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    <title>UTas ePrints - Quantitative phase-analysis by the Rietveld method using X-ray powder-diffraction data: application to the study of alteration halos associated with volcanic-rock-hosted massive sulfide deposits</title>
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    <meta content="Monecke, T." name="eprints.creators_name" />
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<meta content="Quantitative phase-analysis by the Rietveld method using X-ray powder-diffraction data: application to the study of alteration halos associated with volcanic-rock-hosted
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<meta content="quantitative phase-analysis, Rietveld method, alteration mineralogy, volcanic-rock-hosted massive sulfide deposits,
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<meta content="Quantitative determination of the mineralogical composition of hydrothermally altered rocks was performed by means of the Rietveld method using X-ray powder-diffraction data. Initially, experiments were carried out to minimize systematic errors arising from preferred orientation of particles as well as micro-absorption. The precision of the proposed method was tested by independent replicate sample-preparation and analyses. The closeness of the replicate phase-determinations showed that random within-laboratory errors were comparatively small. Expressed as chemical compositions, the quantitative results are in good
agreement with the major oxide concentrations determined by X-ray fluorescence. The results indicate that the relative abundances of phases and refined element substitutions were accurately determined. The method developed was applied to hydrothermally altered rocks from the Waterloo volcanic-rock-hosted massive sulfide (VHMS) deposit in Queensland, Australia. Hierarchical cluster analysis led to the discrimination of several mineralogically distinct alteration-induced assemblages. These mineral
assemblages are characteristic of specific zones of alteration. The strong spatial zoning with respect to the mineralized body and the distinct mineralogical assemblages of the alteration halo are interpreted to result primarily from varying degrees of hydrolytic decomposition and potassium metasomatism of the wallrocks. Based on these results, we suggest that quantitative phase-analysis
by the proposed method represents a new powerful tool in studies of alteration halos. " name="eprints.abstract" />
<meta content="2001" name="eprints.date" />
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<meta content="Canadian Mineralogist" name="eprints.publication" />
<meta content="39" name="eprints.volume" />
<meta content="6" name="eprints.number" />
<meta content="1617-1633" name="eprints.pagerange" />
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<meta content="BARRETT, T.J., CATTALANI, S. &amp; MACLEAN, W.H. (1993): Volcanic lithogeochemistry and alteration at the Delbridge
massive sulfide deposit, Noranda, Quebec. J. Geochem.
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BERGMANN, J., FRIEDEL, P. &amp; KLEEBERG, R. (1998): BGMN-a
new fundamental parameters based Rietveld program for
laboratory X-ray sources, its use in quantitative analysis
and structure investigations. CPD Newslett. 20, 5-8.
________ &amp; KLEEBERG, R. (1998): Rietveld analysis of
disordered layer silicates. In EPDIC 5-Proc. European
Powder Diffraction Conf. (R. Delhez &amp; E.J. Mittemeijer,
eds.). Mat. Sci. Forum 278-281, 300-305.
________, ________ , HAASE, A. &amp; BREIDENSTEIN, B. (2000):
Advanced fundamental parameter model for improved
profile analysis. In EPDIC 6-Proc. European Powder
Diffraction Conf. (R. Delhez &amp; E.J. Mittemeijer, eds.). Mat.
Sci. Forum 347-349, 303-308.
________ , ________ &amp; TAUT, T. (1994): A new structure
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________ , ________ &amp; ________ (1997): Quantitative phase
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improved stability and convergence behavior. Adv. X-Ray
Anal. 40, 425.
________ , MONECKE, T. &amp; KLEEBERG, R. (2001): Alternative
algorithm for the correction of preferred orientation in
Rietveld analysis. J. Appl. Crystallogr. 34, 16-19.
BERRY, R.F., HUSTON, D.L., STOLZ, A.J., HILL, A.P., BEAMS,
S.D., KURONEN, U. &amp; TAUBE, A. (1992): Stratigraphy,
structure, and volcanic-hosted mineralization of the Mount
Windsor Subprovince, North Queensland, Australia. Econ.
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BISH, D.L. (1993): Studies of clays and clay minerals using Xray powder diffraction and the Rietveld method. In CMS
Workshop Lectures. 5. Computer Applications to X-ray
Powder Diffraction Analysis of Clay Minerals (R.C.
Reynolds, Jr. &amp; J.R. Walker, eds.). The Clay Minerals
Society, Boulder, Colorado (79-121).
________ &amp; HOWARD, S.A. (1988): Quantitative phase
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________ &amp; POST, J.E. (1993): Quantitative mineralogical
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Mineral. 78, 932-940.
________ &amp; REYNOLDS, R.C., JR. (1989): Sample preparation
for X-ray diffraction. In Modern Powder Diffraction (D.L.
Bish &amp; J.E. Post, eds.). Rev. Mineral. 20, 73-99.
________ &amp; VON DREELE, R.B. (1989): Rietveld refinement of
non-hydrogen atomic positions in kaolinite. Clays Clay
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BRINDLEY, G.W. (1945): The effect of grain or particle size on X-ray reflections from mixed powders and alloys,
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BROSTIGEN, G. &amp; KJEKSHUS, A. (1969): Redetermined crystal
structure of FeS2 (pyrite). Acta Chem. Scand. 23, 2186-2188.
COMODI, P. &amp; ZANAZZI, P.F. (1995): High-pressure structural
study of muscovite. Phys. Chem. Minerals 22, 170-177.
DOLLASE, W.A. (1971): Refinement of the crystal structures of epidote, allanite and hancockite. Am. Mineral. 56, 447-464.
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structure refinements of magnesite, calcite, rhodochrosite,
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aspects of the stereochemistry of calcite type carbonates.
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GEMMELL, J.B. (2000): Zonation of dioctahedral true mica
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YOUNG, R.A. &amp; POST, B. (1962): Electron density and thermal
effects in alpha quartz. Acta Crystallogr. 15, 337-346." name="eprints.referencetext" />
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<meta content="Quantitative determination of the mineralogical composition of hydrothermally altered rocks was performed by means of the Rietveld method using X-ray powder-diffraction data. Initially, experiments were carried out to minimize systematic errors arising from preferred orientation of particles as well as micro-absorption. The precision of the proposed method was tested by independent replicate sample-preparation and analyses. The closeness of the replicate phase-determinations showed that random within-laboratory errors were comparatively small. Expressed as chemical compositions, the quantitative results are in good
agreement with the major oxide concentrations determined by X-ray fluorescence. The results indicate that the relative abundances of phases and refined element substitutions were accurately determined. The method developed was applied to hydrothermally altered rocks from the Waterloo volcanic-rock-hosted massive sulfide (VHMS) deposit in Queensland, Australia. Hierarchical cluster analysis led to the discrimination of several mineralogically distinct alteration-induced assemblages. These mineral
assemblages are characteristic of specific zones of alteration. The strong spatial zoning with respect to the mineralized body and the distinct mineralogical assemblages of the alteration halo are interpreted to result primarily from varying degrees of hydrolytic decomposition and potassium metasomatism of the wallrocks. Based on these results, we suggest that quantitative phase-analysis
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    <h1 class="ep_tm_pagetitle">Quantitative phase-analysis by the Rietveld method using X-ray powder-diffraction data: application to the study of alteration halos associated with volcanic-rock-hosted massive sulfide deposits</h1>
    <p style="margin-bottom: 1em" class="not_ep_block"><span class="person_name">Monecke, T.</span> and <span class="person_name">Kohler, S.</span> and <span class="person_name">Kleeberg, R.</span> and <span class="person_name">Herzig, P.M.</span> and <span class="person_name">Gemmell, J.B.</span> (2001) <xhtml:em>Quantitative phase-analysis by the Rietveld method using X-ray powder-diffraction data: application to the study of alteration halos associated with volcanic-rock-hosted massive sulfide deposits.</xhtml:em> Canadian Mineralogist, 39 (6). pp. 1617-1633. ISSN 0008-4476</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/1969/1/Monecke%2C_Kohler%2C_Kleeberg%2C_Herzig%2C_Gemmell_2001.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/1969/1/Monecke%2C_Kohler%2C_Kleeberg%2C_Herzig%2C_Gemmell_2001.pdf"><span class="ep_document_citation">PDF</span></a> - Full text restricted - Requires a PDF viewer<br />950Kb</td></tr></table><div class="not_ep_block"><h2>Abstract</h2><p style="padding-bottom: 16px; text-align: left; margin: 1em auto 0em auto">Quantitative determination of the mineralogical composition of hydrothermally altered rocks was performed by means of the Rietveld method using X-ray powder-diffraction data. Initially, experiments were carried out to minimize systematic errors arising from preferred orientation of particles as well as micro-absorption. The precision of the proposed method was tested by independent replicate sample-preparation and analyses. The closeness of the replicate phase-determinations showed that random within-laboratory errors were comparatively small. Expressed as chemical compositions, the quantitative results are in good
agreement with the major oxide concentrations determined by X-ray fluorescence. The results indicate that the relative abundances of phases and refined element substitutions were accurately determined. The method developed was applied to hydrothermally altered rocks from the Waterloo volcanic-rock-hosted massive sulfide (VHMS) deposit in Queensland, Australia. Hierarchical cluster analysis led to the discrimination of several mineralogically distinct alteration-induced assemblages. These mineral
assemblages are characteristic of specific zones of alteration. The strong spatial zoning with respect to the mineralized body and the distinct mineralogical assemblages of the alteration halo are interpreted to result primarily from varying degrees of hydrolytic decomposition and potassium metasomatism of the wallrocks. Based on these results, we suggest that quantitative phase-analysis
by the proposed method represents a new powerful tool in studies of alteration halos. </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">quantitative phase-analysis, Rietveld method, alteration mineralogy, volcanic-rock-hosted massive sulfide deposits,
Waterloo VHMS deposit, Queensland, Australia.</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">ID Code:</th><td valign="top" class="ep_row">1969</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">19 Sep 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=1969;">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=1969">item control page</a></p>
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