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<table cellpadding="3" cellspacing="0" width="100%" class="forumline"> <thead> <caption><table border="0" cellspacing="0" cellpadding="0" width="100%" class="forumheader"> <tr> <td align="left" valign="bottom" width="25"><img src="http://picsrv.fora.pl/AcidTechTiger/images/hdr_left.gif" width="25" height="27" alt="" /></td> <td align="center" class="forumheader-mid">Topic review</td> <td align="right" valign="bottom" width="25"><img src="http://picsrv.fora.pl/AcidTechTiger/images/hdr_right.gif" width="25" height="27" alt="" /></td> </tr></table></caption> </thead> <tbody> <tr> <th class="thCornerL" width="22%" height="26">Author</th> <th class="thCornerR">Message</th> </tr> <tr> <td width="22%" align="left" valign="top" class="row1"><span class="name"><a name=""></a><b>lompiacv</b></span></td> <td class="row1" height="28" valign="top"><table width="100%" border="0" cellspacing="0" cellpadding="0"> <tr> <td width="100%"><img src="http://picsrv.fora.pl/AcidTechTiger/images/post_old.gif" width="12" height="9" alt="Post" title="Post" border="0" /><span class="postdetails">Posted: Sun 12:48, 16 Jan 2011<span class="gen"> </span> Post subject: ugg stivali Total Station and the South CASS topog</span></td> </tr> <tr> <td colspan="2"><hr /></td> </tr> <tr> <td colspan="2"><span class="postbody">Total Station and the South CASS software topographic map of the Survey and Mapping <br /> <br /> <br />Note the word, the development of point of note will be removed, (the switch 64) 64 Chen Changshou: metallogenic conditions of the region of Su Pute mineral supplement a mostly collection of smaller particle size; developed in the silk mylonite mica quartz pyrite mostly dense star-shaped, thin veins and stockwork, local to agglomerate and form iron cap. Epidotization mainly developed in the basic volcanic rocks, the alteration mostly strip or area, a wide range of local and brass associated pyrite mineralization. Mainly in silicified structural zone within the quartz in pyrite sericite quartzite mylonite formation lens, and the associated star disseminated pyrite. Su Pute in copper point: the distribution of iron in Fort Devonian cambron group on the second lithologic sub-group, in which abnormalities were found in a copper ore body, produced in the pyrite sericite rock and plagioclase amphibolite contact area the amphibolite rocks, copper mineralization with long> 2km, width 15 ~ 67m, mineralization was strongly limonitization, surface copper mineralization expressed as larvae L malachite, native rock,<a href="http://www.uggsstivali.org" target="_blank">ugg stivali</a>, the fine can be seen chalcopyrite vein, grade more in 0.21 × 10 ~ 3.92 × 1n. . Figure 2 alteration and mineralization specimens specimens Su Pute quiet area 2 zinc alteration and mineralization of points: the distribution of iron in Fort Devonian cambron group on the second lithologic sub-group of altered rocks as ferromanganese quality marble and sulfide iron cap,<a href="http://www.uggsbootsbillig.com" target="_blank">ugg boots günstig</a>, iron and manganese in the iron cap quality marble alteration zone up to 8005000m, width 17 ~ 120m, the loss of holes in the iron cap growth, the surface was strongly altered iron of the brown and fading phenomenon, grade more in 0.1 × 1O ~ (on the next page 61) retain only the surface features. \Click the \Remove unwanted according to the actual sketch the triangle and save. Left Click the \\1.1 × 1O. 4 Prospecting area (1) Lead in the region belong to the same Maizi with cocoa Tall Basin, Su Pute wing area in the Southwest sub-basin Maizi anticline in the same tectonic setting and metallogenic conditions. District Neikang Bu Iron Fort, the distribution of group formation lead, zinc and copper polymetallic mineralization close to one acid-basic volcanic rocks and volcanic activity of a Clearance of clastic deposition of calcium deposits, tectonic flysch-type construction, calcium deposition of an interbedded calcareous clastic sandstone and marble in the general distribution of iron and manganese star disseminated pyrite, layered skarn (volcanic steam hydrothermal metamorphic rocks), and the distribution of iron cap, interbedded calcareous sandstone and marble with iron and manganese and copper mineralization of zinc, copper fabric of basic volcanic rocks (copper ore body),<a href="http://www.monclerjackens.net" target="_blank">moncler daunenjacke</a>, followed by extensive development of the region structure of a pyrite altered rock (local with silicification silicified) sericite quartz mylonite, mylonite belt length> 7000m, tens of meters to 200 meters wide and mylonite belt in the late stages of sexual activity with Zhang, ductile shear zones of the more obvious characteristics of activity, with tectonic deformation of the weak East, West, strong features, mylonite zone within the lens cap ~ layered distribution of iron; Moreover, the local sub-volcanic rocks (amphibolite rocks) and the basic ~ acid is not intrusive development; from the volcano sedimentary, structural characteristics and magmatic activities are very beneficial. (2) Su Pute region surrounding the nature of alteration and mineralization conditions and comparable with Cocoa Tall zinc, alteration features basically the same. Su Pute marble region manganese (iron hat) The leaching deeper, resulting in poor surface ore grade change, but the leaching depth should be 30m or more (compared Cocoa Tall zinc and surface engineering), down should be the primary zone. (3) Heavy physical alteration of the area,<a href="http://www.uggsstivali.org" target="_blank">stivali ugg</a>, alteration intensity was expected to NCKU mine geological background. Lead prospecting in addition to studies, should be noted that copper, gold (silver) integrated prospecting. Received :2009-06-05 Next we want to make the necessary terrain and note, that is filling and add some text that frame, \Figure the size of the input vertical and horizontal dimensions, in Figure Name column enter the necessary information,<a href="http://www.monclerjackens.net" target="_blank">Moncler online</a>, point to determine, so that a complete topographic map is complete. 6 Conclusion Through the above steps, basically completed a topographic mapping from the measurement to the whole process, of which there are many details without making some detail, it is only in the mapping process can personally do more and more practice makes perfect. 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