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<table border="0" cellpadding="3" cellspacing="1" width="100%" class="forumline"> <tr> <th class="thCornerL" width="22%">Autor</th> <th class="thCornerR">Wiadomość</th> </tr> <tr> <td width="22%" align="left" valign="top" class="row1"><span class="name"><a name=""></a><b>defgf10aj</b></span></td> <td class="row1" valign="top"><table width="100%" border="0" cellspacing="0" cellpadding="0"> <tr> <td width="100%"><img src="http://picsrv.fora.pl/Elveron/images/icon_minipost.gif" width="12" height="9" alt="Post" title="Post" border="0" /><span class="postdetails">Wysłany: Sob 3:12, 13 Lis 2010<span class="gen"> </span> Temat postu: ghd stijltang Ore mining area of Jiangxi down (min</span></td> </tr> <tr> <td colspan="2"><hr /></td> </tr> <tr> <td colspan="2"><span class="postbody">Ore mining area of Jiangxi down (mineralized) phase of the study <br /> <br /> <br />Salt scattered in the veins in the upper part of the sulfides are distributed late in the lower low and high sulfur distribution in the upper and early stage mineral filling and replacement. Ⅲ carbonate, wolframite and sulfide phases: distributed in the veins, the upper part of tungsten and tungsten carbonate veins usually in the same vein quartz veins alternate, alternating at the saw in the quartz vein breccia containing tungsten was contained tungsten cemented into brecciated carbonate structures. Veins saw wolframite, scheelite and minor fluorite,<a href="http://www.ghdstijltang.net" target="_blank" class="postlink">ghd stijltang</a>, sulfides, vein side of a muscovite, carbonate and chlorite. In summary, the mine ore (mineralized) phase characteristics shown in Table 1. As can be seen from the table: (1) metallogenic evolution through a continuous process but show stage, from early to late or from deep to shallow, followed by TR elements appear granodiorite Nb mineralization , Ta, TR element mineralization in two-mica monzogranite Ta, Nb, W,<a href="http://www.uggbootssaler.org" target="_blank" class="postlink">ugg boots sale</a>, Be mineralization muscovite alkali-feldspar granite (Be), (Rb),<a href="http://www.ghd-styler.org" target="_blank" class="postlink">ghd styler</a>, w mineralized pegmatite like w, Be, (Rb) mineralization feldspar and quartz veins or quartz feldspar veins w, blo, Bi mineralization quartz vein w, Mo, Bi quartz sulphide mineralization w, S mineralization carbonate veins. (2) from the metamorphic alteration from the hydrothermal metasomatism metasomatism, from morning to night from the bottom of the order of K-feldspar K-feldspar appears weak, weak petrochemical albitization albite, muscovite, weak Yun-ying Yan Liu Jianping, etc. 3: Jiangxi Dajishan metallogenic (mineralization) stage of the study of 19 of a muscovite, electrical petrochemical, fluoritization of a muscovite, fluorite, silicification, sericite mica of a , silicification, carbonation, chlorite. (3) ore-forming elements of the development trend has obvious successor. From morning to night, from the TR-÷ Na, Ta, TR-÷ Ta, Nb, w, Be-÷ (Be), (Rb), W-} W, Be, (Rb) -} W, Be, Mo -} W,<a href="http://www.uggs-ireland.com" target="_blank" class="postlink">uggs ireland</a>, Mo, Bi, Table 1Tablel sulfide a w, the evolution of the carbonate sequence. (4) ore-forming conditions change. Structural conditions from the relatively closed to the relatively open; physical and chemical conditions, temperature from hot to cold, high to low pressure, pH from alkaline to acidic and then alkaline, redox environment and then restore from the restore to oxidation. Mining Area mineralization (mineralization) stage of the phase characteristics of the table Characteristicstableofdifferentmetallizationstages characteristics of mineral alteration characteristics symbiotic nature of diagenesis and tectonic setting of the temperature solution I1 containing TR ore mineralization temperature plagioclase, microcline perthite, stone weak K-feldspar British base, biotite, magnetite, monazite, zircon phase of 640 ℃ of granodiorite rocks fossils, sphene, limonite of closure II2 Ta-containing plagioclase, microcline, perthite , of stone feldspar mineralization closed the British rock Nb-TR, biotite muscovite, monazite, xenotime 550 ℃ 334 ℃ albitization slurry of weak two-mica granite, easy to calcite, apatite, with Ta-I3 plagioclase, microcline, perthite, albitization white mica quartz, albite, garnet, muscovite green column of 526 ℃ 3O9 ℃ Nb-W-Be Shi Shi silicon beryllium, niobium and tantalum iron mine,<a href="http://www.ghdglaetteisen-guenstig.com" target="_blank" class="postlink">GHD glätteisen günstig</a>, fine spar, black and white mica granite greisen tungsten ore, containing scheelite Ⅱ II Be a 503 ℃ 280 ℃ 1r Wei muscovite, microcline, quartz, beryl, from none to 455 ℃ to 255 ℃ crystal (Rb) of a quartz w turtles the wolframite phase of sleep may pegmatite w E Ⅲ 5 with a muscovite, microcline, quartz, beryl, muscovite of 293 ℃ (Rb) Be long of a silicon-wolframite veins of quartz with muscovite of Ⅲ 6 w-Be muscovite, tourmaline, quartz, beryl, including tourmalinization 287 ℃-Mo quartz vein Be garnet, wolframite, molybdenite fluoritization silicified hydrothermal muscovite Ⅲ Phase Ⅲ 7 of w-Mo containing muscovite, quartz, wolframite, scheelite, fluorite of the magnetic 260 ℃-Bi iron sulfur quartz, pyrite, bismuthinite, natural bismuth, toxic compounds silicide sand veins, sphalerite ore, galena, molybdenite phase sericite quartz on Ⅲ 8 w containing muscovite, carbonate, fluorite, wolframite, Bai Baiyun mother of opening 1r carbonate carbonate veins through deaf 2129 ℃ tungsten ore, yellow World iron ore chlorite 1r E Note: According to Lu HZ temperature ore-forming materials [1] of the original Ministry of Heavy Industry Company Changsha 205 geological exploration team. Dajishan tungsten deposit summary report Geological Survey. 1953. [2] Jiangxi Nonferrous Geological Exploration Company 615 teams. The whole mining area of Jiangxi County Dajishan supplementary geological exploration report. 1961. [3] Second Jiangxi Metallurgical and Geological Exploration Team. Dajishan tungsten tantalum and niobium mine granite geological exploration report of beryllium deposits. 1969. Mouth <br /> More articles related to topics： <br /> <br /> <br /> <a href="http://www.naturalnemetody.fora.pl/font-color-darkblue-npr-color,2/ugg-botas-analysis-of-surface-coal-mine-slope-stab,4496.html#183218" target="_blank" class="postlink">ugg botas Analysis of surface coal mine slope stab</a> <br /> <br /> <a href="http://www.20lbs20days.com/forum/viewtopic.php?p=179232#179232" target="_blank" class="postlink">ugg botas Explore the more secure and better cable</a> <br /> <br /> <a href="http://www.hydrocodonen.fora.pl/forum-testowe,1/ugg-stiefel-degree-of-inversion-structures-of-the,776.html#786" target="_blank" class="postlink">ugg stiefel Degree of inversion structures of the</a></span></td> </tr> </table></td> </tr> <tr> <td colspan="2" height="1" class="spaceRow"><img src="http://picsrv.fora.pl/Elveron/images/spacer.gif" alt="" width="1" height="1" /></td> </tr> </table>
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