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CROMA Falsa Caratula Cerro De Pasco 2 CROMA Contenido General.pmd 2 02/01/2012, 07:20 p.m. Geología del Cuadrángulo de Cerro de Pasco Hoja 22-k Boletín N° 144 Serie A Carta Geológica Nacional Escala 1:50,000 Por: Rildo Rodríguez M. Eber Cueva T. Víctor Carlotto C. Lima, Perú 2011 SERIE A: CARTA GEOLÓGICA NACIONAL N°144, 2011 Hecho el Depósito Legal N° 2012-00376 Razón Social: Instituto Geológico Minero y Metalúrgico (INGEMMET) Domicilio: Av. Canadá N° 1470, San Borja, Lima-Perú Primera Edición, INGEMMET 2011 Se terminó de imprimir el 18 de enero del año 2012 en los talleres de Imprenta Cano s.r.l. © INGEMMET Derechos Reservados. Prohibida su reproducción Presidente del Consejo Directivo: Walter Casquino Secretario General: Juan Carlos Lam Comité Editor: Walter Casquino, Víctor Carlotto, Lionel Fidel, Humberto Chirif, Giovanna Alfaro Dirección encargada del estudio: Dirección de Geología Regional Unidad encargada de la edición: Unidad de Relaciones Institucionales Revisión Geocientífica: Norman Castillo Digitalización y SIG: Federico Nureña Corrección gramatical y de estilo: Juan E. Quiroz Diagramación: Sonia Bermúdez Portada: Ciudad minera de Cerro de Pasco, desarrollada a los alrededores del tajo Raúl Rojas. Referencia bibliográfica: Rodríguez, R., Cueva, E. & Carlotto, V. (2011).- Geología del cuadrángulo de Cerro de Pasco (22-k). INGEMMET, Boletín, Serie A: Carta Geológica Nacional, 144, 164 p, 4 mapas. CROMA referencias.pmd 1 11/01/2012, 02:24 p.m. Contenido RESUMEN .......................................................................................................................................................................................... 1 CAPÍTULO I ....................................................................................................................................................................................... 5 INTRODUCCIÓN ........................................................................................................................................................................ 5 CAPÍTULO II .................................................................................................................................................................................... 11 ESTRATIGRAFÍA ....................................................................................................................................................................... 11 CAPÍTULO III ................................................................................................................................................................................... 49 ROCAS INTRUSIVAS ................................................................................................................................................................. 49 CAPÍTULO IV ................................................................................................................................................................................... 61 GEOQUÍMICA MAGMÁTICA ...................................................................................................................................................... 61 CAPÍTULO V .................................................................................................................................................................................... 71 GEOLOGÍA ESTRUCTURAL Y TECTÓNICA ............................................................................................................................ 71 CAPÍTULO VI ................................................................................................................................................................................... 89 GEOLOGÍA ECONÓMICA ......................................................................................................................................................... 89 CAPÍTULO VII ................................................................................................................................................................................ 133 INTERPRETACIÓN Y DETERMINACIÓN DE ANOMALÍAS SIGNIFICATIVAS Y SU RELACIÓN CON LAS FRANJAS METALOGENÉTICAS .................................................................................................................................... 133 CAPÍTULO VIII .............................................................................................................................................................................. 139 ROCAS Y MINERALES INDUSTRIALES ............................................................................................................................... 139 CAPÍTULO IX ................................................................................................................................................................................. 149 GEOPATRIMONIO, GEOTURISMO, CONSERVACIÓN Y SITIOS DE INTERÉS GEOLÓGICO ............................................. 149 BIBLIOGRAFÍA ............................................................................................................................................................................. 155 CROMA Contenido General.pmd 1 02/01/2012, 07:20 p.m. 2 CROMA Contenido General.pmd 2 02/01/2012, 07:20 p.m. Boletín N°144 Serie A - INGEMMET Dirección de Geología Regional RESUMEN El Cuadrángulo de Cerro de Pasco (22-k) se localiza en las ríos distales con intercalaciones de llanura de inundación y deltas altiplanicies interandinas de la parte central del Perú, entre la del Grupo Goyllarizquisga, el cual podría abarcar desde el Jurásico Cordillera Occidental y la Cordillera Oriental. Las ¾ partes del superior hasta el Cretácico inferior. En el Albiano, se tiene una área del cuadrángulo están conformadas por las planicies sedimentación volcano-sedimentaria de la Formación interandinas y forman parte de la cuenca del lago Junín, lugar Chayllacatana. Finalizando el Cretácico inferior se instala donde nace el río Marañón. Hacia la parte norte, el relieve es más nuevamente una plataforma carbonatada de las formaciones Chulec, abrupto, formado por valles en «V», los cuales son efecto de la Pariatambo y Jumasha, que alcanza hasta finales del Cretácico erosión hecha por la red hidrográfica del río Huallaga. superior. La evolución geológica ha ocurrido en 9 ciclos: Precámbrico, Sobre las rocas mesozoicas, en fuerte discordancia angular, se Paleozoico inferior, Paleozoico superior, Pérmico superior-Jurásico encuentra la Formación Pocobamba de edad Paleocena?-Eocena, inferior, Jurásico superior?-Cretácico, Cretácico medio-superior, compuesta por conglomerados y areniscas de abanicos aluviales Paleógeno, Neógeno y Cuaternario; y se han repartido en 5 y ríos proximales. Luego en discordancia, se encuentra la Formación dominios tectonoestratigráficos: Occidental, Central, Surocidental, Calera del Oligoceno, compuesta por lutitas, areniscas y niveles Nororiental y Oriental. En la parte oriental y noroeste del de toba depositados en ambiente lacustre con intervención cuadrángulo de Cerro de Pasco, afloran las rocas más antiguas volcánica. Finalmente, en discordancia angular, se encuentran las de la zona de estudio, el grado de metamorfismo ha permitido tobas de la Formación Huayllay y los conglomerados de la atribuir a estas rocas al Complejo Metamórfico del Marañón cuya Formación Jeroc del Mioceno superior. edad puede llegar al Precámbrico, aunque nuevos datos ponen Los sistemas estructurales han sido determinados en base a datos en duda esta consideración. de campo, relacionándolos con la estratigrafía y la geología de las El Paleozoico inferior está conformado por las areniscas y pizarras zonas aledañas, además de bibliografía de estudios anteriores. Se del Grupo Cabañillas, que afloran en la parte central de la zona de han diferenciado 5 dominios estructurales casi paralelos a la estudio, formando una franja alargada de dirección N-S, la cual dirección andina : el Dominio Occidental, que corresponde a la faja constituye el alto de Cerro de Pasco. La parte superior del Paleozoico plegada y fallada de Marañón, que está compuesto por fallas inferior se encuentra erosionada, y no es posible observar el inversas NO-SE a N-S convergentes al este; el Dominio contacto con las secuencias del Paleozoico superior. El ciclo del Suroccidental, ubicado entre las fallas Huallay y proyección de la Paleozoico superior-Triásico inferior está conformado por areniscas falla Tarma; el Dominio Central, caracterizado por fallas inversas y lutitas negras de medio fluvial, correspondientes a la parte inferior N-S convergentes al oeste; el Dominio Nororiental constituido por del Grupo Ambo. Luego se tiene una secuencia volcánica de riolitas fallas inversas N-S convergentes tanto al oeste y al este, y el con fiames, sobreyacida en discordancia por una secuencia Dominio Oriental, con fallas inversas N-S convergentes al oeste. arenosa intercalada con calizas fosilíferas pertenecientes los grupos Las rocas ígneas intrusivas se encuentran divididas en 6 eventos. Tarma-Copacabana del Pérmico inferior. El Grupo Mitu, atribuido El evento más antiguo es el Carbonífero, compuesto por granitos al Pérmico medio-superior-Triásico inferior, se encuentra en de textura fanerítica; seguido del Pérmico superior-Triásico inferior, discordancia sobre las areniscas y calizas de los grupos Tarma- constituido por granitos. Posteriormente, le sigue el evento del Copacabana indivisos, y está compuesto principalmente de Eoceno, compuesto por manifestaciones subvolcánicas ubicadas areniscas, conglomerados
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