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Airborne Gravity 2010 - Geoscience Australia

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<strong>Airborne</strong> <strong>Gravity</strong> <strong>2010</strong><br />

Summary<br />

The De Beers Airship <strong>Gravity</strong> Project<br />

David Hatch 1 and Brad Pitts 2<br />

1 De Beers Group Services, Johannesburg, South Africa<br />

(Now with Gedex Inc, Toronto Canada) (David.Hatch@Gedex.ca)<br />

2 De Beers Prospecting Botswana (Pty) Ltd, Gaborone, Botswana<br />

(Now with Simplicity Projects Botswana (Pty) Ltd, Gaborone Botswana)<br />

(brad@simplicity.co.bw)<br />

To successfully execute a diamond exploration program in Botswana, De Beers Group Exploration<br />

required that a large, high-quality gravity data set be acquired. The 4000 km 2 area could not be<br />

surveyed on the ground within the allotted time, and the noise and resolution levels of existing airborne<br />

gravity gradiometer systems were considered to be inadequate to confidently explore the area.<br />

To rapidly acquire high-quality gravity data, the solution of mounting an existing instrument on a<br />

radically more stable airborne platform was investigated. A Zeppelin airship provided two significant<br />

advantages over a fixed wing aircraft platform for gravity surveying, i.e., it represented a benign<br />

acceleration environment arising from the increased stability, and it could be operated as a slow<br />

moving platform Tests of the Bell Geospace Air-FTG® system mounted in a Zeppelin airship<br />

demonstrated that the data quality was sufficient to achieve the goals of the project.<br />

The challenges of an airship program in Botswana were formidable. The hot summer daytime<br />

temperatures, high elevation, and harsh desert conditions of the survey location combine to produce a<br />

very difficult operating environment. The largest impact on productivity was airship downtime which<br />

was mainly attributed to the deployment of a prototype airship where it was exposed at all times during<br />

maintenance, mooring and surveying to the harsh desert conditions. The weather also accounted for a<br />

significant amount of downtime, although this was not unexpected given the severe summer weather<br />

and strong seasonal winds.<br />

The high-quality airship gravity data allowed kimberlite targets to be confidently selected without the<br />

large number of false targets associated with an equivalent fixed-wing survey (i.e., Type I errors). This<br />

greatly reduced associated follow-up costs and the risk of missing potentially economic bodies (i.e.,<br />

Type II errors). The discovery of a new kimberlite in an area that had been heavily prospected utilising<br />

other exploration techniques is described.<br />

Introduction<br />

The Jwaneng Mine in South-Central Botswana is the richest diamond deposit in the world. Since the<br />

mine opened 25 years ago, the surrounding region has been covered by successive waves of<br />

diamond exploration utilizing both heavy mineral sampling and geophysics. The goal of the exploration<br />

program between 2005 and 2008 was to discover all kimberlites which had the potential to be<br />

economic that had not been detected in these earlier phases.<br />

High resolution magnetic data had been collected over the area, but as is commonly found, some<br />

pipes do not possess a magnetic response. Electromagnetic techniques are often used to assist in the<br />

discovery of non-magnetic kimberlites. However, the area is covered by younger Kalahari Group<br />

sediments up to 100 m thick which can be impregnated with saline ground water. This greatly reduces<br />

the effectiveness of electromagnetic surveys, and a time-domain survey carried out in the area<br />

confirmed that the response of kimberlites would be masked.<br />

Orientation surveys conducted over kimberlites in the Jwaneng cluster showed the majority of these<br />

possessed a significant gravity anomaly. Given the previous exploration experience over the area,<br />

acquisition of airborne gravity data was thought to be the most cost-effective and timely route to make<br />

new discoveries over the roughly 4000 km 2 exploration area. The use of the Bell Geospace full tensor<br />

97

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