2 edition of The Mesozoic Carpentaria Basin and the Cainozoic Karumba Basin, north Queensland found in the catalog.
The Mesozoic Carpentaria Basin and the Cainozoic Karumba Basin, north Queensland
|Other titles||Carpentaria and Karumba basins, north Queensland.|
|Statement||J. Smart ... [et al.].|
|Series||Bulletin ;, 202, Bulletin (Australia. Bureau of Mineral Resources, Geology and Geophysics) ;, 202.|
|Contributions||Smart, J., Australia. Bureau of Mineral Resources, Geology and Geophysics.|
|LC Classifications||QE340 .A39 no. 202, QE675 .A39 no. 202|
|The Physical Object|
|Pagination||vi, 73 p. :|
|Number of Pages||73|
|LC Control Number||90134692|
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Get this from a library. The Mesozoic Carpentaria Basin and the Cainozoic Karumba Basin, north Queensland. [J Smart; Australia. Bureau of Mineral Resources, Geology and Geophysics.;]. The Mesozoic Carpentaria Basin and the Cainozoic Karumba Basin, north Queensland / J.
Smart [et al.] Geology of the Hodgkinson and Laura basins, Queensland [cartographic material] / compiled by the Bureau Tectonic units and structural subdivisions (with aeromagnetic and gravity data) Bowen Basin. The Mesozoic Carpentaria and Cainozoic Karumba Basins, Queensland. Bureau of Mineral Resources, Aus tralia-Bulletin.
Notes on the Mesozoic and Caino zoic stratigraphy of the Georgetown area. The Mesozoic Carpentaria Basin and the Cainozoic Karumba Basin, North Queensland; Department of National Development & Energy, Bureau of Mineral Resources, Geology and Geophysics: Canberra, Australia, ; p.
Cited by: 3. Carpentaria Basin ; Karumba Basin. Geology, mineralisation and company exploration in the Croydon and Gilbert River and Esmeralda sheet areas, North Queensland / T.J. Denaro &. The BMR Journal of Australian Geology & Geophysics was started in March Init became the AGSO Journal of Australian Geology & Geophysics.
After 24 years, 17 volumes and a change of policy, it was incorporated into the Australian Journal of Earth Sciences. Karst and Pseudokarst in Northern Australia. and terminal surfaces are related to cycles of activity within the Cainozoic Karumba Basin.
They have been correlated with surfaces elsewhere in. Mesozoic and Cainozoic geology of the Lawn Hill, Westmoreland, Mornington, and Cape Van Diemen Sheet areas, Queensland.
/ Lunar Laser Ranger site, Orroral Valley ACT, foundation investigation - NOTE BY MR. PHILLIPS, C.E. The author of this book, the late Edward Palmer, was himself one of that brave band of pioneer squatters who in the early sixties swept across North Queensland with their flocks and herds, settling, as if by magic, great tracts of hitherto unoccupied country, and thereby opening several new ports on the east coast and on the shores of the Gulf of Carpentaria, to.
Grigorescu, M. Mineralogy of the north-eastern Bowen Basin and north-eastern Surat Basin, Queensland (CD ROM). Geological Survey of Queensland - Record /02 22pp REFID: On November 2,we entered into an agreement with Iron Duyfken Pty Ltd to acquire three (3) project areas in the Georgina Basin of Queensland, Australia.
We agreed to pay A$, and issueshares of Common Stock as consideration. The Maureen uranium deposit is associated with Late Palaeozoic felsic intrusives and volcanics in north-eastern Queensland, Australia. It is located towards the western margin of the Newcastle Range-Featherbed volcanic field.
Ben Lomond is some 50 km WSW of the city of Townsville, while Maureen is a further km to the NW of the similar Ben Lomond deposit (which is 50 km west of Townsville.
Nov 16, · The Great Artesian Basin (GAB) in Australia underlies semi-arid and arid regions across million km2 or one-fifth of Australia.
The basin’s groundwater resources were discovered around and their development allowed pastoral activities, homestead and town water supplies, and petroleum and mining ventures to exist. The GAB is a multi-layered confined aquifer system, with.
The Mesozoic Carpentaria Basin and the Cainozoic Karumba Basin, North Queensland (Bulletin ) Department of National Development & Energy, Bureau of Cited by: 4. The sedimentary manganese ore deposit of Groote Eylandt, Australia, is an example of the Orthoquartzite-Glauconite-Clay Association, and was formed during a short Cenomanian Age transgression and regression across the Middle Proterozoic sandstone basement of the niarbylbaycafe.com by: Full text of "Early days in North Queensland / #c by Edward Palmer" See other formats.
LEGEND INTERNATIONAL HOLDINGS INC Securities Registration Statement (S-1/A) The major structural feature in the McArthur Basin is the north to north-west trending Batten Trough or Batten Fault Zone approximately 70 kilometres wide, to which Legend’s holdings lie to the east. adjacent to the Georgina Basin which hosts Legend’s.
records about 25 ages between 0 and 62 Ma. At Mt Leyshon in north Queensland a 40Ar/39Ar date (Vasconcelos, a,b) verifies the K/Ar ages. From a pre-Jurassic regolith profile on Kangaroo Island two samples of alunite were collected but they generated ages of and Ma.
Full text of "Vertebrate palaeontology of Australasia" See other formats. AGENCY AGREEMENT filed by Legend International Holdings Inc on August 7th,arrangements or commitments based upon the book value, income or any other attribute of the Company or the Subsidiaries.
services will be negotiated separately and in good faith and be consistent with the fees paid to investment banks in North America for. The geology of Queensland is divided into three main structural divisions: the Proterozoic shield in the north-west and north, the PalaeozoicMesozoic Tasman Orogenic Zone (including the intracratonic Permian to Triassic Bowen and Galilee Basins) in the east, and overlapping Mesozoic rocks of the Great Australian Basin (Figure 1).26A national-scale vulnerability assessment of SWI: Literature review, data review and method development Figure 26 Massacre Inlet area on the southern shores of the Gulf of Carpentaria, just on the Queensland side of the Queensland/NT border.
Well developed small strand plains are broken up and separated by tidal flats The basin is.boundaries at rates of to 10 km/yr (Bott and Dean ) may widen convergent plate boundary zones in continents to extensive regions of complex 'foreland' deformation (Vilotte et al.
), such as the widespread late MesozoicCainozoic deformation and basin inversion of north-west Europe in the Alpine foreland (Dewey ).