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		<title>Proyecto de sal y polihalita de Lorca</title>
		<link>https://geomnia.es/septima-entrada/</link>
		
		<dc:creator><![CDATA[ana]]></dc:creator>
		<pubDate>Tue, 12 Sep 2023 15:54:41 +0000</pubDate>
				<category><![CDATA[exploración]]></category>
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					<description><![CDATA[<p>Un proyecto promovido por Geomnia</p>
<p>La entrada <a href="https://geomnia.es/septima-entrada/">Proyecto de sal y polihalita de Lorca</a> se publicó primero en <a href="https://geomnia.es">Geomnia</a>.</p>
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					<h1 class="elementor-heading-title elementor-size-default">PROYECTO DE SAL Y POLIHALITA DE LORCA</h1>				</div>
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						<span  >
							realización						</span>
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						marzo 2016-
septiembre 2021					</p>
				
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							cliente						</span>
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						Geomnia
(proyecto propio)					</p>
				
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									<p class="p1">El Permiso de Investigación “Luis Carlos” (22.381) totaliza 23 cuadrículas mineras solicitadas para la exploración de recursos de sales sódico-potásicas y se encuentra en la Hoja 953 (Lorca) del Mapa Topográfico Nacional escala 1:50.000. El permiso afecta únicamente al municipio de Lorca (Comunidad Autónoma de la Región de Murcia). El permiso fue solicitado el 12 de septiembre de 2014, siendo otorgado el 2 de diciembre de 2018, encontrándose en su segundo año de investigación.</p><p class="p2"><span class="s1">LORCA SAL se encuentra en la denominada Cuenca de Lorca, que pertenece a una cadena de cuencas intramontañosas neógenas localizada en la Zona Interna de la Cordillera Bética. La cuenca, de morfología rectangular, queda delimitada por fallas normales en sus márgenes y hacia el Sureste y Noroeste por dos grandes sistemas de fracturas, que se orientan NO-SE (Fallas de Alhama de Murcia y Nordbética) y que forman parte de la fractura de Cádiz-Alicante.</span></p><p class="p2"><span class="s1">Sociedad Española de Talcos, S.A. desarrolla en 2003 una investigación de aguas minero-industriales, con la realización de 5 sondeos mecánicos: LRC1, LRC2, LRC3, LRC4 y LRC5. Estos sondeos intersectaron la Unidad Salina de la Cuenca de Lorca, que es objeto del Plan de Investigación. LRC3 fue realizado en el depocentro de la unidad, donde la sal queda muy superficial (&lt;70m) y alcanza una potencia superior a los 200 m. Estos datos complementan a los sondeos S4 y S5 realizados por el IGME para investigación de pizarras bituminosas. </span><span class="s2">En definitiva, la formación salina se localiza a un mínimo de 62,7 m desde superficie y alcanza los 297,9 m de profundidad. La potencia total oscila desde los 43 m (S5) a los 235,2 m (S4)</span></p>								</div>
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															<img fetchpriority="high" decoding="async" width="600" height="390" src="https://geomnia.es/wp-content/uploads/24-polihalita.jpeg" class="attachment-large size-large wp-image-2925" alt="polihalita geomnia" srcset="https://geomnia.es/wp-content/uploads/24-polihalita.jpeg 600w, https://geomnia.es/wp-content/uploads/24-polihalita-370x241.jpeg 370w, https://geomnia.es/wp-content/uploads/24-polihalita-410x267.jpeg 410w" sizes="(max-width: 600px) 100vw, 600px" />															</div>
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					<div class="sc_table_wrap"><h2 class="sc_item_title sc_table_title sc_align_left sc_item_title_style_default"
			><span class="sc_item_title_text">SONDEOS REALIZADOS</span><span class="sc_item_title_text2"> PARA EL PROYECTO</span></h2><div		class="sc_table sc_table_default alignleft trx_addons_inline_1260015825" ><table cellspacing="0" summary="sondeos realizados">
	<thead>
		<tr>
			<th>SONDEO</th>
			<th>Realizado por</th>
			<th>Techo sal (metros cota sondeo)</th>
			<th> Base sal (metros cota sondeo)</th>
			<th>Techo Sal m.s.n.m</th>
			<th>Base Sal m.s.n.m</th>
			<th>Potencia total en metros</th>
		</tr>
	</thead>
	<tbody>
		<tr>
			<td>LRC-1</td>
			<td>SETSA</td>
			<td>132,5</td>
			<td>280.5</td>
			<td>262.5</td>
			<td>114.5</td>
			<td>148</td>
		</tr>
		<tr>
			<td>LRC-2</td>
			<td>SETSA</td>
			<td>153</td>
			<td>168</td>
			<td>254</td>
			<td>239</td>
			<td>15*</td>
		</tr>
		<tr>
			<td>LRC-3</td>
			<td>SETSA</td>
			<td>62</td>
			<td>265.5</td>
			<td>305</td>
			<td>101.5</td>
			<td>203.5</td>
		</tr>
		<tr>
			<td>LRC-4</td>
			<td>SETSA</td>
			<td>135</td>
			<td>297</td>
			<td>268</td>
			<td>106</td>
			<td>162</td>
		</tr>
		<tr>
			<td>LRC-5</td>
			<td>SETSA</td>
			<td>120,5</td>
			<td>244</td>
			<td>304.5</td>
			<td>183.5</td>
			<td>121</td>
		</tr>
		<tr>
			<td>S4</td>
			<td>IGME</td>
			<td>62,7</td>
			<td>297.9</td>
			<td>311.3</td>
			<td>76.1</td>
			<td>235.2</td>
		</tr>
	</tbody>
	<tfoot>
		<tr>
			<td>S5</td>
			<td>IGME</td>
			<td>116</td>
			<td>159</td>
			<td>259</td>
			<td>216</td>
			<td>43</td>
		</tr>
	</tfoot>
</table></div></div>				</div>
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															<img decoding="async" width="1000" height="750" src="https://geomnia.es/wp-content/uploads/24-pozo-exploracion-geomnia.jpg" class="attachment-full size-full wp-image-2926" alt="pozo polihalita" srcset="https://geomnia.es/wp-content/uploads/24-pozo-exploracion-geomnia.jpg 1000w, https://geomnia.es/wp-content/uploads/24-pozo-exploracion-geomnia-768x576.jpg 768w, https://geomnia.es/wp-content/uploads/24-pozo-exploracion-geomnia-370x278.jpg 370w, https://geomnia.es/wp-content/uploads/24-pozo-exploracion-geomnia-840x630.jpg 840w, https://geomnia.es/wp-content/uploads/24-pozo-exploracion-geomnia-410x308.jpg 410w" sizes="(max-width: 1000px) 100vw, 1000px" />															</div>
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									<p class="p1">A partir <span class="s1">de</span> los datos de intersecciones se elaboró un mapa de isopacas de la formación salina sobre una superficie mínima definida por la envolvente de los sondeos LRC1, LRC3, LRC4, LRC5, S4 y S5, lo cual define un polígono de 3 km de longitud x 0,7 km de anchura (210 Has).</p><p class="p1">La siguiente tabla muestra los volúmenes estimados y Mt para las diferentes unidades salinas definidas en el sector central del Permiso. Cabe destacar que los recursos estimados para el total de la unidad salina rondan los 750 Mt. Para la unidad de Sal Blanca, se estiman unos recursos de unos 360 Mt y para la Unidad polihalítica (H1), unos 211 Mt.</p>								</div>
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					<div class="sc_table_wrap"><div		class="sc_table sc_table_default trx_addons_inline_1762929206" ><table cellspacing="0" summary="RECURSOS ESTIMADOS">
	<thead>
		<tr>
			<th></th>
			<th>Volumen (Mm3)</th>
			<th>Millones toneladas (Mt)</th>
		</tr>
	</thead>
	<tbody>
		<tr>
			<td>SAL GRIS o SUCIA*</td>
			<td>18.26</td>
			<td>38.34</td>
		</tr>
		<tr>
			<td>SAL BLANCA (H2)</td>
			<td>170.85</td>
			<td>358.79</td>
		</tr>
		<tr>
			<td>SAL + ANHIDRITA-POLIHALITA (H1)</td>
			<td>46.61</td>
			<td>97.89</td>
		</tr>
		<tr>
			<td>UNIDAD POLIHALITA (H1)</td>
			<td>100.82</td>
			<td>211.73</td>
		</tr>
		<tr>
			<td>SAL MURO</td>
			<td>20.42</td>
			<td>42.88</td>
		</tr>
	</tbody>
	<tfoot>
		<tr>
			<td>TOTAL</td>
			<td>356.97</td>
			<td>749.63</td>
		</tr>
	</tfoot>
</table></div></div>				</div>
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									<p class="p1">El siguiente esquema ilustra la posición de los diferentes sondeos y la modelización 3D realizada para las diferentes unidades salinas.</p>								</div>
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															<img decoding="async" width="1482" height="779" src="https://geomnia.es/wp-content/uploads/24-POLIHALITA-geomnia.jpeg" class="attachment-full size-full wp-image-2924" alt="esquema lorca" srcset="https://geomnia.es/wp-content/uploads/24-POLIHALITA-geomnia.jpeg 1482w, https://geomnia.es/wp-content/uploads/24-POLIHALITA-geomnia-768x404.jpeg 768w, https://geomnia.es/wp-content/uploads/24-POLIHALITA-geomnia-370x194.jpeg 370w, https://geomnia.es/wp-content/uploads/24-POLIHALITA-geomnia-840x442.jpeg 840w, https://geomnia.es/wp-content/uploads/24-POLIHALITA-geomnia-410x216.jpeg 410w" sizes="(max-width: 1482px) 100vw, 1482px" />															</div>
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		<p>La entrada <a href="https://geomnia.es/septima-entrada/">Proyecto de sal y polihalita de Lorca</a> se publicó primero en <a href="https://geomnia.es">Geomnia</a>.</p>
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