Journal articles on the topic 'Gawler Ranges Volcanics'

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1

Pankhurst, M. J., B. F. Schaefer, P. G. Betts, N. Phillips, and M. Hand. "A mesoproterozoic continental flood rhyolite province, the Gawler Ranges, Australia: the end member example of the Large Igneous Province clan." Solid Earth Discussions 2, no. 2 (September 9, 2010): 251–74. http://dx.doi.org/10.5194/sed-2-251-2010.

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Abstract. Rhyolite and dacite lavas of the Mesoproterozoic upper Gawler Range Volcanics (GRV) (>30 000 km3 preserved), South Australia, represent the remnants of one of the most voluminous felsic magmatic events preserved on Earth. Geophysical interpretation suggests eruption from a central cluster of feeder vents which supplied large-scale lobate flows >100 km in length. Pigeonite inversion thermometers indicate eruption temperatures of 950–1100 °C. The lavas are A-type in composition (e.g. high Ga/Al ratios) and characterised by elevated primary halogen concentrations (~1600 ppm Fluorine, ~400 ppm Chlorine). These depolymerised the magma such that temperature-composition-volatile non-Arrhenian melt viscosity modelling suggests they had viscosities of <3.5 log η (Pa s). These physicochemical properties have led to the emplacement of a Large Rhyolite Province, which has affinities in emplacement style to Large Basaltic Provinces. The low viscosity of these felsic magmas has produced a unique igneous system on a scale which is either not present or poorly preserved elsewhere on the planet. The Gawler Range Volcanic Province represents the erupted portion of the felsic end member of the family of voluminous, rapidly emplaced terrestrial magmatic provinces.
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2

Pankhurst, M. J., B. F. Schaefer, P. G. Betts, N. Phillips, and M. Hand. "A Mesoproterozoic continental flood rhyolite province, the Gawler Ranges, Australia: the end member example of the Large Igneous Province clan." Solid Earth 2, no. 1 (March 31, 2011): 25–33. http://dx.doi.org/10.5194/se-2-25-2011.

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Abstract. Rhyolite and dacite lavas of the Mesoproterozoic upper Gawler Range Volcanics (GRV) (>30 000 km3 preserved), South Australia, represent the remnants of one of the most voluminous felsic magmatic events preserved on Earth. Geophysical interpretation suggests eruption from a central cluster of feeder vents which supplied large-scale lobate flows >100 km in length. Pigeonite inversion thermometers indicate eruption temperatures of 950–1100 °C. The lavas are A-type in composition (e.g. high Ga/Al ratios) and characterised by elevated primary halogen concentrations (~1600 ppm fluorine, ~400 ppm chlorine). These depolymerised the magma such that temperature-composition-volatile non-Arrhenian melt viscosity modelling suggests they had viscosities of <3.5 log η (Pa s). These physicochemical properties have led to the emplacement of a Large Rhyolite Province, which has affinities in emplacement style to Large Basaltic Provinces. The low viscosity of these felsic magmas has produced a unique igneous system on a scale which is either not present or poorly preserved elsewhere on the planet. The Gawler Range Volcanic Province represents the erupted portion of the felsic end member of the family of voluminous, rapidly emplaced terrestrial magmatic provinces.
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3

Campbell, E. M., and C. R. Twidale. "The gawler ranges, South Australia: an unusual volcanic massif." Australian Geographer 22, no. 1 (May 1991): 24–33. http://dx.doi.org/10.1080/00049189108703018.

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4

GILES, C. "Petrogenesis of the Proterozoic Gawler Range Volcanics, South Australia." Precambrian Research 40-41 (October 1988): 407–27. http://dx.doi.org/10.1016/0301-9268(88)90078-2.

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5

Allen, S. R., C. J. Simpson, J. McPhie, and S. J. Daly. "Stratigraphy, distribution and geochemistry of widespread felsic volcanic units in the Mesoproterozoic Gawler Range Volcanics, South Australia*." Australian Journal of Earth Sciences 50, no. 1 (February 2003): 97–112. http://dx.doi.org/10.1046/j.1440-0952.2003.00980.x.

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6

Fraser, G. L., R. G. Skirrow, and A. R. Budd. "Geochronology of Mesoproterozoic gold mineralization in the Gawler Craton, and temporal links with the Gawler Range Volcanics." Geochimica et Cosmochimica Acta 70, no. 18 (August 2006): A185. http://dx.doi.org/10.1016/j.gca.2006.06.371.

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7

Morrow, Nicole, and Jocelyn McPhie. "Mingled silicic lavas in the Mesoproterozoic Gawler Range Volcanics, South Australia." Journal of Volcanology and Geothermal Research 96, no. 1-2 (February 2000): 1–13. http://dx.doi.org/10.1016/s0377-0273(99)00143-2.

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8

Campbell, E. M., and C. R. Twidale. "The evolution of bornhardts in silicic volcanic rocks in the gawler ranges." Australian Journal of Earth Sciences 38, no. 1 (February 1991): 79–93. http://dx.doi.org/10.1080/08120099108727957.

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9

Rajagopalan, Shanti, Shi Zhiqun, and Robert Major. "Geophysical Investigations of Volcanic Terrains: A Case History from the Gawler Range Volcanic Province, South Australia." Exploration Geophysics 24, no. 3-4 (September 1993): 769–78. http://dx.doi.org/10.1071/eg993769.

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10

Peucat, J. J., R. Capdevila, C. M. Fanning, R. P. Ménot, L. Pécora, and L. Testut. "1.60 Ga felsic volcanic blocks in the moraines of the Terre Adélie Craton, Antarctica: Comparisons with the Gawler Range Volcanics, South Australia." Australian Journal of Earth Sciences 49, no. 5 (October 2002): 831–45. http://dx.doi.org/10.1046/j.1440-0952.2002.00956.x.

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11

Agangi, Andrea, Jocelyn McPhie, and Vadim S. Kamenetsky. "Magma chamber dynamics in a silicic LIP revealed by quartz: The Mesoproterozoic Gawler Range Volcanics." Lithos 126, no. 1-2 (September 2011): 68–83. http://dx.doi.org/10.1016/j.lithos.2011.06.005.

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12

Chapman, N. D., M. Ferguson, S. J. Meffre, A. Stepanov, R. Maas, and K. J. Ehrig. "Pb-isotopic constraints on the source of A-type Suites: Insights from the Hiltaba Suite - Gawler Range Volcanics Magmatic Event, Gawler Craton, South Australia." Lithos 346-347 (November 2019): 105156. http://dx.doi.org/10.1016/j.lithos.2019.105156.

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13

Ferguson, Matthew R. M., Kathy Ehrig, and Sebastien Meffre. "Insights into magma histories through silicate-oxide crystal clusters: Linking the Hiltaba Suite intrusive rocks to the Gawler Range Volcanics, Gawler Craton, South Australia." Precambrian Research 321 (February 2019): 103–22. http://dx.doi.org/10.1016/j.precamres.2018.11.015.

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14

McPhie, J., F. DellaPasqua, S. R. Allen, and M. A. Lackie. "Extreme effusive eruptions: Palaeoflow data on an extensive felsic lava in the Mesoproterozoic Gawler Range Volcanics." Journal of Volcanology and Geothermal Research 172, no. 1-2 (May 2008): 148–61. http://dx.doi.org/10.1016/j.jvolgeores.2006.11.011.

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15

Garner, A., and J. McPhie. "Partially melted lithic megablocks in the Yardea Dacite, Gawler Range Volcanics, Australia: implications for eruption and emplacement mechanisms." Bulletin of Volcanology 61, no. 6 (November 23, 1999): 396–410. http://dx.doi.org/10.1007/s004450050281.

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16

Allen, S. R., and J. McPhie. "The Eucarro Rhyolite, Gawler Range Volcanics, South Australia: A >675 km3, compositionally zoned lava of Mesoproterozoic age." Geological Society of America Bulletin 114, no. 12 (December 2002): 1592–609. http://dx.doi.org/10.1130/0016-7606(2002)114<1592:tergrv>2.0.co;2.

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17

McPhie, Jocelyn, Fernando DellaPasqua, Sharon Allen, and Mark Lackie. "New constraints on source location and emplacement mechanisms of extensive felsic units in the Gawler Range Volcanics, South Australia." ASEG Extended Abstracts 2006, no. 1 (December 2006): 1–3. http://dx.doi.org/10.1071/aseg2006ab109.

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18

Roache, M. W., S. R. Allen, and J. McPhie. "Surface and subsurface facies architecture of a small hydroexplosive, rhyolitic centre in the Mesoproterozoic Gawler Range Volcanics, South Australia." Journal of Volcanology and Geothermal Research 104, no. 1-4 (December 2000): 237–59. http://dx.doi.org/10.1016/s0377-0273(00)00208-0.

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19

Ferguson, Matthew R. M., Kathy Ehrig, Sebastien Meffre, and Sandrin Feig. "From magma to mush to lava: Crystal history of voluminous felsic lavas in the Gawler Range Volcanics, South Australia." Lithos 346-347 (November 2019): 105148. http://dx.doi.org/10.1016/j.lithos.2019.105148.

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20

Wade, Claire E., Anthony J. Reid, Michael T. D. Wingate, Elizabeth A. Jagodzinski, and Karin Barovich. "Geochemistry and geochronology of the c. 1585Ma Benagerie Volcanic Suite, southern Australia: Relationship to the Gawler Range Volcanics and implications for the petrogenesis of a Mesoproterozoic silicic large igneous province." Precambrian Research 206-207 (June 2012): 17–35. http://dx.doi.org/10.1016/j.precamres.2012.02.020.

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21

Allen, S. R., J. McPhie, G. Ferris, and C. Simpson. "Evolution and architecture of a large felsic Igneous Province in western Laurentia: The 1.6 Ga Gawler Range Volcanics, South Australia." Journal of Volcanology and Geothermal Research 172, no. 1-2 (May 2008): 132–47. http://dx.doi.org/10.1016/j.jvolgeores.2005.09.027.

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22

Curtis, S., C. Wade, and A. Reid. "Sedimentary basin formation associated with a silicic large igneous province: stratigraphy and provenance of the Mesoproterozoic Roopena Basin, Gawler Range Volcanics." Australian Journal of Earth Sciences 65, no. 4 (May 3, 2018): 447–63. http://dx.doi.org/10.1080/08120099.2018.1460398.

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23

Agangi, Andrea, Vadim S. Kamenetsky, and Jocelyn McPhie. "The role of fluorine in the concentration and transport of lithophile trace elements in felsic magmas: Insights from the Gawler Range Volcanics, South Australia." Chemical Geology 273, no. 3-4 (May 2010): 314–25. http://dx.doi.org/10.1016/j.chemgeo.2010.03.008.

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24

Kamenetsky, V. S., N. Morrow, and J. McPhie. "Origin of high-Si dacite from rhyolitic melt: evidence from melt inclusions in mingled lavas of the 1.6 Ga Gawler Range Volcanics, South Australia." Mineralogy and Petrology 69, no. 3-4 (June 26, 2000): 183–95. http://dx.doi.org/10.1007/s007100070020.

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