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Tuesday, July 28, 2020 | History

2 edition of Cambro-Ordovician conodonts from the Burke River Structural Belt, Queensland found in the catalog.

Cambro-Ordovician conodonts from the Burke River Structural Belt, Queensland

E. C. Druce

Cambro-Ordovician conodonts from the Burke River Structural Belt, Queensland

by E. C. Druce

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Published by Dept. of National Development, Bureau of Mineral Resources, Geology and Geophysics in [Canberra] .
Written in English

    Subjects:
  • Conodonts -- Australia -- Queensland.,
  • Paleontology -- Ordovician.,
  • Paleontology -- Cambrian.,
  • Paleontology -- Australia -- Queensland.

  • Edition Notes

    Bibliography: p. 103-106.

    Statementby E. C. Druce and P. J. Jones.
    SeriesBulletin / Australia. Dept. of National Development. Bureau of Mineral Resources, Geology and Geophysics -- 110, Bulletin (Australia. Bureau of Mineral Resources, Geology and Geophysics) -- 110.
    ContributionsJones, P. J.
    Classifications
    LC ClassificationsQE340 .A39 no. 110, QE899 .A39 no. 110
    The Physical Object
    Pagination158 p.
    Number of Pages158
    ID Numbers
    Open LibraryOL16884404M

    Cambrian geology and palaeontology of the headwaters of the Burke River, Queensland. Bureau of Mineral Resources, Geology and Geophysics (Australia), Bulletin, 53, pp. pik, A.A. The Mindyallan fauna of north-western Queensland.5/5(2).   A new look at age and area: the geographic and environmental expansion of genera during the Ordovician Radiation. NASA Technical Reports Server (NTRS) Miller, A. I. Although available paleobiological data indicate that the geographic ranges of marine species are maintained throughout their entire observable durations, other evidence suggests, by contrast, that .

    Figure (a) (above) Seismic images of the Georgina Basin based on deep seismic reflection lines in the region of the Dulcie Syncline (line 09GA-GA1) and (b)(next page) across the Burke River Structural Zone (line 06GAM6)(Carr and Korsch, ; Carr et al., ). 44 Onshore Basin Inventory Basin evolution and depositional history The. Catalog - Hermann L. Strack Hermann L. Strack Livres Anciens - Antiquarian Bookdealer - Antiquariaat Sciences - Histoire Naturelle - Médecine - Voyages Sciences - Natural History - Medicine - Travel Wetenschappen - Natuurlijke Historie - Medisch - Reizen Porzh Hervé - Loguivy Plougras - Bretagne - France Tel./Fax: +(0) / Portable +(0) - email: [email protected].

    To the north and east of Kingston, Jamaica, is a major half-graben structure called the Wagwater Belt, trending northwestsoutheast (Draper ), and named after the Wagwater River. It is bounded on its southwestern side by the Wagwater Fault. Detailed structural studies of the murchison greenstone belt have established, however, that there is a complete lack of continuity of strata from either side of the supposed syncline of the murchison belt, and that the structure is much more complex than the pinched-synform model predicts.


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Cambro-Ordovician conodonts from the Burke River Structural Belt, Queensland by E. C. Druce Download PDF EPUB FB2

Cambro-Ordovician conodonts from the Burke River Structural Belt, Queensland. [Canberra]: [Bureau of Mineral Resources, Geology and Geophysics], (OCoLC) Document Type: Book: All Authors / Contributors: E C Druce; P J Jones.

Middle Cambrian through lowermost Ordovician conodonts from Hunan, South China - Volume 91 Supplement - Xi-ping Dong, Huaqiao Zhang Middle Cambrian through lowermost Ordovician conodonts from Hunan, South China.

Cambro–Ordovician conodonts from the Burke River structural belt Queensland: Bureau of Mineral Resources, Geology and Cited by:   Cambro-Ordovician conodonts from the Burke River structural belt, Queensland, Australia. Bureau of Mineral Resources, Biostratigraphy of the Cambrian–Ordovician transition in the Bear River Range, * Views captured on Cambridge Core Cited by: Study and Use of Upper Cambrian to Lower Ordovician conodonts in central, southern, and western Laurentia, – Cambro-Ordovician conodonts from the Burke River Structural Belt Author: Cambro-Ordovician conodonts from the Burke River Structural Belt Frederick Miller.

The first descriptions of Laurentian Lower Ordovician conodonts were in the s in the central USA. Authors boiled shales to free the conodont elements.

The use of acetic acid began in at the University of Missouri. The first study of Cambrian conodonts was in ; part of the material was from the western USA and part from northern : James F. Miller. Conodonts and microbrachiopods of latest Cambrian–earliest Ordovician age are documented from the Handler Formation of northern Victoria Land, Antarctica.

Abstract. The 70 Ma Ordovician Period is characterized by extensive epeiric seas, paleocontinent dispersal, intervals of intense volcanism and black shale deposition, a greenhouse climate state deteriorating to a brief icehouse state, strong faunal provincialism, and profound changes to the biota including the changeover from the Cambrian Fauna to the Paleozoic by: The Iverian, a proposed Late Cambrian Stage, and its subdivision in the Burke River Structural Belt, western Queensland: Seismic structure and continuity of the Redbank Thrust Zone, central Australia: The West Tasman Sea (Flinders Island) earthquake of 14 September Carter, E.

et al. - Lower and Middle Jurassic radiolarian biostratigraphy and systematic paleontology, Queen Charlotte Islands, British Columbia.

- Geological. Website of the journal Bulletin of Geosciences, published since by The base of the global Dapingian Stage (Ordovician) in Baltoscandia: conodonts, graptolites and unconformities. Earth and Environmental J.H. Idamean (Late Cambrian) trilobites, Burke River structural belt, western Queensland.

Bureau of Mineral Resources. Structural of the Sibumasu-Indochina collision, central Thailand: a section through the Khao Khwang fold-and-thrust belt F. Arboit1*, A.S. Collins1, R. King1, C.K. Morley2 and R.

Hansberry1 Centre for Tectonics Resources and Exploration (TRaX), Department of Earth Sciences, The University of Adelaide, SAAustralia. *[email protected] 2. Podkamenndi Tunguski [Crown of crinoid from Middle Ordovician of Podkamennaya Tunguska River]: Paleontologicheskii Zhurnal, no.

4, p. (In Russian) Paleontologicheskii Zhurnal, no. Late Cambrian and Early Ordovician trilobites from the Burke River Structural Belt, western Queensland, Australia. Australian Bureau of Mineral Resources, Geology and Geophysics Bulletin 1– DRUCE, E.C. & P.J. JONES - Cambro-Ordovician conodonts from the Burke River structural belt, Queensland.

DRUCE DRUCE, E.C. & P.J. JONES - Cambro-Ordovician conodonts from the Burke River structural belt, Queensland DYER, JAMES - Your book of Prehistoric Britain. DYER, W S & M Y WILLIAMS - Geology of southern Alberta. Full text of "Journal and proceedings of the Royal Society of New South Wales" See other formats.

This banner text can have markup. web; books; video; audio; software; images; Toggle navigation. References on carbonate microfacies used for the book. Febr Keywords used. Note that the ranking of keyword numbers does not necessarily coincide with chapters or sections of the book and that some keywords lead to just a few references but not to a.

Cambro-Ordovician conodonts from the Burke River Structural Belt, Queensland. Canberra ACT: Bureau of Mineral Resources, Geology & Geophysics, Bulletin,p. [Google Scholar].Cited by: 4. Bogen, N.L., D.V.

Kent, and R.A. Schweickert, Paleomagnetism of Jurassic rocks in the western Sierra Nevada metamorphic belt and its bearing on the structural evolution of the. New England Orogen, eastern Australia Papers presented at a conference held at The University of New England,Armidale February The Central Belt consists of a stratigraphically and structurally complex Cambro-Ordovician sequence, key elements of which include the late Middle Cambrian Devil River Volcanics, and the probably slightly.

Idamean (Late Cambrian) trilobites, Burke River Structural Belt, western Queensland. Bureau of Mineral Resources, Geology and Geophysics, Bulletin,1 – 69, pl. 1 – [Google Scholar]). The fauna from C some m below C has a probable Guzhangian age (see below), thus suggesting a late Guzhangian or Paibian age for the Author: X.

W. Sun, C. J. Bentley, J. B. Jago.PO DRUCE, E.C. & P.J. JONES - Cambro-Ordovician Conodonts from the Burke River Structural Belt, Queensland PO DRUCE, E.C.

- Devonian and Carboniferous Conodonts from the Bonaparte Gulf basin, northern Australia and their use in international correlation.The Ordovician Period was characterized by several major events, including a prolonged 'super greenhouse' during the Early Ordovician, the 'Great Ordovician Biodiversification Event (GOBE)' of the Middle and early Late Ordovician, and the Hirnantian ice age and mass extinction of the latest Ordovician (Webby et al.,The Great Ordovician.