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The Velardeña Zn–(Pb–Cu) Skarn-Epithermal Deposits, Central

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The Velardeña Zn–(Pb–Cu) Skarn-Epithermal Deposits, Central Boletín de la Sociedad Geológica Mexicana / 72 (3) / A270719/ 2020 / 1 The Velardeña Zn–(Pb–Cu) skarn-epithermal deposits, central-northern Mexico: New physical-chemical constraints on ore-forming processes El sistema skarn-epitermal de Zn–(Pb–Cu) de Velardeña, Durango (México): Nuevos datos fisicoquímicos de los procesos de mineralización Abigail Jiménez-Franco1,2,3*, Carles Canet4,5, Pura Alfonso6, Eduardo González-Partida7, Abdorrahman Rajabi8, Edgar Escalante9 ABSTRACT 1 Departament de Mineralogia, Petrologia i Geologia ABSTRACT RESUMEN Aplicada, Universitat de Barcelona, Marti i Franquès s/n, 08028, Barcelona, Catalunya, Spain. The Velardeña mining district is economically 2 El distrito minero Velardeña es económicamente el más Institut de Nanociència i Nanotecnologia, IN2UB the most important of Durango state. The Facultat de Química, Universitat de 8 Barcelona, Av. importante del estado de Durango. En él, las mine- Diagonal 645, 08028 Barcelona, Catalunya, Spain. ore deposits occur in different skarn zones ralizaciones comprenden diferentes zonas de skarn, developed within the intrusive contact between 3 desarrolladas entre el contacto de calizas mesozoicas, Posgrado en Ciencias de la Tierra, Universidad Na- Mesozoic limestones and Eocene granitic stocks cional Autónoma de México, Ciudad Universitaria, stocks y diques del Eoceno. Los depósitos de Velardeña Coyoacán, 04510, CDMX, Mexico. and dikes. The most important ore deposits are más importantes están relacionados al dique Santa related to the Santa María dike and Reyna de 4 María, y el stock porfídico Reyna de Cobre (separados Centro de Ciencias de la Atmósfera, Universidad Cobre porphyritic stock (separated from each Nacional Autónoma de México, Ciudad Universitar- entre sí ~10 km). La mineralización ocurre como ia, Coyoacán, 04510, CDMX, Mexico. other by 10 km). They occur as irregularly reemplazamiento, formando cuerpos irregulares cerca shaped replacement masses developed near the 5 del contacto con los intrusivos, caracterizados por una Instituto de Geofísica, Universidad Nacion- intrusive contact and have a skarn paragenesis al Autónoma de México, Ciudad Universitaria, paragénesis típica de skarn (calcisilicatos y sulfuros). Coyoacán, 04510, CDMX, Mexico. dominated by calc-silicates and sulfides. The Las asociaciones minerales muestran texturas de mineral assemblages show replacement textures 6 Dept. d’Enginyeria Minera, Industrial i TIC, Uni- reemplazo dominados por clinopiroxeno cálcico (Di and are dominated by calcic clinopyroxene 97- versitat Politècnica de Catalunya, Av. de les Bases de Hd4 Jh ) y granate (Ad Grs ) en el Manresa 61-73, 08242 Manresa, Barcelona, Spain. (Di Hd Jh ) and garnet (Ad Grs ) 53 2-02 04-01 100-57 43-00 97-53 42-02 04-01 100-57 43-00 exoskarn, y wollastonita particularmente abundante en in the exoskarn, with wollastonite particularly 7 Centro de Geociencias, Universidad Nacional el endoskarn. Los hidrosilicatos son actinolita, epidota abundant in the endoskarn. Hydrous silicates Autónoma de México, Campus Juriquilla, 76230, y clorita; los sulfuros incluyen pirita, esfalerita, pirro- Santiago de Querétaro, Mexico. are actinolite, epidote, and chlorite, whereas sulfides include pyrite, sphalerite, pyrrhotite, tita, galena, calcopirita y sulfosales. Scheelita, hema- 8 School of Geology, College of Science, University of tita, cuarzo y calcita también están presentes. El geo- Tehran, 16th Azar St., Enghelab Sq., Tehran, Iran. galena, chalcopyrite, and sulfosalts. Scheelite, hematite, quartz, and calcite are also present. barómetro de esfalerita estima que las mineralizaciones 8 Industrias Peñoles, prolongación Comonfort s/n, According to sphalerite geobarometry, the tipo skarn de Velardeña se formaron a profundidades Col. Metalurgica, 27370, Torreón, Coahuila, Mexico. skarns formed at hypabyssal depths (~3–4 km). hipabisales (~ 3-4 km). La mineralización metálica * Corresponding author: (A. Jiménez-Franco) They developed by a succession of replacive se desarrolló por una sucesión de eventos de reemplaza- [email protected] mineralizing events, including (a) a prograde miento, que incluyen (a) una etapa prógrada a ≥470 stage at temperatures from ≥470 to 335 °C a 335 °C y baja f(CO2), seguida por (b) la etapa retrógrada de 335 a 220 °C. Hubo un aumento gene- in conditions of low f (CO2), followed by (b) a retrograde stage from 335 to 220 °C. There was ral de f(O2), durante el descenso de temperatura en la formación del yacimiento, debido a la mezcla de fluidos How to cite this article: a general increase in f (O2), accompanying the Jiménez-Franco, A., Canet, C., Alfonso P., González- temperature decline during the formation of the mineralizantes con agua más fría, oxidante y diluida. Partida, E., Rajabi, A., Escalante, E., 2020, The system, which accounts for a process of mixing Durante la etapa retrógrada, se formaron wollastonita, Velardeña Zn–(Pb–Cu) The Velardeña Zn–(Pb– granate cálcico y clinopiroxeno. La etapa prógrada dio Cu) skarn-epithermal deposits, central-northern with cooler, oxidizing, and dilute water. During Mexico: new physical-chemical constraints on the retrograde stage, wollastonite, calcic garnet lugar a la formación de hidrosilicatos, sulfuros (inclu- ore-forming processes: Boletín de la Sociedad and clinopyroxene formed. On the other hand, yendo sulfosales), scheelita y hematita. Además de las Geológica Mexicana, 72 (3), A270719. http://dx.doi. hydrous silicates, sulfides, sulfosalts, scheelite, mineralizaciones tipo skarn en Velardeña, hay vetas org/10.18268/BSGM2020v72n3a270719 and hematite crystallized during the retrograde epitermales de calcita, fluorita, adularia y esfalerita, stage. Skarn mineralization is crosscut by veins cortando los calcosilicatos. La mineralización en estas Manuscript received: February 22, 2019 of calcite, fluorite, adularia, and sphalerite. The vetas se estima que se formó a <200 °C. Por ello, Corrected manuscript received: August 30, 2019 Manuscript accepted: September 6, 2019 vein mineralization formed at temperatures es plausible proponer que los depósitos minerales que below 200 °C. The different ore deposits of conforman el distrito minero Velardeña constituyen un Peer Reviewing under the responsibility of Velardeña constitute a telescoped skarn–epith- sistema skarn-epitermal telescópeado. Universidad Nacional Autónoma de México. ermal mineral system. Palabras clave: paragénesis, geoter- This is an open access article under the CC BY-NC-SA Keywords: paragenesis, geothermom- mometría, telescopeo skarn-epiter- license(https://creativecommons.org/licenses/by-nc-sa/4.0/) etry, epitermal–skarn telescoping, geo- mal, modelización geoquímica, sulfu- chemical modeling, massive sulfides. ros masivos. The Velardeña Zn–(Pb–Cu) skarn-epithermal deposits, central-northern Mexico http://dx.doi.org/10.18268/BSGM2020v72n3a270719 2 / Boletín de la Sociedad Geológica Mexicana // 7272 (3)(3) // A270719/A270719 / 2020 2020 1. Introduction Another large ore deposit of this type is that of the Velardeña Pb–Zn(–Cu) mining district in Mesozoic carbonate rocks are widely distributed central-northern Mexico, economically the most throughout central-northern and eastern Mexico, important district of Durango state. Felder (1979) INTRODUCTION and in many places they were intruded by felsic calculated a total of 24 Mt of ore reserves for to intermediate plutonic and hypabyssal rocks of only one of the mineralized areas in Velardeña, Eocene age. As a result, numerous skarn deposits the Santa María mine (Figure 1). This mine was were formed through a complex succession of the only productive one in the entire district in metallogenic stages (Camprubí, 2009). Some of the 1970s and, after a three-decade interruption these skarns are giant base-metal deposits, such of mining activities, Industrias Peñoles resumed as the Naica Zn–Pb(–Cu–Au–Ag) deposit in exploration in 2006. Due to its economic and geo- Chihuahua state (processing capacity: 690,000 t/ logical interest, several works have been focused yr of run-of-mine (ROM) ore Industrias Peñoles, on the skarn mineralization of the Santa María 2016), the Concepción del Oro Cu(–Pb–Zn–Au) mine, notably the metallogenic evolution (Spurr deposit (936000 t/yr ROM ore; SGM, 2014) and and Garrey, 1908; Levich, 1973; Gilmer et al., the Francisco I. Madero Zn–Cu–Pb(–Ag) deposit 1986, 1988; Gilmer, 1987a, 1987b) and structural (2200000 t/yr ROM ore; Industrias Peñoles, geology perspectives (Pinet and Tremblay, 2009). 2016), both in Zacatecas state, and the Charcas However, the reactivation of exploration car- Zn–Cu (–Ag–Pb) deposit in San Luis Potosí state ried out in 2006 revealed new areas with economic (1460000 t/yr ROM ore; Southern Copper Cor- potential in the northwest of the district, mainly at poration, 2016). Reyna de Cobre (Figure 1). Figure 1 Location and detailed geological map of the Velardeña mining district, showing the two main ore deposits: Santa María and Reyna de Cobre. Minor ore occurrences are (1) La Industria, (2) La Esperanza, (3) Antares, (4) San Mateo, (5) Santa Isabel, and (6) Guardarraya. The schematic stratigraphic column (right) is based on SGM (1997). Geological schematic cross- sections of the Santa María (from La Industria to Santa María) and San Lorenzo (from San Mateo to Reyna del Cobre) ranges are shown in Figure 2. The top map shows the location of the Velardeña mining district in relation to the three main geological provinces of central-northern Mexico (Key: SMO = Sierra Madre Oriental; SMOc = Sierra Madre Occidental; CP = Central
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