3,010 research outputs found
Addendum to 'Highly efficient blue photoluminescence from colloidal lead-iodide nanoparticles' [Journal of Physics D. 39 (8) 1477, 2006]
No full textIn a recent paper (Finlayson C E and Sazio P J A 2006 J. Phys. D: Appl. Phys. 39 1477–80) we reported on the properties of colloidal lead (II) iodide nanoparticles, synthesized via a route using coordinating solvents. Our samples were characterized as having highly efficient and photostable photoluminescence in the blue region of the visible spectrum. Subsequent experiments show the observed behaviour of these nanoparticles during nucleation and ripening to be more complicated than originally reported and we believe that the observed photoluminescence may be related to extraneous factors, beyond the experimental methods as previously described
Finlayson, A J (Arthur James), NX34356
No full textThis record was harvested from a previous catalogue system and will be withdrawn in 2025. Information in this record may be superseded or incomplete. Visit this record in UMA's new catalogue at: https://archives.library.unimelb.edu.au/nodes/view/385089Surname: FINLAYSON. Given Name(s) or Initials: A J (ARTHUR JAMES). Military Service Number or Last Known Location: NX34356. Missing, Wounded and Prisoner of War Enquiry Card Index Number: 15439.230831
Item: [2016.0049.17382] "Finlayson, A J (Arthur James), NX34356
Florius Infortunatus, scribe and author
No full textFinlayson Charles-P. Florius Infortunatus, scribe and author. In: Scriptorium, Tome 19 n°1, 1965. pp. 108-109
Plural wife: the life story of Mabel Finlayson Allred
No full textEdited by Martha Bradley-Evans.Includes bibliographical references.Introduction -- Martha Bradley-Evans; Preface -- Mabel Finlayson Allred; My Life Story -- Mabel Finlayson Allred; Postlude: Dedication to their parents -- The Allred children; "My Darling Mabel": Letters and poetry -- From Rulon C. Allred to Mabel Allred
Lagorchestes asomatus Finlayson 1943
No full textLagorchestes asomatus Finlayson, 1943 Trans. Roy. Soc. South. Aust. 67(2): 319, figs xxxiii, xxxiv. (30 November 1943). Common name. Central Hare-wallaby. Current name. Lagorchestes asomatus Finlayson, 1943; following Jackson & Groves (2015). Material. AM M.28248, cast of holotype cranium and both dentaries of SAM M.3710, sex unknown, Western Plateau, between Mt Farewell and Lake Mackay, Northern Territory. Cast registered in the AM on 8 December 1992. Condition of cast. Cast of cranium and both dentaries, missing 3rd right upper (maxillary) incisor and left dentary missing angular process. Comments. Described only from the holotype cranium and dentaries, holotype in SAM.Published as part of Parnaby, Harry E., Ingleby, Sandy & Divljan, Anja, 2017, Type Specimens of Non-fossil Mammals in the Australian Museum, Sydney, pp. 277-420 in Records of the Australian Museum 69 (5) on page 401, DOI: 10.3853/j.2201-4349.69.2017.1653, http://zenodo.org/record/523780
Trichosurus vulpecula subsp. raui Finlayson 1963
No full text<i>Trichosurus vulpecula raui</i> Finlayson, 1963 <p> <i>Trans. R. Soc. S. Aust.</i> 87: 18, tables 1–2. (December 1963).</p> <p> <b>Common name</b>. Common Brush-tailed Possum.</p> <p> <b>Current name</b>. <i>Trichosurus vulpecula vulpecula</i> (Kerr, 1792), following Jackson & Groves (2015).</p> <p> <b>Paratypes</b>. (2, by subsequent determination): <b>M.4839</b> (formerly SAM M2515), male; <b>M.4840</b> (formerly SAM M2525), female, both study skins and skulls, collected by H. H. Finlayson and F. J. Rau in August 1928 from Rocky River, Flinders Island, South Australia, received from South Australian Museum in 1930.</p> <p> <b>Comments</b>. Although the two AM specimens were sent from SAM three decades before publication of Finlayson’s paper, they evidently form part of the original series of 30 specimens he referred to in his description. Aitken (1976) states that two paratypes were sent to theAM: SAM M.2515, male and SAM M.2525, female, both skins and skulls, with same collection data and locality as the holotype (SAM M.2518) given in the South Australian Museum register. Finlayson cites the registration number of the holotype only, in his account.</p>Published as part of <i>Parnaby, Harry E., Ingleby, Sandy & Divljan, Anja, 2017, Type Specimens of Non-fossil Mammals in the Australian Museum, Sydney, pp. 277-420 in Records of the Australian Museum 69 (5)</i> on page 328, DOI: 10.3853/j.2201-4349.69.2017.1653, <a href="http://zenodo.org/record/5237800">http://zenodo.org/record/5237800</a>
North America / drawn by J. Finlayson engraved by J. Yeager.
No full textRelief shown by hachures.; Enclosed by large text block providing information about boundaries, geographic features, and discovery and settlement of North America.; Northwest boundary of Missouri Territory at 54⁰ 40' N. latitude.; Likely from: Carey, Henry Charles. A complete historical ... American atlas. Philadelphia, 1827
Age and Chemostratigraphy of the Finlayson Lake District, Yukon: Implications for Volcanogenic Massive Sulfide (VMS) Mineralization and Tectonics along the Western Laurentian Continental Margin
No full textAbstractThe Yukon-Tanana terrane in the Finlayson Lake district, Yukon, represents one of the first arc–back-arc systems that formed adjacent to the Laurentian continental margin in the mid-Paleozoic. Back-arc rocks contain many large and high-grade volcanogenic massive sulfide (VMS) deposits. This study integrates U-Pb zircon geochronology, lithogeochemistry, and Hf-Nd isotopes to establish precise controls on tectonomagmatic activity adjacent to the western Laurentian margin in the Late Devonian to Early Mississippian. High-precision chemical abrasion- (CA-) ID-TIMS U-Pb zircon geochronology defines coeval arc (ca. 363.1 to 348 Ma) and back-arc (ca. 363.3 to 355.0 Ma) magmatism in the Finlayson Lake district that intruded continental crust of Laurentian affinity (e.g., Snowcap assemblage). Mafic and felsic rocks display geochemical and isotopic characteristics that are consistent with being formed from mixtures of depleted asthenosphere and enriched lithospheric mantle sources. These melts variably entrained Laurentian continental crust via high-temperature crustal melting due to basaltic underplating. The high-temperature back-arc felsic magmatism occurs at specific time periods coinciding with VMS deposits and supports previous genetic models for VMS mineralization that suggest elevated heat flow and hydrothermal circulation were due to regional-scale rift-related magmatism rather than from local subvolcanic intrusions. The short timescales and transient nature of tectonomagmatic events in the Finlayson Lake district suggest that rapid and complex subduction initiation of oceanic and continental crust fragments facilitated coeval compression, extension, and magmatism in the arc and back-arc regions. We thus reevaluate the presently accepted tectonostratigraphic framework of the Finlayson Lake district and suggest revised interpretations that shed light on VMS depositional environments and a possible broader association with the ca. 358 Ma Antler Orogeny. Results of this study have implications for incipient tectonics, magmatism, and mineralization along the western Laurentian continental margin and other orogenic belts globally
Pseudomys apodemoides Finlayson 1932
No full textPseudomys apodemoides Finlayson, 1932. Trans. Proc. R. Soc. S. Aust., 56:170. TYPE LOCALITY: Australia, Southern Australia, Coombe. DISTRIBUTION: S.E. South Australia; W. Victoria; New South Wales. COMMENT: Ride, 1970, included this species in albocinereus, but Baverstock et al., 1977, Aust. J. Biol. Sci., 30:471-485, considered it a distinct species.Published as part of James H. Honacki, Kenneth E. Kinman & James W. Koeppl, 1982, Order Rodentia (Part 5), pp. 504-560 in Mammal Species of the World (1 st Edition), Lawrence, Kansas, USA :Alien Press, Inc. & The Association of Systematics Collections on page 545, DOI: 10.5281/zenodo.735303
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An 11 600 year-old communal structure from the Neolithic of southern Jordan
No full textThe authors present a new type of communal
and monumental structure from the earliest
Neolithic in western Asia. A complement to
the decorated stone pillars erected at G¨obekli
Tepe in the north, ‘Wadi Faynan 16 Structure
O75’ in the southern Levant is a ritualised
gathering place of a different kind. It serves to
define wider western Asia as an arena of social
experiment in the tenth millennium BC, one
in which community seems to take precedence
over economy
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