News Release Sep 19,1997 as carried by Stockwatch
Aeromagnetic data acquired for Chinchaga Craton diamond properties Marum Resources Inc MMU Shares issued 14,903,616 Sep 23 close $0.165 Wed 24 Sept 97 News Release Mr Richard Boulay reports, The company reports that it has acquired high resolution aeromagnetic data covering its Chinchaga Craton diamond properties in northern Alberta. Data acquisition was performed by Spectra Exploration Geoscience Corp of Calgary. Spectra is currently processing the data for high frequency, shallow targets which also have deep root expressions. A preliminary review of the unprocessed data indicates several areas of potential interest, including localized, high frequency anomalies which are powerful enough to appear on the total field magnetic maps. Marum's Chinchaga Craton diamond properties consist of a 100% interest in 400,000 acres of permits distributed in a north-south pattern adjacent to and immediately west of a property which Mount Hope Resources recently reported as containing over 20 anomalies which appear in a cluster. Marum's properties were specifically acquired to capture a coincidence of diverse geological conditions which favour the localization of kimberlite pipe targets. These conditions include: A requirement that the underlying craton possess thick, cool roots that have not been subjected to thermal re-heating. Both the Chinchaga Craton and the associated Buffalo Head Craton have these characteristics. The Alberta Geological Survey report "Diamonds in Alberta" favours the Chinchaga over the Buffalo Head as a potential diamond host terrane on the basis of the Chinchaga's mix of Archean isotope geochemistry and cooler, deeper crustal roots. The existence of a pronounced gravity low within the craton to pinpoint the location of super-cool root zones. Regional gravity data clearly shows that the Chinchaga and Buffalo Head Cratons form a single circular unit, similar in size and shape to the Slave Craton in the NWT. A pronounced ring shaped gravity low occurs within the Chinchaga-Buffalo Head Craton complex. Both the Ashton and Monopros kimberlite pipes occur on this low-gravity ring. The core Ashton permits appear to cover approximately 30 degrees of circumference on the east side of the Chinchaga-Buffalo Head low-gravity ring. The Marum properties cover approximately 45 degrees of circumference on the west side of the ring. The presence of deep, crustal faults. It appears that the distribution of kimberlite pipes in northern Alberta is directly related to the deep, crustal scale faults associated with the Peace River Arch, especially in areas which contain swarms of smaller stress release faults. Satellite imagery indicates that this apparently essential structural combination exists in the core Ashton permit block as well as in Marum's Chinchaga properties where the Chinchaga valley itself is the surface expression of a deep crustal fault. The presence of Shaftsbury Embayments. The Wabasca, Peace River and Chinchaga erosional embayments expose the upper Cretaceous Shaftsbury formation to the surface. The Shaftsbury formation is now known to be rich in kimberlitic volcanic ash layers. If, as is suspected, the Ashton pipes are of Shaftsbury age (90 to 95 million years old) the properties located in the Shaftsbury embayments will have the potential for Shaftsbury age pipes to occur at surface rather than being deeply buried by overlying sedimentary rocks. The Marum Chinchaga properties and the Ashton Buffalo Head property are both located in Shaftsbury embayments. The presence of diamond indicator minerals. Marum has previously reported the existence of indicator minerals in the area and the recovery of two clear microdiamonds from a trench sample of a Cretaceous age sedimentary rock outcrop located on one of its Chinchaga Craton properties. A geological and sampling crew will be dispatched to the Chinchaga area in advance of the receipt of the processed aeromagnetic data in order to investigate the stronger anomalies. (c) Copyright 1997 Canjex Publishing Ltd. canada-stockwatch.com |