[meteorite-list] Impact Minerals/CITIC to Drill Meteorite Impact Site in Australia for Nickel
From: Ron Baalke <baalke_at_meteoritecentral.com>
Date: Thu, 26 Aug 2010 16:36:07 -0700 (PDT) Message-ID: <201008262336.o7QNa7Mg016413_at_zagami.jpl.nasa.gov> http://www.mineweb.co.za/mineweb/view/mineweb/en/page674?oid=110310&sn=Detail&pid=102055 Impact Minerals/CITIC to drill huge Sudbury-like WA meteorite impact site for nickel Mineweb August 26, 2001 SUMMARY An infill soil geochemistry survey at Target NH1 at the Yarrabubba Joint Venture Project near Meekatharra in Western Australia has defined two priority drill targets for nickel mineralisation; The Yarrabubba Project covers a large (>50 km) diameter meteorite impact structure that has similar geological features to those at the large Sudbury mining camp in Canada, and that has produced about 20% of the World's nickel; These two areas have not been drilled; A drill programme to test these targets will commence as soon as possible after the statutory Aboriginal Heritage Survey is completed in late September; Impact Minerals has a 20% share of the Yarrabubba Project and is in Joint Venture with CITIC Nickel Australia Pty Ltd (60%) and four private investors (20%). The Yarrabubba Impact Structure Impact Minerals' 20%-owned Yarrabubba Project, located 50 km south east of Meekatharra in Western Australia, has most of the geological characteristics of the World Class Sudbury mining camp in Canada which has produced about 20% of the World's nickel. It is generally accepted that a major meteorite impact occurred at Sudbury and that this gave rise to the many large nickel-copper-PGE deposits in that area. The Yarrabubba Joint Venture tenements cover about 1,200 sq km. Within these there is a very large magnetic low in regional airborne magnetic data and outcrops of distinctive geological structures indicative of shock metamorphism which have been interpreted (in published scientific papers) to be caused by a major meteorite impact. The feature in this area is called the Yarrabubba Impact Structure. Interpretation of close-spaced airborne magnetic data flown by the Yarrabubba Joint Venture has defined in more detail the large magnetic low (Figure 1). It is at least 50 km long and up to 15 km wide and is interpreted to be caused by both the meteorite impact and by related subsequent hydrothermal fluids that may form mineral deposits within the intensely fractured rocks. These fluids have caused extensive magnetite destruction and development of sericite, an alteration mineral. The airborne magnetic data has also revealed multiple radial and concentric structures prospective for deposits of nickel, copper and platinum group metals, similar to those which host nickel deposits at the Sudbury mining camp. Soil Geochemistry Results Previous soil geochemistry programmes at Yarrabubba identified Target NH1 as a highly ranked area of about 10 sq km that warranted infill soil sampling to define specific drill targets (Figure 1). A programme of 1,494 soil samples taken at a spacing of 50 m by 50 m was completed in the June Quarter 2010. The samples were submitted for multi-metal analysis by the MMI-M partial digest method at SGS Laboratories in Perth Two areas, called NH1A and NH1B, contain significant nickel responses of between 10 and 58 times background and which are each coincident with a north west to south east trending zone of linear magnetic anomalies interpreted to be part of a major concentric fault related to the impact event. The two areas are coincident with strong magnetic gradients (Figure 2). At Target NH1A the peak nickel responses are in part coincident with strong cobalt responses of between 20 and 55 times background and weak copper responses of between 5 and 6 times background. At Target NH1B the peak nickel responses are sub-parallel to and are partly coincident with modest copper responses of between 6 and 10 times background. The south east part of NH1B is also coincident with modest to strong cobalt responses of between 10 and 50 times background. Drill Programme Applications for Aboriginal heritage surveys and Government environmental approvals were lodged in the June Quarter. The Heritage Survey is expected to be completed by the end of September and Government approvals are due shortly. A drill programme will commence as soon as possible after the statutory approvals have been received. There are many other smaller areas containing elevated nickel responses that may warrant further exploration if the drilling at NH1A and NH1B is encouraging. Received on Thu 26 Aug 2010 07:36:07 PM PDT |
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