Geochronology of Mexican mineral deposits. VIII: the Zacatepec polymetallic skarn, Oaxaca


Por: Camprubi, Antoni, Cabrera-Roa, Miguel Angel, Gonzalez-Partida, Eduardo, Lopez-Martinez, Margarita

Publicada: 1 ene 2019
Categoría: Earth and planetary sciences (miscellaneous)

Resumen:
The Zn-Pb-Ag(-W) skarn deposits at Zacate-pec (or Miiygixy) in Oaxaca are associated with jocks of the Sierra Madre del Sur (SMS) magmatic province, and located in its easternmost part, in southern Mexico. This region consists of Eocene to Miocene calc-alkaline hypabyssal and volcanic rocks, with intermediate to felsic compositions that intrude or overlie Cretaceous carbonate sequences. Prograde mineralization in the Zacatepec skarn deposits was dated by means of the Ar-40/Ar-39 method in a sample of the granitic hypabyssal body, with which the formation of these deposits is directly associated. The isochron ages thus yielded are 17.52 +/- 0.14 Ma for biotite and 17.33 +/- 0.40 Ma for hornblende. Such ages are in accordance with several other magmatic-hydmthermal deposits (epithermal. skarn. and porphyry-type deposits) that are hosted by Miocene rocks in central Oaxaca state. Deposits in the region with known ages for Miocene hypabyssal rocks with which they are closely related are Taviche,Lachigalla, Cobre Grande, Aurena, Natividad, Altagracia-Aguila-Arista, Santa Margarita-Azucena, and Guiclavazar. The plausible ages for these ore deposits determine a time bracket between < 23.8 and < 13.01 Ma (early to middle Miocene) that can be considered as favorable for the finding of magmatic-hydmthermal car deposits. The latter can be tentatively used to define a new metallogenic period that corresponds to a new metallogenic province, for which the rocks derived from the Miocene magmatism of the SMS constitute the metallotect. Although such metallogenic activity has not been altogether overlooked, no previous papers have focused on its relevance and extent in space and time. Therefore, this province constitutes the fifth Miocene mineralized region known in Mexico. besides the southernmost Sierra Madre Occidental, the Trans-Mexican Volcanic Belt, the Gulf of California. and the alkaline province in Chiapas.

Filiaciones:
Camprubi, Antoni:
 Univ Nacl Autonoma Mexico, Inst Geol, Ciudad Univ, Coyoacan 04510, Cdmx, Mexico

 Instituto de Geología, Universidad Nacional Autónoma de México. Ciudad Universitaria, Coyoacán, CDMX, 04510, Mexico

Cabrera-Roa, Miguel Angel:
 Univ Nacl Autonoma Mexico, Ciencias Tiena, Ciudad Univ, Coyoacan 04510, Cdmx, Mexico

 Posgrado en Ciencias de la Tierra, Universidad Nacional Autónoma de México. Ciudad Universitaria, Coyoacán, CDMX, 04510, Mexico

Gonzalez-Partida, Eduardo:
 Univ Nacl Autonoma Mexico, Ctr Geociencias, Blvd Juriquilla 3001, Queretaro 76230, Qro, Mexico

 Centro de Geociencias, Universidad Nacional Autónoma de México. Boulevard Juriquilla 3001, Querétaro, Qro., 76230, Mexico

Lopez-Martinez, Margarita:
 Ctr Invest Cient & Educ Super Ensenada, Carretera Ensenada Tijuana 3918, Ensenada 22860, Baja California, Mexico

 Centro de Investigación Científica y Educación Superior de Ensenada. Carretera Ensenada-Tijuana No. 3918, Zona Playitas, Ensenada, B.C., 22860, Mexico
ISSN: 14053322
Editorial
UNIV NACIONAL AUTONOMA MEXICO, INST GEOGRAFIA, CIUDAD UNIV, FAC ECONOMIA, CIRCUITO INTEROR S-N, 1ER PISO, EDIFICIO B, COYOACAN C P, 04510, MEXICO, México
Tipo de documento: Article
Volumen: 71 Número: 1
Páginas: 207-218
WOS Id: 000455704700012

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