Skip to main content Accessibility help

We use cookies to distinguish you from other users and to provide you with a better experience on our websites. Close this message to accept cookies or find out how to manage your cookie settings.

Close cookie message
×
  1. Home
  2. Journals
  3. Geological Magazine
  4. Volume 99
Journal Home
Refine listing

Refine listing

Access:
Publication date:

Actions for selected content:

Select all | Deselect all
  • View selected items
  • Export citations
  • Download PDF (zip)
  • Save to Kindle
  • Save to Dropbox
  • Save to Google Drive

Save Search

You can save your searches here and later view and run them again in "My saved searches".

Please provide a title, maximum of 40 characters.
Cancel
×
< Back to all issues

Volume 99 - October 1962

Contents

Page 4 of 5

Correspondence

  • Structures of Devon and Cornwall

  • S. Simpson
  • Published online by Cambridge University Press:
    01 May 2009, pp. 284-286
    • Article
      • You have access
    • PDF
    • Export citation

  • Malvern Structures

  • T. Whitworth
  • Published online by Cambridge University Press:
    01 May 2009, pp. 375-379
    • Article
      • You have access
    • PDF
    • Export citation

  • ? Early Tertiary Fold Movements in Mull

  • E. B. Bailey
  • Published online by Cambridge University Press:
    01 May 2009, pp. 478-479
    • Article
      • You have access
    • PDF
    • Export citation

Reviews

Correspondence

  • The Occurrence of Pedunculate Brachiopods in Soft Sediments

  • D. V. Ager
  • Published online by Cambridge University Press:
    01 May 2009, pp. 184-186
    • Article
      • You have access
    • PDF
    • Export citation

Articles

  • The Structure of the Scotia Arc

  • Donald D. Hawkes
  • Published online by Cambridge University Press:
    01 May 2009, pp. 85-91

  • It is suggested that the Scotia Arc was formed after the disruption of a continental strip between South America and Antarctica by an eastward advance of the Pacific crust; volcanic island arcs and associated trenches developed at the juction of the Pacific and Atlantic crustal types; the Scotia Arc migrated eastward with time; and that the crustal structure of the Scotia Sea is in the process of changing from an oceanic (Pacific) to a continental type.

Correspondence

  • Torridonian Microfossils

  • J. Sutton
  • Published online by Cambridge University Press:
    01 May 2009, p. 379
    • Article
      • You have access
    • PDF
    • Export citation

Reviews

Correspondence

  • Festoon Bedding

  • J. Sutton, J. V. Watson
  • Published online by Cambridge University Press:
    01 May 2009, pp. 286-287
    • Article
      • You have access
    • PDF
    • Export citation

  • Precambrian Perthosites in Nyasaland

  • Mihir K. Bose
  • Published online by Cambridge University Press:
    01 May 2009, p. 92
    • Article
      • You have access
    • PDF
    • Export citation

Reviews

Correspondence

  • Validation of the Name Nothodiscus for a Genus of Cretaceous Ammonites

  • R. Casey
  • Published online by Cambridge University Press:
    01 May 2009, pp. 479-480
    • Article
      • You have access
    • PDF
    • Export citation

Reviews

Review

Reviews

Correspondence

  • Origin of Albite Porphyroblasts

  • K. A. Jones
  • Published online by Cambridge University Press:
    01 May 2009, pp. 92-94
    • Article
      • You have access
    • PDF
    • Export citation

Reviews

Correspondence

  • New Record of Anthraconauta Tenuis

  • John Myers
  • Published online by Cambridge University Press:
    01 May 2009, p. 94
    • Article
      • You have access
    • PDF
    • Export citation

Page 4 of 5