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Burstall Granite

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Journal Article
Published: 01 September 1992
Journal of the Geological Society (1992) 149 (5): 693–696.
...I. CARTWRIGHT; N. H. S. OLIVER Abstract Marbles adjacent to the Burstall granite, Mary Kathleen, Australia, record up-temperature fluid flow during contact metamorphism. These fluids were water-rich and probably partially derived from devolatilization reactions. By contrast, Fe-rich skarns closer...
Journal Article
Journal: Economic Geology
Published: 01 November 1987
Economic Geology (1987) 82 (7): 1805–1826.
... mineralization in metasedimentary rocks of the host Corella Formation. Widespread high-temperature contact metasomatism and skarn formation related to the emplacement of the U-rich, 1,730-m.y. A-type Burstall Granite produced large volumes of banded calc-silicate skarn. An Sm-Nd age of 1,766 + or - 80 m.y...
Journal Article
Published: 01 September 1994
Journal of the Geological Society (1994) 151 (5): 803–812.
... the Burstall Granite, Australia Journal of the Geological Society London 1992 149 693 696 Cartwright I. Buick I.S. Millimetre-scale channelled fluid infiltration in Reynolds Range marbles: variations in fluid fluxes and intrinsic permeabilities Journal of the Geological Society London...
Journal Article
Journal: Geology
Published: 01 January 2016
Geology (2016) 44 (1): 15–18.
... protracted fractionation. This enrichment makes granites a plausible passive source of U, provided that orogenic fluids can somehow interact with and extract metals from these typically impermeable rocks. Indeed, Oliver et al. (1999) suggested that leaching of the U-rich Burstall Granite (and/or adjacent...
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Journal Article
Published: 01 December 2012
Mineralogical Magazine (2012) 76 (8): 3003–3017.
...). T able 1. Parameters of disposal system components used in the modelling. Item Material OD * (m) ID * (m) Length (m) Borehole Granite host rock 0.560 Dependent on well design Casing Mild steel 0.454 0.419 >1000 Container Stainless steel 0.360 0.320...
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Image
Schematic illustration of the depositional, diagenetic, and ore-forming evo...
Published: 01 September 2006
). The Burstall igneous event between 1755 and 1730 Ma resulted in incision of the Eastern Creek Volcanics in the west, to the mid-Myally subgroup in the central area, and part way through the Quilalar Formation in the east ( Blake, 1987 ; Jackson et al., 2002 ). By the end of the Burstall igneous event
Journal Article
Journal: Economic Geology
Published: 01 September 2006
Economic Geology (2006) 101 (6): 1159–1188.
...). The Burstall igneous event between 1755 and 1730 Ma resulted in incision of the Eastern Creek Volcanics in the west, to the mid-Myally subgroup in the central area, and part way through the Quilalar Formation in the east ( Blake, 1987 ; Jackson et al., 2002 ). By the end of the Burstall igneous event...
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Journal Article
Published: 01 February 2014
Bulletin de la Société Géologique de France (2014) 185 (2): 75–92.
... calcalkaline Burstall Granite emplaced at 1737 ± 15 Ma, and the enclosing calc-silicates, as well as highly saline fluids derived from evaporites [ Oliver et al. , 1999 ]. An early phase of U and REE enrichment is presumed to have occurred in the skarns, at or near the present orebody and related in time...
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Journal Article
Published: 27 May 2003
Canadian Journal of Earth Sciences (2003) 40 (5): 681–699.
... . Cartwright I. Oliver N.H.S. 1992 . Direction of fluid flow during contact metamorphism around the Burstall Granite, Australia . Journal of the Geological Society , London, 149 : 693 – 696 . Cecile M.P. 1983 . Some aspects of Selwyn Basin structure, northern Selwyn Mountains, Yukon...
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Series: Short Courses
Published: 01 January 2016
DOI: 10.3749/9780921294726.ch10
EISBN: 978-0-921294-72-6
... of shallow-water shelf sedimentary rocks close to the contact with the foliated, coarse-grained Th–U-rich Burstall Granite. The Coralla Formation (1780–1760 Ma) is composed of metamorphosed evaporitic calcsilicate rocks with marble, metapelite, metapsammite and minor metavolcanic rocks. This formation has...
FIGURES
Series: Short Courses
Published: 01 January 2016
DOI: 10.3749/9780921294726.ch06
EISBN: 978-0-921294-72-6
... metamorphosed calc-silicate, mafic to intermediate igneous and sedimentary rocks (see chapter 10 for a more detailed description). The skarn results from extensive hydrothermal interaction between the U–Th-rich high-K calc-alkaline Burstall Granite (1737 ± 15 Ma) and enclosing carbonate rocks with highly saline...
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Journal Article
Published: 24 July 2001
Canadian Journal of Earth Sciences (2001) 38 (7): 1093–1106.
... of Gillam, Manitoba Lamothe and Auclair 1999 SW4-01 0.7 Dune sand, Great Sand Hills, Saskatchewan Wolfe et al. 2001 SW6-01 5 Basal sand, Burstall Sand Hill, Saskatchewan Wolfe et al. 2001 TAG-8, TAG-11 2000,? Fluvial sand, TAGLU core, Mackenzie River estuary, Northwest Territories...
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Series: Short Courses
Published: 01 January 2016
DOI: 10.3749/9780921294726.ch02
EISBN: 978-0-921294-72-6
...-rich A-type high-K calc-alkaline Burstall granite (7–12 ppm U) emplaced at 1737 ± 15 Ma and the enclosing calc-silicate rocks and highly saline fluids derived in part from the evaporitic Corella Formation sedimentary rocks ( Oliver et al. 1999 ). A first phase of U and REE enrichment may have...
FIGURES
Series: Short Courses
Published: 01 January 2013
DOI: 10.3749/9780921294689.ch15
EISBN: 978-0-921294-68-9
...-silicate, mafic to intermediate igneous and sedimentary rocks. Skarn results from an extensive hydrothermal interaction between the U-Th-rich high-K calc-alkaline Burstall Granite (1737 ± 15 Ma) and enclosing carbonate rocks with highly saline fluids derived from evaporite ( Oliver et al. 1999...
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