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Starcore International Mining and El Creston Property development news: The Creston Deposit is largely underlain by foliated Proterozoic Creston Granite and Laramide granitic porphyry and hydrothermal breccia. At the deposit molybdenum +/- copper mineralization are hosted in both hydrothermal breccias and the surrounding quartz vein stockwork. In addition, a supergene copper blanket consisting largely of chalcocite has been identified occurring primarily on the west and south sides of the deposit. The alteration pattern within the deposit is complex resulting from multiple intrusions and overlapping alteration. Low-angle normal faults divide the El Creston deposit in to three main tectonic slices causing sliding towards N-NNE In profile the El Creston deposit can be imaged as a series of tectonic slices, having their root in the footwall of the Creston Fault. Find extra info on Gold producer.

Molybdenite was discovered on the property in 1965 by Newmont Mining Corp. (Newmont). Between 1965 and 1967 Newmont completed limited mapping, sampling, trenching and drilled 26 holes totalling 8100 m (26,578 feet) in length. From 1967 to 1990 minor exploration consisting of thin section and alteration studies and limited drill core sampling was completed. Starcore acquired the property through acquisition of Creston Moly from Bankruptcy in 2015. Exploration at Ajax was concentrated in two drilling programs completed by Newmont Mines in 1967-68 (26 holes-8100.9 metres) and Tenajon Resources Corp 2005-2007 (22 holes-7258.6 metres). Following the 2007 an updated resource calculation was completed by Giroux Consultants the results of which are summarized below.

Mineralization is generally made up of breccia that commonly is concordant with a limestone/shale contact (in the San Martin and San Jose areas) which forms the relatively steeply dipping tronco deposits, these troncos contact the younger volcanic flows (dacite and ignimbrite) where they have formed the more horizontal manto portions of the deposit. The mineralized economic breccia grades from 30 g Ag/t to 250 g Ag/t. Exploration has been concentrated along the NE trending breccia zone however evidence of a northerly trend in area 30 leads us to suspect possible other structures together with 2.0 g Au/t to 30 g Au/t over widths that vary from 1.0 to 17.0 m but average 4.0 m. See additional details on https://starcore.com/.