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Calgary, Alberta- Newsfile Corp. Elmer B. This intrusive is located on the same structural trend that hosts the Globe-Miami, Resolution and Ray porphyry deposits which have similar age dates and zircon inheritance from basement source rocks as the intrusive at Mineral Mountain. All the data, along with the size of the mineralized footprint, alteration patterns and widespread copper mineralization suggest the Laramide intrusive at Mineral Mountain could host a large porphyry copper system. The IP survey is designed to test the depth extent of the copper mineralization exposed in both targets and establish drill locations for the next phase of exploration.

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Calgary, Alberta- Newsfile Corp. Elmer B.

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This intrusive is located on the same structural trend that hosts the Globe-Miami, Resolution and Ray porphyry deposits which have similar age dates and zircon inheritance from basement source rocks as the intrusive at Mineral Mountain.

All the data, along with the size of the mineralized footprint, alteration patterns and widespread copper mineralization suggest the Laramide intrusive at Mineral Mountain could host a large porphyry copper system.

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The IP survey is designed to test the depth extent of the copper mineralization exposed in both targets and establish drill locations for the next phase of exploration. The geophysical survey consists of nine, m spaced lines designed to test at depths of more than m and will include the historical chargeability anomaly outlined in within Target 1.

Significance of Age Dates: A recent study by Seedorff, et al.

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The ages of the inherited zircon cores correspond closely to the ages of basement rocks implying that basement rocks of similar ages and lithologies contributed to the magmas that produced these Laramide porphyry copper deposits. The study was able to investigate the intrusives hosting the Laramide porphyry copper deposits at various depth due to normal faulting related to extensional tectonics during the Cenozoic period that dismembered and tilted many of these intrusives exposing various depth within the porphyry systems for study.

Source: Seedorff et. The study of the zircons yielded a Laramide age and a significant amount of inheritance from older Precambrian age basement rocks.

The Laramide age dates based on 27 age determinations ranged from 66 to 74 Ma. The Precambrian zircons fall into two statistical groups: younger Proterozoic and older Proterozoic. These Proterozoic dates line up well with the units in the region.

Structural Analysis: An analysis of 1, measurements of dikes and mineralized veins to determine the geometry of the Laramide age intrusive Ritchie gives dates for the Fox Creek type based on points found in association with Middle Woodland ceramics from two New York sites.

Discussion There has been a considerable amount of confusion surrounding the Fox Creek type.

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Here, Steubenville points were recovered from non-ceramic sites dating to the Archaic period. Ritchie in discusses the Steubenville type as it is found in eastern and southern New York.

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However, in his revised edition he notes that these points should be called Fox Creek. Fox Creek points, in contrast to Steubenville points, have been found in association with ceramics which date to the Middle Woodland period.

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Ritchie notes that despite general resemblances in morphology, Steubenville points of the upper Ohio Valley had a history separate from that of the Fox Creek points, which have ceramic associations.



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