Upper Palaeozoic formations in the Mt. Morgan district faunas by W. G. H. Maxwell

Cover of: Upper Palaeozoic formations in the Mt. Morgan district | W. G. H. Maxwell

Published by University of Queensland Press in Brisbane .

Written in English

Read online

Places:

  • Australia,
  • Mount Morgan Region.

Subjects:

  • Invertebrates, Fossil -- Australia -- Mount Morgan Region.,
  • Paleontology -- Paleozoic.,
  • Paleontology -- Australia -- Mount Morgan Region.

Edition Notes

Bibliography: p. 50-54.

Book details

Statementby W. G. H. Maxwell.
Series[Papers] - University of Queensland, Dept. of Geology ; v. 4, no. 5, Papers (University of Queensland. Dept. of Geology) ;, v. 4, no. 5.
Classifications
LC ClassificationsQE340 .P36 vol. 4, no. 5, QE770 .P36 vol. 4, no. 5
The Physical Object
Pagination69 p. :
Number of Pages69
ID Numbers
Open LibraryOL5239744M
LC Control Number75310896

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The genus Strophalosia in the Permian of Queensland ; and, The palaeontology, stratigraphy and structure of the upper palaeozoic formations in the Mt.

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Morgan district -- stratigraphy and structure. By W. (William Graham Henderson) Maxwell. Download PDF (32 MB)Author: W. (William Graham Henderson) Maxwell. Stratigraphic Unconformities: Review of the Concept and Examples from the Middle-Upper Paleozoic Chapter (PDF Available) December with 1, Reads How we measure 'reads'Author: Pavel Kabanov.

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δ 13 C org stable isotope data correlated to conodont-constrained global isotopic curves indicates. Mount Everest is composed of Upper Carboniferous limestones.

Coal formation started in the Carboniferous age. Carboniferous in geology means coal bearing. [most of the coal found in India is not of Carboniferous period; High quality coal of Great Lakes Region-USA, U.K and Ruhr region is Carboniferous coal]. Aryan Rock System. The early Upper Cretaceous I-type granites in the arc correlate with the Gangdise batholith in Tibet, but it is unclear how these granites relate to I-type granites in the Mogok Metamorphic belt.

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