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Rockley Volcanics

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Journal Article
Journal: Economic Geology
Published: 01 October 1995
Economic Geology (1995) 90 (6): 1553-1569.
... quartzite and quartz-mica schist of the Triangle Group, immediately below ultramafic shoshonitic volcanic rocks of the Rockley Volcanics. Geologic relationships imply that mineralization and alteration are probably synchronous with later stages of contact metamorphism and, hence, postdate upper greenschist...
Series: Geological Society, London, Special Publications
Published: 01 January 2003
DOI: 10.1144/GSL.SP.2003.213.01.13
EISBN: 9781862394612
...-term (hours to months) changes in SO 2 flux can be a good proxy for magma eruption rate. The relatively high SO 2 production rate during the early stages of renewed dome growth at SHV may be due in part to changes in vent and conduit permeability during the ‘residual’ volcanic activity between...
Image
F ig . 3. Ordovician to Early Silurian <b>volcanic</b> (and intrusive) rocks in th...
Published: 01 December 2003
F ig . 3. Ordovician to Early Silurian volcanic (and intrusive) rocks in the eastern Lachlan fold belt of New South Wales (modified from Scheibner and Basden, 1998 ). The Junee-Narromine, Molong, Rockley-Gulgong, and Kiandra volcanic belts are shown.
Journal Article
Journal: Economic Geology
Published: 01 June 2014
Economic Geology (2014) 109 (4): 1117-1135.
... to the east of the Cadia district, occurring as the arc volcanic rocks of the Rockley-Gulgong volcanic belt (RGVB). KVB = Kiandra volcanic belt. Our study provides new geologic descriptions of volcanosedimentary units from across the Cadia district. Reconstruction of the facies architecture...
FIGURES | View All (17)
Image
U–Pb probability and ε Hf  plots from Early to Middle Ordovician rocks of t...
Published: 14 July 2016
Fig. 13. U–Pb probability and ε Hf plots from Early to Middle Ordovician rocks of the Macquarie Volcanic Province (formerly Macquarie Arc), Lachlan Orogen. (A, B, C) Phase 1 MIT Mitchell Formation. (D, E, F) WAH1 Phase 2 Fairbridge Volcanics. (G, H, I) OR3 Phase 4 Rockley Volcanics. (J, K, L
Journal Article
Published: 31 July 2014
Journal of the Geological Society (2014) 171 (5): 723-736.
... without regard for potential displacements or temporal constraints. Fergusson & Colquhoun (1996) and Colquhoun et al . (1999) described conformable contacts in the northern part of the Rockley–Gulgong Volcanic Belt, also dismissed by Meffre et al . (2007) . They detailed a conformable...
FIGURES | View All (6)
Series: Special Publications of the Society of Economic Geologists
Published: 01 January 2013
DOI: 10.5382/SP.17.11
EISBN: 9781629491639
... in four N-trending structural belts that crop out poorly over a strike length of ~450 km (Fig. 9 ). These belts are, from west to east, the Junee-Narromine, Molong, and Rockley-Gulgong volcanic belts, which form the three main exposed parts of the arc. The Kiandra volcanic belt crops out to the south...
FIGURES | View All (12)
Journal Article
Journal: Economic Geology
Published: 01 December 2003
Economic Geology (2003) 98 (8): 1607-1636.
...F ig . 3. Ordovician to Early Silurian volcanic (and intrusive) rocks in the eastern Lachlan fold belt of New South Wales (modified from Scheibner and Basden, 1998 ). The Junee-Narromine, Molong, Rockley-Gulgong, and Kiandra volcanic belts are shown. ...
FIGURES | View All (23)
Image
Figure 3. Middle Ordovician to Early Silurian tectonic reconstruction of La...
in > Geology
Published: 01 December 2003
Tabberabberan (Tabb.) deformation. Acronyms: JNVB— Junee-Narromine volcanic belt; MVB—Molong volcanic belt; RGVB—Rockley-Gulgong volcanic belt; KVB—Kiandra volcanic belt; MF—Moyston fault; AF—Avoca fault; HF—Heathcote fault; KF—Kancoona fault; GF—Gilmore fault; HT-LP—high temperature–low pressure.
Journal Article
Journal: Economic Geology
Published: 01 June 2014
Economic Geology (2014) 109 (4): 1051-1077.
... , 2009 ; Fergusson, 2009 ). The poorly outcropping Junee-Narromine volcanic belt is the most westerly and longest volcanic belt in the Macquarie Arc ( Fig. 1 ). The Molong and Rockley-Gulgong belts to the east are proposed to have been rifted from the main arc, represented by the Junee-Narromine...
FIGURES | View All (12)
Image
Regional geologic map of the district surrounding the E26 deposit. A. Ordov...
Published: 01 June 2014
Fig. 1 Regional geologic map of the district surrounding the E26 deposit. A. Ordovician volcanic belts and the location of the Parkes region. JNVB = Junee-Narromine volcanic belt, KVB = Kiandra volcanic belt, MVB = Molong volcanic belt, RGVB = Rockley-Gulgong volcanic belt (from Walshe et al
Image
Geology of the Late Ordovician Macquarie Arc of New South Wales. The Ordovi...
Published: 01 June 2014
of the Cadia district, occurring as the arc volcanic rocks of the Rockley-Gulgong volcanic belt (RGVB). KVB = Kiandra volcanic belt.
Journal Article
Journal: Geology
Published: 01 December 2003
Geology (2003) 31 (12): 1073-1076.
... Tabberabberan (Tabb.) deformation. Acronyms: JNVB— Junee-Narromine volcanic belt; MVB—Molong volcanic belt; RGVB—Rockley-Gulgong volcanic belt; KVB—Kiandra volcanic belt; MF—Moyston fault; AF—Avoca fault; HF—Heathcote fault; KF—Kancoona fault; GF—Gilmore fault; HT-LP—high temperature–low pressure. ...
FIGURES
Journal Article
Published: 14 July 2016
Canadian Journal of Earth Sciences (2016) 53 (11): 1372-1415.
...Fig. 13. U–Pb probability and ε Hf plots from Early to Middle Ordovician rocks of the Macquarie Volcanic Province (formerly Macquarie Arc), Lachlan Orogen. (A, B, C) Phase 1 MIT Mitchell Formation. (D, E, F) WAH1 Phase 2 Fairbridge Volcanics. (G, H, I) OR3 Phase 4 Rockley Volcanics. (J, K, L...
FIGURES | View All (25)
Journal Article
Journal: Economic Geology
Published: 01 June 2014
Economic Geology (2014) 109 (4): 1035-1050.
...Fig. 1 Regional geologic map of the district surrounding the E26 deposit. A. Ordovician volcanic belts and the location of the Parkes region. JNVB = Junee-Narromine volcanic belt, KVB = Kiandra volcanic belt, MVB = Molong volcanic belt, RGVB = Rockley-Gulgong volcanic belt (from Walshe et al...
FIGURES | View All (13)
Series: Reviews in Economic Geology
Published: 01 January 2008
DOI: 10.5382/Rev.15.03
EISBN: 9781629490229
... in this part of the province. In contrast, large east-west–trending dome and basin folds, formed in the western part of the province, expose granitoid-greenstone terrane in the core of the domes. Important examples are the Milli Milli, Jeerinah, and Rockley anticlines and the Brockman, Hardey, and Turner...
FIGURES | View All (23)