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Journal of the Geological Society; May 2007; v. 164; no. 3; p. 581-597; DOI: 10.1144/0016-76492005-184
© 2007 Geological Society of London
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Original Article

Magneto-biostratigraphy of the Middle to Upper Triassic transition, central Spitsbergen, arctic Norway

Mark W. Hounslow1, Mengyu Hu1, Atle MØrk2, Jorunn Os Vigran2, Wolfgang Weitschat3 and Michael J. Orchard4

1 1Department of Geography, Lancaster University, Lancaster LA1 4YB UK (e-mail: m.hounslow@lancs.ac.uk)
2 2SINTEF Petroleum Research, N-7465 Trondheim, Norway
3 3Geologisch-Paläontologisches Institut und Museum, Universität Hamburg, Bundesstrasse 55, 20146 Hamburg, Germany
4 4Geological Survey of Canada, 101–605 Robson Street, Vancouver, BC, V6b 5J3, Canada

Palaeomagnetic and biostratigraphic data were obtained for the latest Ladinian and most of the Carnian (Botneheia Formation to basal Kapp Toscana Group), from two sections in central Spitsbergen (Svalbard archipelago). Thermal and alternating field (AF) demagnetization reveals a magnetization of both normal and reversed polarities. The mean directions pass reversal and fold tests and are similar to other European Late Triassic palaeopoles. One of the sections displays 15° of vertical-axis, clockwise, tectonic rotation on a décollement in the underlying Botneheia Formation. The magnetostratigraphy is dominated by normal polarity in the uppermost Botneheia Formation and into the Tschermakfjellet and basal De Geerdalen formations. A substantial hiatus characterizes the Ladinian–Carnian boundary in central Spitsbergen, so reverse magnetozones, identified in Tethyan sections near this boundary, are absent. Magnetostratigraphic correlation, along with palynostratigraphic constraints, indicates that most of the De Geerdalen Formation is Lower Carnian. The magnetostratigraphy and palynology indicates that the Isfjorden Member (upper unit of the De Geerdalen Formation) is probably mid-Carnian in age. Change in the lithological architecture in the Isfjorden Member, compared with the underlying parts of the De Geerdalen Fm, suggests a hiatus near the base of the member, which may represent a mid-Carnian unconformity, not previously recognized on Spitsbergen.




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Geological Society of America BulletinHome page
M. W. Hounslow, C. Peters, A. Mork, W. Weitschat, and J. O. Vigran
Biomagnetostratigraphy of the Vikinghogda Formation, Svalbard (Arctic Norway), and the geomagnetic polarity timescale for the Lower Triassic
Geological Society of America Bulletin, September 1, 2008; 120(9-10): 1305 - 1325.
[Abstract] [Full Text] [PDF]




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