Academic literature on the topic 'Olympic IOCG Province'
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Journal articles on the topic "Olympic IOCG Province"
Reid, Anthony. "The Olympic Cu-Au Province, Gawler Craton: A Review of the Lithospheric Architecture, Geodynamic Setting, Alteration Systems, Cover Successions and Prospectivity." Minerals 9, no. 6 (June 20, 2019): 371. http://dx.doi.org/10.3390/min9060371.
Full textCherry, A. R., V. S. Kamenetsky, J. McPhie, J. M. Thompson, K. Ehrig, S. Meffre, M. B. Kamenetsky, and S. Krneta. "Tectonothermal events in the Olympic IOCG Province constrained by apatite and REE-phosphate geochronology." Australian Journal of Earth Sciences 65, no. 5 (May 20, 2018): 643–59. http://dx.doi.org/10.1080/08120099.2018.1465473.
Full textKontonikas-Charos, Alkis, Cristiana L. Ciobanu, Nigel J. Cook, Kathy Ehrig, Roniza Ismail, Sasha Krneta, and Animesh Basak. "Feldspar mineralogy and rare-earth element (re)mobilization in iron-oxide copper gold systems from South Australia: a nanoscale study." Mineralogical Magazine 82, S1 (February 28, 2018): S173—S197. http://dx.doi.org/10.1180/minmag.2017.081.040.
Full textSillitoe, Richard H., Georgi Magaranov, Veselin Mladenov, and Robert A. Creaser. "ROSEN, BULGARIA: A NEWLY RECOGNIZED IRON OXIDE-COPPER-GOLD DISTRICT." Economic Geology 115, no. 3 (May 1, 2020): 481–88. http://dx.doi.org/10.5382/econgeo.4731.
Full textGauthier, Michel, and Francis Chartrand. "Metallogeny of the Grenville Province revisited." Canadian Journal of Earth Sciences 42, no. 10 (October 1, 2005): 1719–34. http://dx.doi.org/10.1139/e05-051.
Full textClark, T., A. Gobeil, and J. David. "Iron oxide - copper - gold-type and related deposits in the Manitou Lake area, eastern Grenville Province, Quebec: variations in setting, composition, and style." Canadian Journal of Earth Sciences 42, no. 10 (October 1, 2005): 1829–47. http://dx.doi.org/10.1139/e05-048.
Full textSchlegel, Tobias U., Thomas Wagner, Adrian Boyce, and Christoph A. Heinrich. "A magmatic source of hydrothermal sulfur for the Prominent Hill deposit and associated prospects in the Olympic iron oxide copper-gold (IOCG) province of South Australia." Ore Geology Reviews 89 (October 2017): 1058–90. http://dx.doi.org/10.1016/j.oregeorev.2016.09.002.
Full textCourtney-Davies, Ciobanu, Verdugo-Ihl, Slattery, Cook, Dmitrijeva, Keyser, et al. "Zircon at the Nanoscale Records Metasomatic Processes Leading to Large Magmatic–Hydrothermal Ore Systems." Minerals 9, no. 6 (June 16, 2019): 364. http://dx.doi.org/10.3390/min9060364.
Full textKeyser, William, Cristiana L. Ciobanu, Kathy Ehrig, Marija Dmitrijeva, Benjamin P. Wade, Liam Courtney-Davies, Max Verdugo-Ihl, and Nigel J. Cook. "Skarn-style alteration in Proterozoic metasedimentary protoliths hosting IOCG mineralization: the Island Dam Prospect, South Australia." Mineralium Deposita, February 27, 2022. http://dx.doi.org/10.1007/s00126-022-01096-1.
Full textDissertations / Theses on the topic "Olympic IOCG Province"
Chalk, H. C. "Mesoproterozoic bimodal magmatism of southern Australia: assessing relative mantle input and implications for IOCG mineralisation prospectivity." Thesis, 2014. http://hdl.handle.net/2440/109703.
Full textMesoproterozoic magmatism of the Gawler Craton and the Curnamona Province demonstrates regions of variable mantle input characteristics. Zircons from Hiltaba Suite granitoids and Gawler Range Volcanics, Gawler Craton, return εHf(T) values ranging from +7.1 to -0.4, +2.0 to -7.4, and +0.2 to -5.3 from the western, central, and eastern Gawler Craton respectively. Ninnerie Supersuite granitoids and Benagerie Volcanic Suite, Curnamona Province, return εHf(T) values ranging from +2.5 to -3.8. Mantle input modelling of the central/eastern Gawler Craton and the Curnamona Province returns similar mantle input fraction values ranging from 0.1 to 0.6, averaging 0.3, and 0.1 to 0.6, averaging 0.3, respectively. Hiltaba Suite magmatism of the western Gawler Craton is compositionally more juvenile than the central and eastern regions. The western Gawler Craton mantle input fractions range from 0.2 to 0.9 averaging 0.5, more elevated than the central/eastern regions of the Gawler Craton and the Curnamona province. The Benagerie Ridge region of the Curnamona Province displays similar bimodal ca. 1590 Ma magmatism, εHf(T) values, mantle input characteristics, crustal preservation (exhumation) and regional iron oxide copper-gold alteration as the highly prospective Olympic IOCG Province, Gawler Craton.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2014
Clark, J. M. "Defining the style of mineralisation at the Cairn Hill magnetite-sulphide deposit; Mount Woods Inlier, Gawler Craton, South Australia." Thesis, 2014. http://hdl.handle.net/2440/109968.
Full textThe Cairn Hill Fe-(Cu-Au) deposit is located within the World-class 1.6 Ga Olympic iron oxide-copper-gold (IOCG) Province of the Gawler Craton, South Australia. Cairn Hill deposit formation was penecontemperaneous with regional orogenesis, and is interpreted as a deep-level, ‘magnetite-rich’ end-member IOCG system hosted by an upper-amphibolite quartzofeldspathic ortho-gneiss and Mesoproterozoic (1600 – 1575 Ma) Hiltaba-equivalent Balta-suite granites and granodiorites. U-Pb zircon SHRIMP dating of a representative host rock and cross-cutting foliated granitic dyke, constrains the timing of mineralisation between ~1587 Ma and ~1525 Ma, respectively; suggesting an affinity to Hiltaba-age granitoids. The deposit strikes E-W over a distance of 1.3 km and is up to 40 m wide. It is characterized by two mineralised zones: the North- and South- Lodes, coincident with subsidiary structures within the transpressional Cairn Hill Shear Zone (CHSZ), and concordant with the strike of the encompassing magnetic anomaly. Progressive exhumation resulted in temperature and pressure decreases under high-fluid pressure causing the CHSZ to cross the brittle-ductile transition. This occurred relatively late in the hydrothermal-metamorphic evolution, resulting in a contractional duplex in a restraining bend suggestive of a positive flower structure providing an optimal conduit for hydrothermal fluid-flow. Early Na-Ca alteration has affected the host rocks predominantly characterised by albite + scapolite + diopside ± actinolite/titanite. Extensive K-Fe metasomatism has affected the host rocks overprinted by localised zones of intense, texturally-destructive high-temperature magnetite-biotite alteration that is typical of a transitional-style IOCG system. Associated hypogene iron mineralisation predominantly consists of magnetite, with extensive zones of a superimposed texturally-complex sulphide assemblage (pyrite-pyrrhotite-chalcopyrite). Definition of the IOCG deposit clan remains a contentious issue, primarily due to mis-classification and poor understanding of some individual deposits. Nevertheless, the general consensus is that IOCG deposits sensu-stricto represent a spectrum between high-temperature, deeper magnetite-rich end-member systems, such as Cairn Hill, and lower-temperature, shallower hematite-rich end-members.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2014
Book chapters on the topic "Olympic IOCG Province"
Spalding, Andrew. "A Latent Legacy: France." In A New Megasport Legacy, 229–48. Oxford University Press, 2022. http://dx.doi.org/10.1093/oso/9780197503614.003.0006.
Full textSpalding, Andrew. "Globalized Standards." In A New Megasport Legacy, 43–82. Oxford University Press, 2022. http://dx.doi.org/10.1093/oso/9780197503614.003.0002.
Full textReports on the topic "Olympic IOCG Province"
Wade, C., A. Reid, A. Fabris, S. Hore, and K. Robertson. Curnamona Province: IOCG frontier between Olympic Cu-Au Province-Mt Isa. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/329164.
Full textCorriveau, L., J. F. Montreuil, O. Blein, E. Potter, M. Ansari, J. Craven, R. Enkin, et al. Metasomatic iron and alkali calcic (MIAC) system frameworks: a TGI-6 task force to help de-risk exploration for IOCG, IOA and affiliated primary critical metal deposits. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/329093.
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