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Orex Minerals Inc V.REX

Alternate Symbol(s):  ORMNF

Orex Minerals Inc. is a Canada-based mineral exploration company. The Company is focused on precious and base metals exploration in Mexico and Canada. The Company is engaged primarily in the acquisition and exploration and evaluation of assets. It has several projects, including two projects located in Durango State, Mexico, the Sandra Silver-Gold Project with Pan American Silver Corp. and the Coneto Gold-Silver Project with Fresnillo PLC. The third project is the Valenciana Gold-Silver-Base Metals Project in Zacatecas State, Mexico. The fourth project is the Jumping Josephine Gold Project in British Columbia, Canada. The Sandra Project is situated north of the town of Tepehuanes, Durango, in the heart of the Mexican Silver Trend, midway between the mining districts of Tovar and Guanacevi. The Coneto Silver-Gold Project is adjacent to the village of Coneto de Comonfort, centrally positioned within the Mexican Silver Trend, over 100 km north of the city of Durango, Mexico.


TSXV:REX - Post by User

Bullboard Posts
Post by AlternativeViewon Nov 04, 2016 8:05pm
81 Views
Post# 25426921

IOGC Deposit At The Chupaderos Caldera In Durango

IOGC Deposit At The Chupaderos Caldera In Durango
I'm not going to bother to fix the formatting. Look here on P1345 instead:
https://www.rodolfocorona.com/archivos/pdf/2007_Corona_Esquivel_et_al_CM_SGA.pdf

We see that a (reasonably) nearby caldera at Durango hosts an IOGC deposit. So, was the classification of Sandra-Escobar as a "caldera" a precipitating factor in the radiometric survey?


3.2.1
Cerro de Mercado (Durango).
Cerro de Mercado ore deposit is located in
the City of Durango (Dur
ango State, Mexico).
Lyons (1998) and Labarthe
et al
. (1990) indi-
cate that this deposit is
located within the Chu-
paderos Caldera, a large rhyolitic volcanic cen-
ter of Oligocene age
(30.8-30.1 Ma, Swanson
et
al.
1978). The caldera consists of a series of
units, beginning ash-flow tuffs (Aguila Forma-
tion) that filled the caldera. The last volcanic
Cacaria Formation (rhyolitic domes, intrusions,
and airfall tuffs) host th
e iron-rich bodies of
Cerro de Mercado (Lyons, 1988).

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