Relevant bibliographies by topics / Nebo-Babel

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  1. Journal articles
  2. Dissertations / Theses

Academic literature on the topic 'Nebo-Babel'

Author: Grafiati
Published: 4 June 2021
Last updated: 12 February 2022

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Journal articles on the topic "Nebo-Babel"

1

Witherly, Ken, and Daniel Sattel. "An assessment of Geotem, Falcon® and ZTEM surveys over the Nebo Babel deposit, Western Australia." ASEG Extended Abstracts 2018, no. 1 (December 2018): 1–7. http://dx.doi.org/10.1071/aseg2018abw10_1e.

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2

Baker, P. M., and R. S. Waugh. "The role of surface geochemistry in the discovery of the Babel and Nebo magmatic nickel–copper–PGE deposits." Geochemistry: Exploration, Environment, Analysis 5, no. 3 (July 19, 2005): 195–200. http://dx.doi.org/10.1144/1467-7873/03-032.

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3

Seat, Zoran, Stephen W. Beresford, Benjamin A. Grguric, Rob S. Waugh, Jon M. A. Hronsky, M. A. Mary Gee, David I. Groves, and Charter I. Mathison. "Architecture and emplacement of the Nebo–Babel gabbronorite-hosted magmatic Ni–Cu–PGE sulphide deposit, West Musgrave, Western Australia." Mineralium Deposita 42, no. 6 (February 27, 2007): 551–81. http://dx.doi.org/10.1007/s00126-007-0123-9.

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4

Godel, B., Z. Seat, W. D. Maier, and S. J. Barnes. "The Nebo-Babel Ni-Cu-PGE Sulfide Deposit (West Musgrave Block, Australia): Pt. 2. Constraints on Parental Magma and Processes, with Implications for Mineral Exploration." Economic Geology 106, no. 4 (June 1, 2011): 557–84. http://dx.doi.org/10.2113/econgeo.106.4.557.

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5

Legault, Jean, Glenn A. Wilson, Alexander V. Gribenko, Michael S. Zhdanov, Shengkai Zhao, and Keith Fisk. "An Overview of the ZTEM and AirMt Airborne Electromagnetic Systems: A Case Study from the Nebo-Babel Ni-Cu-PGE Deposit, West Musgrave, Western Australia." Preview 2012, no. 158 (June 2012): 26–32. http://dx.doi.org/10.1071/pvv2012n158p26.

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6

Seat, Z., S. W. Beresford, B. A. Grguric, M. A. M. Gee, and N. V. Grassineau. "Reevaluation of the Role of External Sulfur Addition in the Genesis of Ni-Cu-PGE Deposits: Evidence from the Nebo-Babel Ni-Cu-PGE Deposit, West Musgrave, Western Australia." Economic Geology 104, no. 4 (July 1, 2009): 521–38. http://dx.doi.org/10.2113/gsecongeo.104.4.521.

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7

Seat, Z., M. A. Mary Gee, B. A. Grguric, S. W. Beresford, and N. V. Grassineau. "The Nebo-Babel Ni-Cu-PGE Sulfide Deposit (West Musgrave, Australia): Pt. 1. U/Pb Zircon Ages, Whole-Rock and Mineral Chemistry, and O-Sr-Nd Isotope Compositions of the Intrusion, with Constraints on Petrogenesis." Economic Geology 106, no. 4 (June 1, 2011): 527–56. http://dx.doi.org/10.2113/econgeo.106.4.527.

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Dissertations / Theses on the topic "Nebo-Babel"

1

Seat, Zoran. "Geology, petrology, mineral and whole-rock chemistry, stable and radiogenic isotope systematics and Ni-Cu-PGE mineralisation of the Nebo-Babel intrusion, West Musgrave, Western Australia." University of Western Australia. School of Earth and Geographical Sciences, 2008. http://theses.library.uwa.edu.au/adt-WU2008.0202.

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Abstract:
The Nebo-Babel Ni-Cu-platinum-group element (PGE) magmatic sulphide deposit, a world-class ore body, is hosted in low-MgO, tube-like (chonolithic) gabbronorite intrusion in the West Musgrave Block, Western Australia. The Nebo-Babel deposit is the first significant discovery of a nickel sulphide deposit associated with the ca. 1078 Ma Giles Complex, which is part of the Warakurna large igneous province (LIP), now making the Musgrave Block a prime target for nickel sulphide exploration. The Musgrave Block is a Mesoproterozoic, east-west trending, orogenic belt in central Australia consisting of amphibolite and granulite facies basement gneisses with predominantly igneous protoliths. The basement lithologies have been intruded by mafic-ultramafic and felsic rocks; multiply deformed and metamorphosed between 1600 Ma and 500 Ma. The Giles Complex, which is part of the Warakurna LIP, was emplaced at ca. 1078 Ma and consists of a suite of layered mafic-ultramafic intrusions, mafic and felsic dykes and temporally associated volcanic rocks and granites. The Giles Complex intrusions are interpreted to have crystallised at crustal depths between 15km and 30km and are generally undeformed and unmetamorphosed.
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