email: cesarjcmining@outlook.es
Cel Phone 5511337862
JC MINING
Services and Mining Projects
Street Lago Wenner 67 Int 302
Col. Pensil Sur, Miguel Hidalgo
Mexico City
South Office
Santa Lucía Project; Guerrero, México.
JC MINING SA DE CV EXPANDS EXPLORATION IN SANTA LUCIA PROJECT, LOCATED IN THE SOUTH MEXICO, STATE OF GUERRERO.
JC MINING SA DE CV expands exploration in the Santa Lucia Project located in south Mexico, state of Guerrero, have been explored more than 11 mineralized target on a property of over 70 thousand hectares. The project includes mineralization porphyry Cu-Mo, epithermal high sulphidation Au-Cu, epithermal low-intermediate sulfidation Au-Ag, diatremes Ag-Pb-Zn (Au) and Fe-Cu-Au veins.
The project's history since the 70`s Cuicuilco Mining Company (Cyprus Amax) left ready for drilling work, making a great investment, its aim was to carry out a drilling program in the porphyry Cu-Mo in Patacual, La Leona, Limon, Rincon I, II and III targets. Cuicuilco Mining builds roads and schools to help neighboring community project.
In 1973 project north Industrias Peñoles Performs geological exploration and geophysics in a brecha, domes and argillic alteration; zones currently identified as epithermal high sulphidation Au-Cu and diatreme Ag-Pb-Zn (Au).
In 1978 the Mexican Geological Service (before CRM) conducts studies of geology in the NW of Santa Lucia Project and determines probable mineral resources in a brecha plumbo-argentiferous, now known as "target La Fortuna" and defined as diatreme Ag-Pb-Zn (Au) .
Currently the company JC MINING SA DE CV subsidiary of AZTECA MINING EXPLORATION SA de CV has defined the project with potential to "World Class Deposit" and he has started an exploration program in porphyry Cu-Mo located in the South Santa Lucia Project.
Geology and Mineralization
Cu-Mo porphyry deposit, in an area of alteration at the moment of 5 x 4 kilometers, includes potassic alteration represented by orthoclase and biotite secondary; calco-sodic alteration of albite-epidote, biotite-magnetite-tourmaline, albitization, phyllic alteration of quartz-sericite-pyrite, quartz-sericite; sericitization, argillic alteration of kaolinite-morntmorillonite, propylitic alteration of chlorite-epidote, chlorite-epidote-pyrite and silicification.
At least 5 mineralized magmatic pulses have been identified, including a quartzomonzonitic porphyry, granitic porphyry, amphibole-tourmaline granodiorite, rhyolitic porphyry and dykes of andesitic composition. The minearalization of copper comes from chalcopyrite, bornite, covelite, chalcosite, malachite, azurite, brocantite and chrysocolla; the molybdenum mineralization comes from molybdenite and ferro-molybdenite.
Magmatic pulses
Porphyry Qz-Monzonite
Porphyric texture with quartz eyes and feldspar crystals, phyllic alteration of quartz-sericite-pyrite, sericitic alteration, albitization, occasional alteration, chalcosodic and potassium alteration with orthoclase phenocrysts. Mineralization of pyrite, malachite, chalcopyrite, bornita, covelite, chalcosite, crisocola, brocantite, azurite and molybdenite. Goetite-jarosite oxides.
Granitic porphyry
Porphyritic texture with feldspar, quartz, amphibole and biotite phenocrysts, potassium alteration with Euhedral orthoclase phenoscristals. Vetilleo quartz and local areas of stockworks. Mineralization of pyrite, chalcopyrite, bornite, molybdenite. Oxides of goethite, hematite, jarosite, turjite and traces of gold.
Granodiorite amphibole-magnetite
Porphyry texture with abundant amphibole and biotite ferromagnesians, moderate to intense magnetite. Potassium alteration of secondary biotite, biotite-tourmaline-magnetite and silicification. Areas of stockwork, pyrite, chalcopyrite and bornite. Oxides of goethite, hematite and jarosite.
Porphyry rhyolitic
Porphyritic texture with quartz eyes, filic alteration of Qz-sericite-pyrite, quartz-molybdenite veinlets, pyrite, chalcopyrite. Oxides of goethite, hematite and jarosite decile moderate.
Granodiorite
Porphyric texture with crystals of feldspar, quartz, biotite and amphibole, traces of fine pyrite and traces of oxides of goethite-hematite.
Granite biotite
Porphyritic texture constituted by quartz feldspar and biotite. Traces of disseminated fine pyrite and oxides of goethite-hematite.
Andesitic dykes
Afanitic texture dark green, weak to moderate magnetite and occasionally potassium alteration of secondary biotite. Traces of fine pyrite, chalcopyrite and molybdenite in contact zones.
Applied dykes
Africitic ocher texture, granite composition of quartz and feldspar.
Structures
At least 3 structural systems have been defined in the Patacual Project, these are normal type faults, normal faults with oblique component and lateral dextral and symmetrical faults. The regional main system has a NW course of 50 ° -70 °, the second system NE 20 ° to North-South and the third system NE 75 ° to East-West. There is a strip of copper-molybdenum mineralization that goes from the target Rincón to Sierrita with Rumbo NE 30 ° and originates from the intersection of the first 2 structural systems.
