Evolution Mining
Mr Klein was appointed as Executive Chairman in October 2011, following the merger of Conquest Mining Limited and Catalpa Resources Limited. Previously he served as the Executive Chairman of Conquest Mining.
Prior to that, Mr Klein was President and CEO of Sino Gold Mining Limited, where, along with Mr Askew (Director from 2002 and Chairman from 2005 of Sino Gold) he managed the development of that company into the largest foreign participant in the Chinese gold industry. Sino Gold was listed on the ASX in 2002 with a market capitalisation of A$100 million and was purchased by Eldorado Gold Corporation in late 2009 for over A$2 billion. It became an ASX/S&P 100 Company, operating two award-winning gold mines and engaging over 2,000 employees and contractors in China. Prior to joining Sino Gold (and its predecessor) in 1995, Mr Klein was employed at Macquarie Bank and PricewaterhouseCoopers.
Mr Klein was a Non-Executive Director of the Lynas Corporation Limited from August 2004 to May 2017, a company with operations in Australia and Malaysia and OceanaGold Corporation from December 2009 to July 2014 a company with operations in the Philippines, USA and New Zealand.
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Evolution Mining
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Evolution Mining is a gold company. The Company is engaged in operating, identifying and developing gold related mining projects in Australia and New Zealand. Its segments are Cowal, Mungari, Mt Carlton, Mt Rawdon, Edna May, Cracow, Pajingo, Exploration and Corporate. It owns and operates approximately seven gold mines, including Cowal in New South Wales; Cracow, Pajingo, Mt Carlton and Mt Rawdon in Queensland, and Mungari and Edna May in Western Australia. The Cowal operation is an open pit mining operation with production from a range of different faces within the single pit. The Edna May gold mineralization consists of high-grade reef structures and associated stockwork veining hosted within approximately three en-echelon tonalitic gneiss intrusions (Edna May, Greenfinch and Golden Point). The Mt Carlton project is a high-sulfidation epithermal style deposit with mineralization occurring within felsic volcanic rocks on the northern margin of the Permian Bowen Basin.