2.66 plus-minus 0.07 Ma and has been more or less continuous since then. Subaerial emergence probably occurred at 1.44 plus-minus 0.08 Ma, in response to a combination of volcanic constructional processes and faultcontrolled volcano-tectonic uplift. The architecture of the dominantly felsic-intermediate volcanic succession reflects contrasts in eruption style, proximity to source, depositional environment and emplacement processes. The juxtaposition of submarine and subaerial facies indicates that for part of the volcanic history, below-wave base to abovewave base, and shoaling to subaerial depositional environments coexisted in most areas. The volcanic facies architecture comprises interfingering proximal (near vent), medial and distal facies associations related to five main volcano
  33. types: (1) submarine felsic cryptodome-pumice cone volcanoes; (2) submarine dacitic and andesitic lava domes;
  34. (3) submarine-to-subaerial scoria cones; (4) submarine-tosubaerial dacitic and andesitic lava domes and (5) subaerial lava-pumice cone volcanoes. The volcanic facies areinterbedded with a sedimentary facies association comprising sandstone and/or fossiliferous mudstone mainly derived from erosion of pre-existing volcanic deposits. The main facies associations are interpreted to have conformable, disconformable,and interfingering contacts, and there are no mappable angular unconformities or disconformities within the volcanic succession." name="eprints.abstract" />
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  45. <meta content="Allen RL (1992) Reconstruction of the tectonic, volcanic and sedimentary setting of strongly deformed Zn-Cu massive sulfide deposits at Benambra, Victoria. Econ Geol 87:825-854
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  48. Ayres LD, Peloquin AS (2000) Subaqueous, Paleoproterozoic,
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  54. Botz R, Stuben D, Winckler G, Bayer R, Schmitt M, Faber E (1996) Hydrothermal gases offshore Milos Island, Greece. Chem Geol 130:161-173
  55. Brown SJA, Barley ME, Krapez B, Cas RAF (2002) The
  56. Late Archean Melita Complex, Eastern Goldfields, Western
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  59. Campos Venuti M, Rossi RL (1996) Depositional facies in the
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  171. transition from a relatively shallow but dominantly belowwave-base submarine setting to a subaerial one. The volcanic activity began at 2.66 plus-minus 0.07 Ma and has been more or less continuous since then. Subaerial emergence probably occurred at 1.44 plus-minus 0.08 Ma, in response to a combination of volcanic constructional processes and faultcontrolled volcano-tectonic uplift. The architecture of the dominantly felsic-intermediate volcanic succession reflects contrasts in eruption style, proximity to source, depositional environment and emplacement processes. The juxtaposition of submarine and subaerial facies indicates that for part of the volcanic history, below-wave base to abovewave base, and shoaling to subaerial depositional environments coexisted in most areas. The volcanic facies architecture comprises interfingering proximal (near vent), medial and distal facies associations related to five main volcano
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  287.     <h1 class="ep_tm_pagetitle">Facies architecture and Late Pliocene-Pleistocene evolution of a felsic volcanic island, Milos, Greece</h1>
  288.     <p style="margin-bottom: 1em" class="not_ep_block"><span class="person_name">Stewart, A.L.</span> and <span class="person_name">McPhie, J.</span> (2006) <xhtml:em>Facies architecture and Late Pliocene-Pleistocene evolution of a felsic volcanic island, Milos, Greece.</xhtml:em> Bulletin of Volcanology, 68 (7-8). pp. 703-726.</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/1467/1/Stewart%2C_McPhie_2006.pdf"><img alt="[img]" src="http://eprints.utas.edu.au/style/images/fileicons/application_pdf.png" class="ep_doc_icon" border="0" /></a></td><td valign="top"><a href="http://eprints.utas.edu.au/1467/1/Stewart%2C_McPhie_2006.pdf"><span class="ep_document_citation">PDF</span></a> - Full text restricted - Requires a PDF viewer<br />3973Kb</td><td><form method="get" accept-charset="utf-8" action="http://eprints.utas.edu.au/cgi/request_doc"><input accept-charset="utf-8" value="1873" name="docid" 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/10.1007/s00445-005-0045-2">http://dx.doi.org/10.1007/s00445-005-0045-2</a></p><div class="not_ep_block"><h2>Abstract</h2><p style="padding-bottom: 16px; text-align: left; margin: 1em auto 0em auto">The volcanic island of Milos, Greece, comprises&#13;
  289. an Upper Pliocene-Pleistocene, thick (up to 700 m),&#13;
  290. compositionally and texturally diverse succession of calcalkaline, volcanic, and sedimentary rocks that record a&#13;
  291. transition from a relatively shallow but dominantly belowwave-base submarine setting to a subaerial one. The volcanic activity began at 2.66 plus-minus 0.07 Ma and has been more or less continuous since then. Subaerial emergence probably occurred at 1.44 plus-minus 0.08 Ma, in response to a combination of volcanic constructional processes and faultcontrolled volcano-tectonic uplift. The architecture of the dominantly felsic-intermediate volcanic succession reflects contrasts in eruption style, proximity to source, depositional environment and emplacement processes. The juxtaposition of submarine and subaerial facies indicates that for part of the volcanic history, below-wave base to abovewave base, and shoaling to subaerial depositional environments coexisted in most areas. The volcanic facies architecture comprises interfingering proximal (near vent), medial and distal facies associations related to five main volcano&#13;
  292. types: (1) submarine felsic cryptodome-pumice cone volcanoes; (2) submarine dacitic and andesitic lava domes;&#13;
  293. (3) submarine-to-subaerial scoria cones; (4) submarine-tosubaerial dacitic and andesitic lava domes and (5) subaerial lava-pumice cone volcanoes. The volcanic facies areinterbedded with a sedimentary facies association comprising sandstone and/or fossiliferous mudstone mainly derived from erosion of pre-existing volcanic deposits. The main facies associations are interpreted to have conformable, disconformable,and interfingering contacts, and there are no mappable angular unconformities or disconformities within the volcanic succession.</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">Article</td></tr><tr><th valign="top" class="ep_row">Keywords:</th><td valign="top" class="ep_row">Volcanic facies architecture . Shallow marine&#13;
  294. volcanism . Felsic dome-cryptodome-pumice cone&#13;
  295. volcanoes . Southern Aegean Volcanic Arc . SHRIMP .&#13;
  296. Geochronology</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/260103.html">260000 Earth Sciences &gt; 260100 Geology &gt; 260103 Vulcanology</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">1467</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">26 Jul 2007</td></tr><tr><th valign="top" class="ep_row">Last Modified:</th><td valign="top" class="ep_row">30 Jan 2008 15:10</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=1467;">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=1467">item control page</a></p>
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