ORCID Profile
0000-0003-2741-6076
Current Organisation
University of Tasmania
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Research Topics
In Research Link Australia (RLA), "Research Topics" refer to ANZSRC FOR and SEO codes. These topics are either sourced from ANZSRC FOR and SEO codes listed in researchers' related grants or generated by a large language model (LLM) based on their publications.
Top 5 Research Topics
ANZSRC Field of Research (FoR)
Geology | Ore Deposit Petrology | Exploration Geochemistry | Ore Deposit Petrology | Sedimentology | Geochronology | Geochemistry | Geochronology And Isotope Geochemistry | Electromagnetism | Chemical Oceanography | Igneous And Metamorphic Petrology | Marine Geoscience | Igneous and Metamorphic Petrology | Geochronology | Geodynamics | Mineral Processing/Beneficiation | Volcanology | Tectonics
ANZSRC Socio-Economic Objective (SEO)
Copper Ore Exploration | Precious (Noble) Metal Ore Exploration | Mineral Exploration not elsewhere classified | Expanding Knowledge in the Earth Sciences | Concentrating processes of other base metal ores | Environmentally Sustainable Mineral Resource Activities not elsewhere classified | Exploration | Iron Ore Exploration | Other |
Related Links
Publications
Pb-isotopic constraints on the source of A-type Suites: Insights from the Hiltaba Suite - Gawler Range Volcanics Magmatic Event, Gawler Craton, South Australia
Publisher: Elsevier BV
Date: 11-2019
The metamorphic sole of the western Tasmanian ophiolite: New insights into the Cambrian tectonic setting of the Gondwana Pacific margin
Publisher: Elsevier BV
Date: 10-2016
Cambrian metamorphic complexes in Tasmania: tectonic implications
Publisher: Informa UK Limited
Date: 12-2000
Revealing the continental margin of Gondwana: The Ordovician arc of the Cordón de Lila (northern Chile)
Publisher: Springer Science and Business Media LLC
Date: 22-09-2010
Insights into magma histories through silicate-oxide crystal clusters: Linking the Hiltaba Suite intrusive rocks to the Gawler Range Volcanics, Gawler Craton, South Australia
Publisher: Elsevier BV
Date: 02-2019
Pyrite Textures, Trace Elements and Sulfur Isotope Chemistry of Bijaigarh Shales, Vindhyan Basin, India and Their Implications
Publisher: MDPI AG
Date: 29-06-2020
DOI: 10.3390/MIN10070588
Abstract: The Vindhyan Basin in central India preserves a thick (~5 km) sequence of sedimentary and lesser volcanic rocks that provide a valuable archive of a part of the Proterozoic (~1800–900 Ma) in India. Here, we present an analysis of key sedimentary pyrite textures and their trace element and sulfur isotope compositions in the Bijaigarh Shale (1210 ± 52 Ma) in the Vindhyan Supergroup, using reflected light microscopy, LA-ICP-MS and SHRIMP-SI, respectively. A variety of sedimentary pyrite textures (fine-grained disseminated to aggregates, framboids, lags, and possibly microbial pyrite textures) are observed reflecting quiet and strongly anoxic water column conditions punctuated by occasional high-energy events (storm incursions). Key redox sensitive or sensitive to oxidative weathering trace elements (Co, Ni, Zn, Mo, Se) and ratios of (Se/Co, Mo/Co, Zn/Co) measured in sedimentary pyrites from the Bijaigarh Shale are used to infer atmospheric redox conditions during its deposition. Most trace elements are depleted relative to Proterozoic mean values. Sulfur isotope compositions of pyrite, measured using SHRIMP-SI, show an increase in δ34S as we move up stratigraphy with positive δ34S values ranging from 5.9‰ (lower) to 26.08‰ (upper). We propose limited sulphate supply caused the pyrites to incorporate the heavier isotope. Overall, we interpret these low trace element signatures and heavy sulfur isotope compositions to indicate relatively suppressed oxidative weathering on land during the deposition of the Bijaigarh Shale.
An advanced stepwise leaching technique for derivation of initial lead isotope ratios in ancient mafic rocks: A case study of Mesoproterozoic intrusions from the Udzha paleo-rift, Siberian Craton
Publisher: Elsevier BV
Date: 12-2019
Proterozoic metamorphism in Tasmania: Implications for tectonic reconstructions
Publisher: Elsevier BV
Date: 10-2008
Ocean and Atmosphere Geochemical Proxies Derived from Trace Elements in Marine Pyrite: Implications for Ore Genesis in Sedimentary Basins
Publisher: Society of Economic Geologists
Date: 07-02-2017
The key role of mica during igneous concentration of tantalum
Publisher: Springer Science and Business Media LLC
Date: 27-05-2014
Multiple felsic events within post-10 Ma volcanism, Southeast Australia: inputs in appraising proposed magmatic models
Publisher: Informa UK Limited
Date: 17-02-2014
Geological setting and timing of the Chah Zard breccia-hosted epithermal gold–silver deposit in the Tethyan belt of Iran
Publisher: Springer Science and Business Media LLC
Date: 26-08-2011
Authigenic monazite and detrital zircon dating from the Proterozoic Rocky Cape Group, Tasmania: Links to the Belt-Purcell Supergroup, North America
Publisher: Elsevier BV
Date: 09-2014
U–Pb geochronology and Pb isotope characteristics of the Chahgaz volcanogenic massive sulphide deposit, southern Iran
Publisher: Informa UK Limited
Date: 16-06-2010
Styles of Cenozoic collisions in the western and southwestern Pacific and their applications to Palaeozoic collisions in the Tasmanides of eastern Australia
Publisher: Elsevier BV
Date: 12-2009
Regional volcanism of northern Zealandia: Post-Gondwana break-up magmatism on an extended, submerged continent
Publisher: Geological Society of London
Date: 16-08-2018
DOI: 10.1144/SP463.9
The Jebel Ohier deposit—a newly discovered porphyry copper–gold system in the Neoproterozoic Arabian–Nubian Shield, Red Sea Hills, NE Sudan
Publisher: Springer Science and Business Media LLC
Date: 30-12-2016
Generation of Silicic Melts in the Early Izu‐Bonin Arc Recorded by Detrital Zircons in Proximal Arc Volcaniclastic Rocks From the Philippine Sea
Publisher: American Geophysical Union (AGU)
Date: 10-2017
DOI: 10.1002/2017GC006948
Diversity in Ruby Geochemistry and Its Inclusions: Intra- and Inter- Continental Comparisons from Myanmar and Eastern Australia
Publisher: MDPI AG
Date: 05-01-2019
DOI: 10.3390/MIN9010028
Abstract: Ruby in erse geological settings leaves petrogenetic clues, in its zoning, inclusions, trace elements and oxygen isotope values. Rock-hosted and isolated crystals are compared from Myanmar, SE Asia, and New South Wales, East Australia. Myanmar ruby typifies metasomatized and metamorphic settings, while East Australian ruby xenocrysts are derived from basalts that tapped underlying fold belts. The respective suites include homogeneous ruby bi-colored inner (violet blue) and outer (red) zoned ruby ruby-sapphirine-spinel composites pink to red grains and multi-zoned crystals of red-pink-white-violet (core to rim). Ruby ages were determined by using U-Pb isotopes in titanite inclusions (Thurein Taung 32.4 Ma) and zircon inclusions (Mong Hsu 23.9 Ma) and basalt dating in NSW, –40 Ma. Trace element oxide plots suggest marble sources for Thurein Taung and Mong Hsu ruby and ultramafic-mafic sources for Mong Hsu (dark cores). NSW rubies suggest metasomatic (Barrington Tops), ultramafic to mafic (Macquarie River) and metasomatic-magmatic (New England) sources. A previous study showed that Cr/Ga vs. Fe/(V + Ti) plots separate Mong Hsu ruby from other ruby fields, but did not test Mogok ruby. Thurein Taung ruby, tested here, plotted separately to Mong Hsu ruby. A Fe-Ga/Mg diagram splits ruby suites into various fields (Ga/Mg 3), except for magmatic input into rare Mogok and Australian ruby (Ga/Mg 6). The erse results emphasize ruby’s potential for geographic typing.
Implications of U–Pb detrital zircon geochronology analysis for the depositional age, provenance, and tectonic setting of continental Mesozoic formations in the East Malaya Terrane, Peninsular Malaysi
Publisher: Wiley
Date: 16-01-2018
DOI: 10.1002/GJ.3131
Matrix effects in Pb/U measurements during LA-ICP-MS analysis of the mineral apatite
Publisher: Royal Society of Chemistry (RSC)
Date: 2016
DOI: 10.1039/C6JA00048G
Abstract: U–Pb ages of several apatite reference materials, acquired by LA-ICP-MS over a 3.5 year period using the Otter Lake apatite as a primary standard, show systematic offsets (up to 3%) from reference ages obtained by isotope dilution mass spectrometry.
Olivine-phyric basalt in the Mesoproterozoic Gawler silicic large igneous province, South Australia: Examples at the Olympic Dam Iron Oxide Cu–U–Au–Ag deposit and other localities
Publisher: Elsevier BV
Date: 08-2016
Pb-isotope ratios and the petrogenesis of the Tunkillia Suite, Gawler Craton
Publisher: Informa UK Limited
Date: 17-05-2021
Provenance of lower Paleozoic sedimentary rocks in Tasmania and Waratah Bay, southern Victoria: constraints from detrital zircon hafnium isotopes and trace-element geochemistry
Publisher: Informa UK Limited
Date: 09-11-2022
The tongon au deposit, northern côte d'ivoire: An example of paleoproterozoic au skarn mineralization
Publisher: Society of Economic Geologists
Date: 11-2017
The ~1.85 Ga carbonatite in north China and its implications on the evolution of the Columbia supercontinent
Publisher: Elsevier BV
Date: 2019
Linking Olympic Dam and the Cariewerloo Basin: Was a sedimentary basin involved in formation of the world’s largest uranium deposit?
Publisher: Elsevier BV
Date: 10-2017
Geochronological constraints on the Tropicana gold deposit and Albany-Fraser orogen, Western Australia
Publisher: Society of Economic Geologists
Date: 23-01-2015
Geochemistry and geochronology of the Chatree epithermal gold-silver deposit: Implications for the tectonic setting of the Loei Fold Belt, central Thailand
Publisher: Elsevier BV
Date: 07-2014
Holocene eruptions of Mt. Popa, Myanmar: Volcanological evidence of the ongoing subduction of Indian Plate along Arakan Trench
Publisher: Elsevier BV
Date: 07-2018
In search of Gondwana heritage in the Outer Melanesian Arc: no pre-upper Eocene detrital zircons in Viti Levu river sands (Fiji Islands)
Publisher: Informa UK Limited
Date: 02-12-2018
Tectonothermal events in the Olympic IOCG Province constrained by apatite and REE-phosphate geochronology
Publisher: Informa UK Limited
Date: 20-05-2018
Chapter 3 Pre-Late Cretaceous basement terranes of the Gondwana active margin of New Caledonia
Publisher: Geological Society of London
Date: 2020
DOI: 10.1144/M51-2016-11
The Lüliang Massif: a key area for the understanding of the Palaeoproterozoic Trans-North China Belt, North China Craton
Publisher: Geological Society of London
Date: 2009
DOI: 10.1144/SP323.5
Age, igneous petrogenesis, and tectonic setting of the Bilihe gold deposit, China, and implications for regional metallogeny
Publisher: Elsevier BV
Date: 06-2016
Alkaline industrial wastes – Characteristics, environmental risks, and potential for mine waste management
Publisher: Elsevier BV
Date: 04-2023
U–Pb zircon geochronology and geochemistry from NE Vietnam: A ‘tectonically disputed’ territory between the Indochina and South China blocks
Publisher: Elsevier BV
Date: 06-2016
Chemistry and origin of the Mayo Kila sapphires, NW region Cameroon (Central Africa): Their possible relationship with the Cameroon volcanic line
Publisher: Elsevier BV
Date: 06-2016
Reply to 'Unclear causes for subduction'
Publisher: Springer Science and Business Media LLC
Date: 29-04-2016
DOI: 10.1038/NGEO2704
Age and pyrite Pb-isotopic composition of the giant Sukhoi Log sediment-hosted gold deposit, Russia
Publisher: Elsevier BV
Date: 05-2008
Detrital mineral morphology and geochemistry: Methods to characterize and constrain the origin of the Nsanaragati blue sapphires, south-western region of Cameroon
Publisher: Elsevier BV
Date: 07-2012
The metamorphic sole of New Caledonia ophiolite: 40Ar/39Ar, U‐Pb, and geochemical evidence for subduction inception at a spreading ridge
Publisher: American Geophysical Union (AGU)
Date: 06-2012
DOI: 10.1029/2011TC003085
Pb‐isotope compositions of the Tasik Chini volcanic‐hosted massive sulfide deposit, Central Belt of Peninsular Malaysia: Implication for source region and tectonic setting
Publisher: Wiley
Date: 19-02-2017
DOI: 10.1111/IAR.12177
The Ban Houayxai epithermal Au–Ag deposit in the Northern Lao PDR: Mineralization related to the Early Permian arc magmatism of the Truong Son Fold Belt
Publisher: Elsevier BV
Date: 07-2014
Lead and Nd isotopic evidence for a crustal Pb source of the giant Broken Hill Pb-Zn-Ag deposit, New South Wales, Australia
Publisher: Elsevier BV
Date: 03-2015
Geology, geochemistry and metallogenesis of the Selinsing gold deposit, central Malaysia
Publisher: Elsevier BV
Date: 07-2014
Basalts erupted along the Tongan fore arc during subduction initiation: Evidence from geochronology of dredged rocks from the Tonga fore arc and trench
Publisher: American Geophysical Union (AGU)
Date: 12-2012
DOI: 10.1029/2012GC004335
Comparison of metal enrichment in pyrite framboids from a metal-enriched and metal-poor estuary
Publisher: Mineralogical Society of America
Date: 04-2014
DOI: 10.2138/AM.2014.4545
The oldest anthropoid primates in SE Asia: Evidence from LA-ICP-MS U-Pb zircon age in the Late Middle Eocene Pondaung Formation, Myanmar
Publisher: Elsevier BV
Date: 07-2014
The Tam Ky-Phuoc Son Shear Zone in central Vietnam: Tectonic and metallogenic implications
Publisher: Elsevier BV
Date: 07-2014
Detrital zircon ages, provenance and tectonic evolution in the early Paleozoic of Tasmania and Waratah Bay, Victoria
Publisher: Informa UK Limited
Date: 12-2021
Volcanology, geochemistry and structure of the Ordovician Cargo Volcanics in the Cargo - Walli region, central New South Wales
Publisher: Informa UK Limited
Date: 03-2007
U-Pb Zircon Age Constraining the Source and Provenance of Gem-Bearing Late Cenozoic Detrital Deposits, Mamfe Basin, SW Cameroon
Publisher: Wiley
Date: 27-06-2012
Melanesian back-arc basin and arc development: Constraints from the eastern Coral Sea
Publisher: Elsevier BV
Date: 11-2016
Nb-Ta fractionation in peraluminous granites: A marker of the magmatichydrothermal transition
Publisher: Geological Society of America
Date: 28-06-2016
DOI: 10.1130/G38086C.1
Quantifying and characterising metal concentrations in Derwent Estuary sediments using portable X-ray fluorescence spectrometry
Publisher: Informa UK Limited
Date: 20-02-2022
Postmagmatic magnetite–apatite assemblage in mafic intrusions: a case study of dolerite at Olympic Dam, South Australia
Publisher: Springer Science and Business Media LLC
Date: 11-12-2015
Geology and geochronology of the Two-Thirty prospect, Northparkes district, NSW
Publisher: Informa UK Limited
Date: 17-01-2021
The Zanhuang Massif, the second and eastern suture zone of the Paleoproterozoic Trans-North China Orogen
Publisher: Elsevier BV
Date: 07-2009
Characterization of Galena and Vein Paragenesis in the Penjom Gold Mine, Malaysia: Trace Elements, Lead Isotope Study and Relationship to Gold Mineralization Episodes
Publisher: Wiley
Date: 12-2015
Propagation of back‐arc extension into the arc lithosphere in the southern N ew H ebrides volcanic arc
Publisher: American Geophysical Union (AGU)
Date: 09-2015
DOI: 10.1002/2015GC005717
Multi-stage enrichment processes for large gold-bearing ore deposits
Publisher: Elsevier BV
Date: 07-2016
Gem Corundum Deposits of Greece: Geology, Mineralogy and Genesis
Publisher: MDPI AG
Date: 15-01-2019
DOI: 10.3390/MIN9010049
Abstract: Greece contains several gem corundum deposits set within erse geological settings, mostly within the Rhodope (Xanthi and Drama areas) and Attico-Cycladic (Naxos and Ikaria islands) tectono-metamorphic units. In the Xanthi area, the sapphire (pink, blue to purple) deposits are stratiform, occurring within marble layers alternating with hibolites. Deep red rubies in the Paranesti-Drama area are restricted to boudinaged lenses of Al-rich metapyroxenites alternating with hibolites and gneisses. Both occurrences are oriented parallel to the ultra-high pressure/high pressure (UHP/HP) Nestos suture zone. On central Naxos Island, colored sapphires are associated with desilicated granite pegmatites intruding ultramafic lithologies (plumasites), occurring either within the pegmatites themselves or associated metasomatic reaction zones. In contrast, on southern Naxos and Ikaria Islands, blue sapphires occur in extensional fissures within Mesozoic metabauxites hosted in marbles. Mineral inclusions in corundums are in equilibrium and/or postdate corundum crystallization and comprise: spinel and pargasite (Paranesti), spinel, zircon (Xanthi), margarite, zircon, apatite, diaspore, phlogopite and chlorite (Naxos) and chloritoid, ilmenite, hematite, ulvospinel, rutile and zircon (Ikaria). The main chromophore elements within the Greek corundums show a wide range in concentration: the Fe contents vary from (average values) 1099 ppm in the blue sapphires of Xanthi, 424 ppm in the pink sapphires of Xanthi, 2654 ppm for Paranesti rubies, 4326 ppm for the Ikaria sapphires, 3706 for southern Naxos blue sapphires, 4777 for purple and 3301 for pink sapphire from Naxos plumasite, and finally 4677 to 1532 for blue to colorless sapphires from Naxos plumasites, respectively. The Ti concentrations (average values) are very low in rubies from Paranesti (41 ppm), with values of 2871 ppm and 509 in the blue and pink sapphires of Xanthi, respectively, of 1263 ppm for the Ikaria blue sapphires, and 520 ppm, 181 ppm in Naxos purple, pink sapphires, respectively. The blue to colorless sapphires from Naxos plumasites contain 1944 to 264 ppm Ti, respectively. The very high Ti contents of the Xanthi blue sapphires may reflect submicroscopic rutile inclusions. The Cr (average values) ranges from 4 to 691 ppm in the blue, purple and pink colored corundums from Naxos plumasite, is quite fixed (222 ppm) for Ikaria sapphires, ranges from 90 to 297 ppm in the blue and pink sapphires from Xanthi, reaches 9142 ppm in the corundums of Paranesti, with highest values of 15,347 ppm in deep red colored varieties. Each occurrence has both unique mineral assemblage and trace element chemistry (with variable Fe/Mg, Ga/Mg, Ga/Cr and Fe/Ti ratios). Additionally, oxygen isotope compositions confirm their geological typology, i.e., with, respectively δ18O of 4.9 ± 0.2‰ for sapphire in plumasite, 20.5‰ for sapphire in marble and 1‰ for ruby in mafics. The fluid inclusions study evidenced water free CO2 dominant fluids with traces of CH4 or N2, and low CO2 densities (0.46 and 0.67 g/cm3), which were probably trapped after the metamorphic peak. The Paranesti, Xanthi and central Naxos corundum deposits can be classified as metamorphic sensu stricto (s.s.) and metasomatic, respectively, those from southern Naxos and Ikaria display atypical magmatic signature indicating a hydrothermal origin. Greek corundums are characterized by wide color variation, homogeneity of the color hues, and transparency, and can be considered as potential gemstones.
U–Pb zircon geochronology from the Alexander terrane, southeast Alaska: implications for the Greens Creek massive sulphide deposit
Publisher: Canadian Science Publishing
Date: 12-2016
Abstract: This paper presents results of a laser ablation – inductively coupled plasma – quadrapole mass spectrometer (LA–ICP–QMS) U–Pb dating study of small in situ zircon grains from s les collected in the vicinity of the Greens Creek massive sulphide deposit, on northern Admiralty Island, southeast Alaska. The Greens Creek mine is a volcanogenic massive sulphide deposit in the central portion of the Alexander Triassic metallogenic belt (ATMB) and is one of the top global silver producers despite having a dominantly mafic metavolcanic stratigraphic footwall. The stratigraphic footwall is a Mississippian mafic metavolcanic sequence with a protolith age of approximately 340–330 Ma. The first U–Pb zircon constrained chronostratigraphy for the area places the deposit near, or at, the base of the host Late Triassic stratigraphy just above an approximately 100 million year old unconformity and probably 10–15 million years older than mineralization at the Palmer and Windy Craggy deposits in the northern portion of the ATMB. The stratigraphic location of the Greens Creek deposit is atypical for a syngenetic massive sulphide deposit, and this may, at least partly, explain its unusual metal endowment. Pre-mineralization Permian U–Pb zircon metamorphic ages are consistent with published 273–260 Ma white mica ages related to the collision of the Admiralty and Craig subterranes, the basement to the ATMB. The much older age of the footwall rocks and their Permian pre-mineralization metamorphism demonstrates that though the mafic volcanic rocks are not genetically linked to the deposit, they likely influenced the style of alteration and mineralization.
Arc and mantle detritus in the post-collisional, Lower Silurian Kabaddah Formation, Lachlan Orogen, New South Wales
Publisher: Informa UK Limited
Date: 03-2007
Understanding the microscale spatial distribution and mineralogical residency of Re in pyrite: Examples from carbonate-hosted Zn-Pb ores and implications for pyrite Re-Os geochronology
Publisher: Elsevier BV
Date: 02-2020
Geochemistry and provenance of the Turquoise Bluff Slate, northeastern Tasmania: tectonic significance
Publisher: Informa UK Limited
Date: 11-12-2018
Geochronology of the DeGrussa volcanic-hosted massive sulphide deposit and associated mineralisation of the Yerrida, Bryah and Padbury Basins, Western Australia
Publisher: Elsevier BV
Date: 09-2015
A Multiproxy provenance approach to uncovering the assembly of East Gondwana in Antarctica
Publisher: Geological Society of America
Date: 13-05-2019
DOI: 10.1130/G45952.1
Magma production along the Lord Howe Seamount Chain, northern Zealandia
Publisher: Cambridge University Press (CUP)
Date: 18-01-2019
DOI: 10.1017/S0016756818000912
Abstract: One of the world’s most notable intraplate volcanic regions lies on the eastern Australian plate and includes two age-progressive trails offshore (Tasmantid and Lord Howe seamount chains) and the world’s longest continental hotspot trail (Cosgrove Track). While most studies agree that these chains formed by the rapid northward motion of the Australian plate over a slowly moving mantle source, the volcanic output along these trails, their plate–mantle interactions and the source of the magmatism remain unconstrained. A geophysical mapping and dredging c aign on the RV Southern Surveyor (ss2012_v06) confirmed the prolongation of the Lord Howe Seamount Chain to the South Rennell Trough, ∼200 km further north than previously s led. Radiometric dating of these new s les at 27–28 Ma, together with previously published results from the southern part of the chain, indicate straightforward northward motion of the Australian plate over a quasi-stationary hotspot as predicted by Indo-Atlantic and Pacific hotspot models. A peak in Lord Howe Seamount Chain magmatism in late Oligocene time, also seen in the Tasmantid and Cosgrove trails, matches a 27–23 Ma slowdown of Australian plate motion. The average magma flux of the Lord Howe hotspot is estimated at 0.4 m 3 s −1 , similar to rates of crustal production at the South Rennell Trough prior to cessation of spreading in middle Oligocene time, supporting a potential genetic relationship to this spreading system. In addition, plate tectonic modelling suggests that the seamounts and plateaus in the Coral Sea may host the earliest evidence of plume activity in the area.
Pyrite compositions from VHMS and orogenic Au deposits in the Yilgarn Craton, Western Australia: Implications for gold and copper exploration
Publisher: Elsevier BV
Date: 12-2016
Evidence for an Intrabasinal Source and Multiple Concentration Processes in the Formation of the Carbon Leader Reef, Witwatersrand Supergroup, South Africa
Publisher: Society of Economic Geologists
Date: 13-08-2013
The Boghen terrane (New Caledonia, SW Pacific): A Jurassic accretionary complex. Preliminary U-Pb radiochronological data on detrital zircon,L'unité de la Boghen (Nouvelle-Calédonie, Pacifique sud-ouest): Un complexe d'accrétion jurassique. Données radiochronologiques préliminaires U-Pb sur les zircons détritiques
Publisher: Cellule MathDoc/CEDRAM
Date: 2002
Evolution of pyrite trace element compositions from porphyry-style and epithermal conditions at the Lihir gold deposit: Implications for ore genesis and mineral processing
Publisher: Society of Economic Geologists, Inc.
Date: 2018
Porphyry fertility in the Northparkes district: indicators from whole-rock geochemistry
Publisher: Informa UK Limited
Date: 06-02-2020
Re-evaluation of contact relationships between Ordovician volcanic belts and the quartz-rich turbidites of the Lachlan Orogen
Publisher: Informa UK Limited
Date: 03-2007
The configuration of Greater Gondwana—Evidence from LA ICPMS, U–Pb geochronology of detrital zircons from the Palaeozoic and Mesozoic of Southeast Asia and China
Publisher: Elsevier BV
Date: 07-2014
Where was the Ailaoshan Ocean and when did it open: A perspective based on detrital zircon U–Pb age and Hf isotope evidence
Publisher: Elsevier BV
Date: 08-2016
Neoproterozoic (ca. 820–830 Ma) mafic dykes at Olympic Dam, South Australia: Links with the Gairdner Large Igneous Province
Publisher: Elsevier BV
Date: 12-2015
Optimisation of laser parameters for the analysis of sulphur isotopes in sulphide minerals by laser ablation ICP-MS
Publisher: Royal Society of Chemistry (RSC)
Date: 2014
DOI: 10.1039/C4JA00011K
Detrital zircon records of Late Cretaceous syn-rift sedimentary sequences of New Caledonia: An Australian provenance questioned
Publisher: Elsevier BV
Date: 03-2011
Earliest Eocene (53 Ma) convergence in the Southwest Pacific: evidence from pre‐obduction dikes in the ophiolite of New Caledonia
Publisher: Wiley
Date: 31-10-2006
Impact of air, laser pulse width and fluence on U–Pb dating of zircons by LA-ICPMS
Publisher: Royal Society of Chemistry (RSC)
Date: 2018
DOI: 10.1039/C7JA00357A
Abstract: The accuracy of zircon U–Pb dating by LA-ICPMS is limited by matrix effects related to differences in U–Pb fractionation between an unknown and the calibration standard.
Cretaceous fore-arc basalts from the Tonga arc: Geochemistry and implications for the tectonic history of the SW Pacific
Publisher: Elsevier BV
Date: 09-2014
A record of spontaneous subduction initiation in the Izu–Bonin–Mariana arc
Publisher: Springer Science and Business Media LLC
Date: 24-08-2015
DOI: 10.1038/NGEO2515
Gold and Trace Element Zonation in Pyrite Using a Laser Imaging Technique: Implications for the Timing of Gold in Orogenic and Carlin-Style Sediment-Hosted Deposits
Publisher: Society of Economic Geologists
Date: 08-2009
In situ location and U‐Pb dating of small zircon grains in igneous rocks using laser ablation–inductively coupled plasma–quadrupole mass spectrometry
Publisher: American Geophysical Union (AGU)
Date: 05-04-2011
DOI: 10.1029/2010GC003405
Zircon megacryst ages and chemistry, from a placer, dunedin Volcanic area, Eastern Otago, New Zealand
Publisher: Informa UK Limited
Date: 09-2009
Age and origin of gem corundum and zircon megacrysts from the Mercaderes-Rio Mayo area, South-west Colombia, South America
Publisher: Elsevier BV
Date: 09-2008
Ordovician cataclasite bands in the tambillo monzogranite: Expression of an early subphase of the ocloyic movements in the cordón Lila, northern Chile,Las bandas de cataclasitas ordovícicas del monzogranito tambillo: Manifestaciones de una subfase temprana de los movimientos oclóyicos en el cordón de Lila, norte de Chile
Publisher: Pontificia Universidad Catolica de Valparaiso
Date: 30-09-2013
Location and migration of Miocene–Quaternary volcanic arcs in the SW Pacific region
Publisher: Elsevier BV
Date: 02-2010
Palaeozoic collision between the North and South China blocks, Triassic intracontinental tectonics, and the problem of the ultrahigh-pressure metamorphism
Publisher: Elsevier BV
Date: 02-2008
U-Pb zircon geochronology of Early Permian to Late Triassic rocks from Singapore and Johor: A plate tectonic reinterpretation
Publisher: Elsevier BV
Date: 07-2014
Mafic volcanic rocks on King Island, Tasmania: evidence for 579Ma break-up in east Gondwana
Publisher: Elsevier BV
Date: 11-2004
Age constraints on the hydrothermal history of the Prominent Hill iron oxide copper-gold deposit, South Australia
Publisher: Springer Science and Business Media LLC
Date: 28-12-2017
A story of olivine from the McIvor Hill complex (Tasmania, Australia): Clues to the origin of the Avebury metasomatic Ni sulfide deposit
Publisher: Mineralogical Society of America
Date: 06-2016
DOI: 10.2138/AM-2016-5509
Age, origin and significance of nodular sulfides in 2680Ma carbonaceous black shale of the Eastern Goldfields Superterrane, Yilgarn Craton, Western Australia
Publisher: Elsevier BV
Date: 06-2013
Gold accumulation in the Archaean Witwatersrand Basin, South Africa — Evidence from concentrically laminated pyrite
Publisher: Elsevier BV
Date: 2015
Neoproterozoic opening of the Pacific Ocean recorded by multi-stage rifting in Tasmania, Australia
Publisher: Elsevier BV
Date: 02-2020
Depositional age and correlation of the Oonah Formation: refining the timing of Neoproterozoic basin formation in Tasmania
Publisher: Informa UK Limited
Date: 15-02-2018
Jurassic volcaniclastic-basaltic andesite-dolerite sequence in Tasmania: New age constraints for fossil plants from Lune River
Publisher: Informa UK Limited
Date: 10-2007
Chronology, petrochemistry of fine grained granite and their implication to Mo-Cu mineralization in Xichong Mo Deposit, Anhui Province, China
Publisher: Wiley
Date: 12-2014
Assessment of magmatic fertility using pXRF on altered rocks from the Ordovician Macquarie Arc, New South Wales
Publisher: Informa UK Limited
Date: 03-08-2021
U–Th–Pb monazite dating and the timing of arc–continent collision in East Timor
Publisher: Informa UK Limited
Date: 18-05-2016
Chapter 7 Post-obduction evolution of New Caledonia
Publisher: Geological Society of London
Date: 2020
DOI: 10.1144/M51-2018-74
Discovery of early cretaceous rocks in New Caledonia: New Geochemical and U-Pb zircon age constraints on the transition from subduction to marginal breakup in the Southwest Pacific
Publisher: University of Chicago Press
Date: 07-2010
DOI: 10.1086/652779
Regional implications of U/Pb SHRIMP age constraints on the tectonic evolution of New Caledonia
Publisher: Elsevier BV
Date: 12-1998
Geochronological, geochemical and Pb isotopic compositions of Tasmanian granites (southeast Australia): Controls on petrogenesis, geodynamic evolution and tin mineralisation
Publisher: Elsevier BV
Date: 06-2017
Provenance of the Eocene sandstones in the southern Chindwin Basin, Myanmar: Implications for the unroofing history of the Cretaceous–Eocene magmatic arc
Publisher: Elsevier BV
Date: 08-2015
Late Paleozoic tectonic evolution of the northern West Chinese Tianshan Belt
Publisher: Informa UK Limited
Date: 08-2006
The Western Ailaoshan Volcanic Belts and their SE Asia connection: A new tectonic model for the Eastern Indochina Block
Publisher: Elsevier BV
Date: 07-2014
The Central Ailaoshan ophiolite and modern analogs
Publisher: Elsevier BV
Date: 07-2014
Geochemistry, geochronology, and tectonic setting of early Permian (~290 Ma) volcanic-hosted massive sulphide deposits of the Tasik Chini district, Peninsular Malaysia
Publisher: Informa UK Limited
Date: 28-01-2016
Development of framboidal pyrite during diagenesis, low-grade regional metamorphism, and hydrothermal alteration
Publisher: Society of Economic Geologists
Date: 12-2009
A Reappraisal of the Poya Terrane (New Caledonia): Accreted Late Cretaceous‐Paleocene Marginal Basin Upper Crust, Passive Margin Sediments, and Early Eocene E‐MORB Sill Complex
Publisher: American Geophysical Union (AGU)
Date: 2018
DOI: 10.1002/2017TC004579
Zircon U-Pb geochronology of granitic rocks of the Cordón de Lila and Sierra de Almeida ranges, northern Chile: 30 m.y. of Ordovician plutonism on the western border of Gondwana
Publisher: Elsevier BV
Date: 12-2014
Timing and genesis of the Karoo-Ferrar large igneous province: New high precision U-Pb data for Tasmania confirm short duration of the major magmatic pulse
Publisher: Elsevier BV
Date: 04-2017
Corundum (sapphire) and zircon relationships, Lava Plains gem fields, NE Australia: Integrated mineralogy, geochemistry, age determination, genesis and geographical typing
Publisher: Mineralogical Society
Date: 06-2015
DOI: 10.1180/MINMAG.2015.079.3.04
Abstract: Gem minerals at Lava Plains, northeast Queensland, offer further insights into mantle-crustal gemformation under young basalt fields. Combined mineralogy, U-Pb age determination, oxygen isotope and petrological data on megacrysts and meta-aluminosilicate xenoliths establish a geochemical evolution in sapphire, zircon formation between 5 to 2 Ma. Sapphire megacrysts with magmatic signatures (Fe/Mg ∼100–1000, Ga/Mg 3–18) grew with ∼3 Ma micro-zircons of both mantle (δ 18 O 4.5–5.6%) and crustal (δ 18 O 9.5–10.1‰) affinities. Zircon megacrysts (3±1 Ma) show mantle and crustal characteristics, but most grew at crustal temperatures (600–800°C). Xenolith studies suggest hydrous silicate melts and fluids initiated from hibolized mantle infiltrated into kyanite+sapphire granulitic crust (800°C, 0.7 GPa). This metasomatized the sapphire (Fe/Mg ∼50–120, Ga/Mg ∼3–11), left relict metastable sillimanite-corundum-quartz and produced minerals enriched in high field strength, large ion lithophile and rare earth elements. The gem suite suggests a syenitic parentage before its basaltic transport. Geographical trace-element typing of the sapphire megacrysts against other eastern Australian sapphires suggests a phonolitic involvement.
Paleomagnetic testing of the Lachlan Orocline hypothesis: Overprinting of remanence in Paleozoic rocks of the Lachlan Orogen in southeast Australia
Publisher: Informa UK Limited
Date: 08-06-2021
Associations between zircon and Fe–Ti oxides in Hiltaba event magmatic rocks, South Australia: atomic- or pluton-scale processes?
Publisher: Informa UK Limited
Date: 15-09-2020
Gold and Arsenopyrite Exsolution and Limits of Arsenic Solubility in Pyrite Investigated by SEM, EPMA, and L-ICPMS
Publisher: Oxford University Press (OUP)
Date: 08-2015
A North American provenance for Neoproterozoic to Cambrian sandstones in Tasmania?
Publisher: Elsevier BV
Date: 10-2001
Origin of Fe-Mn ± Si layers associated with the Permian volcanic-hosted massive sulphide deposits in the Tasik Chini district, Peninsular Malaysia
Publisher: Elsevier BV
Date: 05-2020
Linking gold mineralization to regional-scale drivers of mineral systems using in situ U–Pb geochronology and pyrite LA-ICP-MS element mapping
Publisher: Elsevier BV
Date: 2019
Synsedimentary to early diagenetic gold in Black shale-hosted pyrite nodules at the Golden Mile deposit, Kalgoorlie, Western Australia
Publisher: Society of Economic Geologists
Date: 22-05-2015
Age and tectonic setting of the Bavanat Cu–Zn–Ag Besshi-type volcanogenic massive sulfide deposit, southern Iran
Publisher: Springer Science and Business Media LLC
Date: 08-03-2012
120 to 0 Ma tectonic evolution of the southwest Pacific and analogous geological evolution of the 600 to 220 Ma Tasman Fold Belt System
Publisher: Geological Society of America
Date: 2003
Middle and Late Ordovician magmatic evolution of the Macquarie Arc, Lachlan Orogen, New South Wales
Publisher: Informa UK Limited
Date: 03-2007
Early Eocene clinoenstatite boninite and boninite-series dikes of the ophiolite of New Caledonia; a witness of slab-derived enrichment of the mantle wedge in a nascent volcanic arc
Publisher: Elsevier BV
Date: 09-2016
Compositional characteristics and geodynamic significance of late M iocene volcanic rocks associated with the C hah Z ard epithermal gold–silver deposit, southwest Y
Publisher: Wiley
Date: 26-10-2017
DOI: 10.1111/IAR.12223
Cenozoic Evolution of the Sulu Sea Arc‐Basin System: An Overview
Publisher: American Geophysical Union (AGU)
Date: 02-2021
DOI: 10.1029/2020TC006630
Geochemistry, geochronology and tectonic implications of Late Silurian – Early Devonian volcanic successions, Central Lachlan Orogen, New South Wales
Publisher: Informa UK Limited
Date: 03-2008
Geochronology of the volcanic rocks in the Lu-Zong basin and its significance
Publisher: Springer Science and Business Media LLC
Date: 10-2008
The Dovyren intrusive complex (northern Baikal region, Russia): isotope–geochemical markers of contamination of parental magmas and extreme enrichment of the source
Publisher: GeoScienceWorld
Date: 03-2015
DOI: 10.1016/J.RGG.2015.02.004
Abstract: The Dovyren intrusive complex includes the ore-bearing (Cu–Ni–PGE) Yoko–Dovyren layered pluton (728 Ma, up to 3.4 km in thickness), underlying ultramafic sills, and comagmatic leuconorite and gabbro-diabase dikes. Studies of Sr–Nd–Pb isotope systems were carried out for 24 intrusive rocks and five associated low- and high-Ti basalts. The high-Ti basalts show 0.7028 ≤ (87Sr/86Sr)T ≤ 0.7048 and 4.6 ≤ εNd(T) ≤ 5.8, similar to the values in MORB. The intrusive basic and ultrabasic rocks are geochemically similar to the low-Ti formation, making a compact cluster of compositions with extremely high ratios of radiogenic Sr and Pb isotopes and low εNd values. The maximum enrichment in radiogenic Sr is shown by the rocks near the pluton bottom ((87Sr/86Sr)T = 0.71387 ± 0.00010 (2σ) εNd(T) = –16.09 ± 0.06), which are the products of crystallization of the most primitive high-Mg magmas. The above-located dunites, troctolites, and gabbro show lower enrichment, probably because of the contamination of the host rocks during the filling of the magma chamber and/or because of the slight heterogeneity of the source. Calculations of the proportions of mixing of the parental melt with carbonate terrigenous material have shown that the variations in the Sr and Nd isotope ratios are due to the incredibly high contamination of the sediments, up to 40–50%. This contradicts the succession of the main rock types in the Yoko–Dovyren pluton in accordance with the crystallization of picrite-basaltic magma. The contribution of 5–10% high-Ti component seems more likely and suggests interaction between two isotopically contrasting magmas in this province in the Late Riphean. In general, the minor variations in εNd(T) of the intrusive rocks and metavolcanics (–14.3 ± 1.1) testify to the isotopically anomalous source of the low-Ti magmas. The time variation trend of εNd and geochemical features of the Dovyren rocks indicate that the products of melting of 2.7–2.8 Ga suprasubduction mantle might have been the massif protolith. Thus, the Dovyren parental magmas formed from a much older (sub)lithospheric source in the Late Riphean. The source was initially enriched in a mafic component with a low Sm/Nd ratio and was isolated from the convecting mantle and mantle melting processes for ~2 Gyr. The existence of such a long-living and at least twice reactivated lithospheric substratum is confirmed by the fact that the Nd isotope evolution trend of the initially nonanomalous mantle protolith includes not only the Dovyren rocks but also the Paleoproterozoic gabbro of the Chinei pluton and the Archean enderbites of the Baikal region. © 2015, V.S. Sobolev IGM, Siberian Branch of the RAS. Published by Elsevier B.V. All rights reserved.
Boninites and Adakites from the Northern Termination of the Tonga Trench: Implications for Adakite Petrogenesis
Publisher: Oxford University Press (OUP)
Date: 11-10-2007
Collision tectonics in the New Hebrides arc (Vanuatu)
Publisher: Wiley
Date: 03-2001
Geochronology and geochemistry of late Jurassic adakitic intrusions and associated porphyry Mo–Cu deposit in the Tongcun area, east China: Implications for metallogenesis and tectonic setting
Publisher: Elsevier BV
Date: 2017
Benambran Orogeny in the Eastern Lachlan Orogen, Australia
Publisher: Informa UK Limited
Date: 03-2007
Tectonics and metallogeny of mainland Southeast Asia — A review and contribution
Publisher: Elsevier BV
Date: 07-2014
Gem-corundum megacrysts from east Australian basalt fields: trace elements, oxygen isotopes and origins∗
Publisher: Informa UK Limited
Date: 10-2009
Advances in trace element “fingerprinting” of gem corundum, ruby and sapphire, Mogok area, Myanmar
Publisher: MDPI AG
Date: 30-12-2014
DOI: 10.3390/MIN5010061
From magma to mush to lava: Crystal history of voluminous felsic lavas in the Gawler Range Volcanics, South Australia
Publisher: Elsevier BV
Date: 11-2019
Geochronology of the Dovyren intrusive complex, northwestern Baikal area, Russia, in the Neoproterozoic
Publisher: Pleiades Publishing Ltd
Date: 26-10-2013
Secular distribution of highly metalliferous black shales corresponds with peaks in past atmosphere oxygenation
Publisher: Springer Science and Business Media LLC
Date: 17-05-2017
Vanadium-rich ruby and sapphire within Mogok Gemfield, Myanmar: implications for gem color and genesis
Publisher: Springer Science and Business Media LLC
Date: 17-08-2014
Zircon U-Pb geochronology, Hf isotopes and geochemistry of intrusive rocks in the Simorgh prospecting area, Lut Block, eastern Iran: petrogenesis and geological implications
Publisher: Springer Science and Business Media LLC
Date: 19-04-2018
Psychological Therapy for At Risk Mental State for Psychosis in a Prison Setting: A Case Study
Publisher: Wiley
Date: 22-12-2015
DOI: 10.1002/JCLP.22250
Chemical U-Th-Pb monazite dating of the Cambrian Tyennan Orogeny, Tasmania
Publisher: Informa UK Limited
Date: 07-2007
Naturaliste Plateau: constraints on the timing and evolution of the Kerguelen Large Igneous Province and its role in Gondwana breakup
Publisher: Informa UK Limited
Date: 03-10-2017
Multiple melting stages and refertilization as indicators for ridge to subduction formation: The New Caledonia ophiolite
Publisher: Elsevier BV
Date: 03-2010
Geodynamic Significance of the Mesoproterozoic Magmatism of the Udzha Paleo-Rift (Northern Siberian Craton) Based on U-Pb Geochronology and Paleomagnetic Data
Publisher: MDPI AG
Date: 29-11-2018
DOI: 10.3390/MIN8120555
Abstract: The emplacement age of the Great Udzha Dyke (northern Siberian Craton) was determined by the U-Pb dating of apatite using laser ablation inductively coupled plasma mass spectrometry (LA-ICPMS). This produced an age of 1386 ± 30 Ma. This dyke along with two other adjacent intrusions, which cross-cut the sedimentary units of the Udzha paleo-rift, were subjected to paleomagnetic investigation. The paleomagnetic poles for the Udzha paleo-rift intrusions are consistent with previous results published for the Chieress dyke in the Anabar shield of the Siberian Craton (1384 ± 2 Ma). Our results suggest that there was a period of intense volcanism in the northern Siberian Craton, as well as allow us to reconstruct the apparent migration of the Siberian Craton during the Mesoproterozoic.
Adakites in the Truong Son and Loei fold belts, Thailand and Laos: Genesis and implications for geodynamics and metallogeny
Publisher: Elsevier BV
Date: 07-2014
Mineralogy of metal contaminated estuarine sediments, Derwent estuary, Hobart, Australia: implications for metal mobility
Publisher: Informa UK Limited
Date: 07-2013
First insights on the metallogenic signature of magmatic fluids exsolved from the active magma chamber of Vesuvius (AD 79 “Pompei” eruption)
Publisher: Elsevier BV
Date: 03-2011
Pyrite trace element behavior in magmatic-hydrothermal environments: An LA-ICPMS imaging study
Publisher: Elsevier BV
Date: 2021
Passive-margin prolonged volcanism, East Australian Plate: Outbursts, progressions, plate controls and suggested causes
Publisher: Informa UK Limited
Date: 10-2012
In situ Pb-isotope analysis of pyrite by laser ablation (multi-collector and quadrupole) ICPMS
Publisher: Elsevier BV
Date: 05-2009
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