Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
GSA Bulletin Signup for GSW Email News
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

GSA Bulletin; July 2001; v. 113; no. 7; p. 939-958; DOI: 10.1130/0016-7606(2001)113<0939:THOTEM>2.0.CO;2
© 2001 Geological Society of America
This Article
Right arrow Figures Only
Right arrow Full Text
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Right arrow Citation Map
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via ISI Web of Science (14)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Curtis, M. L.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Tectonic history of the Ellsworth Mountains, West Antarctica: Reconciling a Gondwana enigma

Michael L. Curtis*,1

1 British Antarctic Survey, Natural Environment Research Council, High Cross, Madingley Road, Cambridge CB3 0ET, UK

Early Paleozoic orogenesis has been recognized along the southern African (Saldanian orogeny) and East Antarctic (Ross orogeny) sectors of the Gondwana paleo- Pacific margin. However, the absence of a contemporaneous orogenic event in the Ellsworth Mountains of West Antarctica, once a contiguous part of this margin, has resulted in their geology being considered enigmatic. In this contribution, widespread, detailed structural studies from all stratigraphic levels of the Ellsworth Mountains allow their tectonic evolution to be reassessed.

Geochemical, stratigraphic, and structural data indicate that the Middle to Upper Cambrian Heritage Group developed in a continental rift basin. Multiple observations of the crucial end-Cambrian contact between this rift sequence and the overlying Crashsite Group reveal the contact to be regionally conformable; there are localized outcrop-scale unconformities. Furthermore, structural continuity can be demonstrated across this key boundary, thus precluding the possibility of an end-Cambrian orogenic event.

The entire stratigraphic succession was affected by two post-Permian phases of deformation. D1 structures are locally developed and superimposed by the main dextral transpressive D2 Permian–Triassic Gondwanian deformation event. D2 is succeeded by an episode of extension orthogonal to orogenic strike.

Recent geochronological data on the early Paleozoic evolution of the Cape fold belt reveal a strong tectonostratigraphic correlation with the Ellsworth Mountains, indicating that this sector of the Gondwana paleo-Pacific margin was affected by Middle to Late Cambrian rifting. A new tectonic model is proposed for the southwestern paleo-Pacific margin of Gondwana that accounts for the presence of rifting along a margin otherwise dominated by active subduction.

Key Words: Cape Province • Ellsworth Mountains • Gondwana • structural geology • Transantarctic Mountains • South Africa




This article has been cited by other articles:


Home page
Geol Soc Am BullHome page
M.J. Flowerdew, I.L. Millar, M.L. Curtis, A.P.M. Vaughan, M.S.A. Horstwood, M.J. Whitehouse, and C.M. Fanning
Combined U-Pb geochronology and Hf isotope geochemistry of detrital zircons from early Paleozoic sedimentary rocks, Ellsworth-Whitmore Mountains block, Antarctica
GSA Bulletin, March 1, 2007; 119(3-4): 275 - 288.
[Abstract] [Full Text] [PDF]


Home page
Geological Society, London, Special PublicationsHome page
A. P. M. Vaughan, P. T. Leat, and R. J. Pankhurst
Terrane processes at the margins of Gondwana: introduction
Geological Society, London, Special Publications, January 1, 2005; 246(1): 1 - 21.
[Abstract] [PDF]


Home page
Geological Society, London, Special PublicationsHome page
A. P. M. Vaughan and R. A. Livermore
Episodicity of Mesozoic terrane accretion along the Pacific margin of Gondwana: implications for superplume-plate interactions
Geological Society, London, Special Publications, January 1, 2005; 246(1): 143 - 178.
[Abstract] [PDF]


Home page
Geological Society, London, Special PublicationsHome page
A. E. Rapalini
The accretionary history of southern South America from the latest Proterozoic to the Late Palaeozoic: some palaeomagnetic constraints
Geological Society, London, Special Publications, January 1, 2005; 246(1): 305 - 328.
[Abstract] [PDF]


Home page
Journal of the Geological SocietyHome page
T.S. Paulsen, J. EncarnaciOn, and A.M. Grunow
Structure and timing of transpressional deformation in the Shackleton Glacier area, Ross orogen, Antarctica
Journal of the Geological Society, December 1, 2004; 161(6): 1027 - 1038.
[Abstract] [Full Text] [PDF]


Home page
Geol Soc Am BullHome page
M. L. Curtis, I. L. Millar, B. C. Storey, and M. Fanning
Structural and geochronological constraints of early Ross orogenic deformation in the Pensacola Mountains, Antarctica
GSA Bulletin, May 1, 2004; 116(5-6): 619 - 636.
[Abstract] [Full Text] [PDF]


Home page
Journal of the Geological SocietyHome page
C. W. Rapela, C.W. Rapela, R.J. Pankhurst, C.M. Fanning, and L.E. Grecco
Basement evolution of the Sierra de la Ventana Fold Belt: new evidence for Cambrian continental rifting along the southern margin of Gondwana
Journal of the Geological Society, July 1, 2003; 160(4): 613 - 628.
[Abstract] [Full Text] [PDF]




JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Geological Society of America