Frederick Sutherland

Dr. Frederick Sutherland

Geoscience, Australian Museum, 1 William Street, Sydney, New South Wales 2010, Australia
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Research Focus & Metrics

Academic Career Length

44Years (1983-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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28 September 2009 in Australian Journal of Earth Sciences
Verified
Journal Article
Closed access
Frederick SutherlandFrederick Sutherland
Frederick Sutherland
Khin ZawKhin Zaw
Khin Zaw
SMSebastien Meffre
Sebastien Meffre
GGG. Giuliani
G. Giuliani
AFAnthony Fallick
Anthony Fallick
GWG. B. Webb
G. B. Webb
Gem corundum, a minor but persistent megacryst in east Australian basalt fields, is mined from some placer concentrations. Laser ablation, inductively coupled plasma mass spectrometry analyses and O isotope determinations on a colour range of corundum from different fields, show that chromophore (Fe, Cr, Ti, V) and genetic indicator (Ga, Mg, δ18O) values can distinguish corundum sources (magmatic, metamorphic and metasomatic) before basalt incorporation. They also characterise corundum groups from different fields. This identified two metamorphic groups, one carrying ruby at Barrington Tops, and a magmatic group distinct from those from other gem fields (lower Fe, northeast Tasmania; higher Fe, Yarrowitch). Ruby-bearing groups show clear provincial characteristics and include lower temperature spinel-facies groups (Barrington, Yarrowitch) and higher temperature garnet-facies groups (Cudgegong–Macquarie River). High Mg/Fe and Ni values in the latter approach those for corundum in diamond, and are a possible diamond indicator. The corundum derived from diverse fold-belt and felsic sources in underlying lithosphere forms a dataset for comparing corundum from other basalt fields.

22 April 2008 in Ore Geology Reviews
Verified
Journal Article
Closed access
Frederick SutherlandFrederick Sutherland
Frederick Sutherland
JDJ.M. Duroc-Danner
J.M. Duroc-Danner
SMSebastien Meffre
Sebastien Meffre

10 July 2002 in Records of the Australian Museum
Verified
Journal Article
Closed access
Frederick SutherlandFrederick Sutherland
Frederick Sutherland
IGI. T. Graham
I. T. Graham
RPR. E. Pogson
R. E. Pogson
DSD. Schwarz
D. Schwarz
GWG. B. Webb
G. B. Webb
TAT. C. Allen
T. C. Allen

30 December 2014 in Minerals
Verified
Journal Article
Open access
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Frederick SutherlandFrederick Sutherland
Frederick Sutherland
Khin ZawKhin Zaw
Khin Zaw
SMSebastien Meffre
Sebastien Meffre
TYTzen-Fui Yui
Tzen-Fui Yui
Kyaw ThuKyaw Thu
Kyaw Thu
Mogok gem corundum samples from twelve localities were analyzed for trace element signatures (LA-ICP-MS method) and oxygen isotope values (δ18O, by laser fluorination). The study augmented earlier findings on Mogok gem suites that suggested the Mogok tract forms a high vanadium gem corundum area and also identified rare alluvial ruby and sapphire grains characterised by unusually high silicon, calcium and gallium, presence of noticeable boron, tin and niobium and very low iron, titanium and magnesium contents. Oxygen isotope values (δ18O) for the ruby and high Si-Ca-Ga corundum (20‰–25‰) and for sapphire (10‰–20‰) indicate typical crustal values, with values >20‰ being typical of carbonate genesis. The high Si-Ca-Ga ruby has high chromium (up to 3.2 wt % Cr) and gallium (up to 0. 08 wt % Ga) compared to most Mogok ruby (<2 wt % Cr; 6), and with other features suggest a potential skarn-like, carbonate-related genesis with a high degree of magmatic fluid input The overall trace element results widen the range of different signatures identified within Mogok gem corundum suites and indicate complex genesis. The expanded geochemical platform, related to a variety of metamorphic, metasomatic and magmatic sources, now provides a wider base for geographic typing of Mogok gem corundum suites. It allows more detailed comparisons with suites from other deposits and will assist identification of Mogok gem corundum sources used in jewelry.

31 January 2015 in Ore Geology Reviews
Verified
Journal Article
Closed access
SVS.V. Vysotskiy
S.V. Vysotskiy
VNVictor Nechaev
Victor Nechaev
АКАлександр Кисин
Александр Кисин
VYV.V. Yakovenko
V.V. Yakovenko
AIA.V. Ignat'Ev
A.V. Ignat'Ev
AAA.I. Agoshkov
A.I. Agoshkov

5 January 2019 in Minerals
Verified
Journal Article
Open access
PDF file
Frederick SutherlandFrederick Sutherland
Frederick Sutherland
Khin ZawKhin Zaw
Khin Zaw
SMSebastien Meffre
Sebastien Meffre
JTJay Thompson
Jay Thompson
KGKarsten Goemann
Karsten Goemann
SHStephen J. Harris
Stephen J. Harris
Ruby in diverse 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, >60–40 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 diverse results emphasize ruby’s potential for geographic typing.