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Reaphook Hill and Mount Frome (a tenement group having amalgamated expenditure commitments, which is part of the Flinders Ranges Project). Joint annual reports for the period 4/8/2001 to 1/7/2015.
During the third year of exploration nominally ending on 1/7/2002 [and subsequent to the starting date of 5/3/2002 for the application of provisions of the Flinders Ranges Project's multi-tenement Amalgamation of Expenditure Agreement (AEA), whence...-
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Published: 07 Aug 1915
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MR 002 Short review of mining operations in the State of South Australia during the half-year ended June 30th, 1904
Articles include reports on: Copper: Wallaroo and Moonta, Paramatta and Yelta, Hamley, Blinman, Burra Burra; Kapunda, Prince Alfred, Lynda, Mutooroo , Paull's, Clara St. Dora and Mount Fitton South Mines, Gold: Tarcoola, Petersburg Mount Torrens,...-
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MR 003 Review of mining operations in the State of South Australia during the half-year ended December 31st, 1904
Articles and summaries are provided for the following: Copper: Wallaroo and Moonta, Paramatta and Yelta, Hamley, Moonta, Blinman, Burra Burra, Kapunda, Sweet Nell (North-West), Mount Gunson (North-West), Prince Alfred, Lynda Mines Gold: Mount...-
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Reaphook Hill. Final report at licence surrender, for the period 1/12/1965 to 13/5/1968.
The reported presence of high geochemical zinc values in the Parachilna Formation rocks exposed there prompted Kennecott Explorations to include the Reaphook Hill outlier of Lower Cambrian sediments into its regional investigation of the stratiform...-
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Published: 25 Mar 1967
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SP 008 Mineral Resources of the Adelaide Geosyncline
This publication has been compiled from a display prepared for the launch of SADME Bulletin 53, held at the Australian Mineral Foundation on 7 December 1987. The importance and diversity of commodities found in the Geosyncline are highlighted in the...-
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ExpNotes PARACHILNA (v2): Explanatory Notes PARACHILNA (second edition, 1999)
The PARACHILNA map area (31 to 32°S, 138 to 139.5°E) occupies the central Flinders Ranges which are made up of folded, mostly marine sedimentary Neoproterozoic and Cambrian rocks of the Adelaide Geosyncline, and adjoining plains underlain by Cainozoic...-
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