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Oroco Resource Corp V.OCO

Alternate Symbol(s):  ORRCF

Oroco Resource Corp. is a Canadian mineral exploration company. The Company is engaged in the acquisition and exploration of mineral properties in Mexico. It holds a net 85.5% interest in those central concessions that comprise 1,173 hectares (ha) (the Core Concessions) of The Santo Tomas Project, located in northwestern Mexico. It also holds an 80% interest in an additional 7,861 ha of mineral concessions surrounding and adjacent to the Core Concessions (for a total Project area of 9,034 hectares, or 22,324 acres). The Project hosts a large, outcropping porphyry copper deposit comprised of fracture-hosted and disseminated copper and molybdenum sulphides with significant gold and silver credits. Its Xochipala Property is comprised of the Celia Gene (100 ha) and the contiguous Celia Generosa (93 ha) concessions. Its Salvador Property is a 100-hectare mining concession, which lies around 25 kilometers (kms) to the west of the Xochipala Property and 30 kms west of Chilpancingo, Guerrero.


TSXV:OCO - Post by User

Bullboard Posts
Comment by calicheon Feb 10, 2018 2:21pm
77 Views
Post# 27539138

RE:RE:Majors with money!

RE:RE:Majors with money!it may be worth more!

billions of pounds of copper millions of ounces of gold and silver and 100s of million pounds of moly 

santo tomas is a big deal

here is a head start on your DD


The Laramide orogeny in southern U.S. and Northern Mexico is represented by a period of intense subduction related magmatism and volcanism, significant copper molybdenum-lead-zinc-silver-gold metallogenesis, and late-stage northeast-directed compressional tectonics 


The sustained magmatic activity along the North American Cordillera during late Mesozoic and Paleogene times produced the emplacement of numerous porphyry copper deposits. This activity extended by most of western Mxico, particularly along the northwestern part of the country. This region, along with Arizona and New Mexico in the United States, contains one of the most important centers of copper mineralization on Earth. Most of the Mexican deposits lie in the eastern part of the Laramide magmatic belt (90-40 Ma) and were formed predominantly between 75 and 50 Ma. The largest deposits occur in northeastern Sonora and are represented by Cananea (∼30 Mt Cu) and La Caridad (∼8 Mt Cu). The copper ores are locally accompanied by molybdenum, tungsten, gold, and other metals. However, the metal distribution is apparently coupled with major changes in the basement of emplacement
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