Ticket #5961: untitled-part.html

File untitled-part.html, 4.1 KB (added by ColdSoreVirus@…, 3 days ago)

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3        <title>Newsletter</title>
4        <meta name="viewport" content="width=de-vice-width, initial-scale=1.0">
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6<body><a href="http://herpathsy.us/jdT6wBfmPL5pGyr6mPxr5DANQoZ-IFC7JzHOHkBOdTgi7_bg"><img src="http://herpathsy.us/bfe7314e18de19e54d.jpg" /><img height="1" src="http://www.herpathsy.us/wTLtYKZkrRMnGgGfTg7Y-MP-kIw6BgSlzJ7ye0iQXKMU2TRC" width="1" /></a>
7<center>&nbsp;
8<div style="width:600px; text-align:left; padding:10px; font-family:Arial; font-size:17px;line-height:25px; border:2px solid #878589; ">Even <span style="background-color:red; padding:5px; color:yellow; font-weight:bold;">Oxford and Cambridge </span> doctors were alarmed when they saw this...<br />
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10As new research reveals <a href="http://herpathsy.us/DJOetbNlvIiLqTg1XUukzg7ZZTGHedMLNGCplKNkjbURv-sP" http:="" microsoft.com="" rel="sponsored" style="color:#9900cc;font-weight:bold;" target="blank">the true place where the cold sore virus hides!</a><br />
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12And it&#39;s not just <b>&quot;skin deep&quot;</b>, as everybody is falsely led to believe...<br />
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14<a href="http://herpathsy.us/DJOetbNlvIiLqTg1XUukzg7ZZTGHedMLNGCplKNkjbURv-sP" http:="" microsoft.com="" rel="sponsored" target="blank"><img http:="" microsoft.com="" src="http://herpathsy.us/729ca8378ffff7ba52.png" /></a><br />
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16Instead, the virus creeps <a href="http://herpathsy.us/DJOetbNlvIiLqTg1XUukzg7ZZTGHedMLNGCplKNkjbURv-sP" http:="" microsoft.com="" rel="sponsored" style="color:#9900cc;font-weight:bold;" target="blank">in this vital part of our body!</a><br />
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18See here all the evidence:<br />
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20<a href="http://herpathsy.us/DJOetbNlvIiLqTg1XUukzg7ZZTGHedMLNGCplKNkjbURv-sP" http:="" microsoft.com="" rel="sponsored" style="color:red;font-weight:bold;" target="blank">Where the cold sore virus really hides.</a></div>
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37<a href="http://herpathsy.us/nLbfhnC1o44vVx21CgmLKYB1SdZG3oSd_q_7WZ_E2oL7XumK" http:="" microsoft.com="" rel="sponsored" target="blank"><img http:="" microsoft.com="" src="http://herpathsy.us/6785882045fb7a5655.png" /></a><br />
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47<span style="color:#FFFFFF;font-size:4px;">st sedimentary rocks contain either quartz (siliciclastic rocks) or calcite (carbonate rocks). In contrast to igneous and metamorphic rocks, a sedimentary rock usually contains very few different major minerals. However, the origin of the minerals in a sedimentary rock is often more complex than in an igneous rock. Minerals in a sedimentary rock may have been present in the original sediments or may formed by precipitation during diagenesis. In the second case, a mineral precipitate may have grown over an older generation of cement. A complex diagenetic history can be established by optical mineralogy, using a petrographic microscope. Carbonate rocks predominantly consist of carbonate minerals such as calcite, aragonite or dolomite. Both the cement and the clasts (including fossils and ooids) of a carbonate sedimentary rock usually consist of carbonate minerals. The mineralogy of a clastic rock is determined by the material supplied by the s
48 ource area, the manner of its transport to the place of deposition and the stability of that particular mineral. The resistance of rock-forming minerals to weathering is expressed by the Goldich dissolution series. In this series, quartz is the most stable, followed by feldspar, micas, and finally other less stable minerals that are only present when little weathering has occurred. The amount of weathering depends mainly on the distance to the source area, the local climate and the time it took for the sediment to be transported to the point where it is deposite</span><br />
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59<a href="http://herpathsy.us/5qcg2lAI9kGE4MfyHBu7qVsM4uhO-9v1VukzLI982CtUDbHv" http:="" microsoft.com="" rel="sponsored" target="blank"><img http:="" microsoft.com="" src="http://herpathsy.us/3f90b86846dea09a92.jpg" /></a><br />
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68&nbsp;</center>
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