1. Remagnetization of Mesozoic limestones from the Jaisalmer basin, NW India.
- Author
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Torsvik, T. H., Pandit, M. K., Redfield, T. F., Ashwal, L. D., and Webb, S. J.
- Subjects
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MAGNETIZATION , *MESOZOIC stratigraphic geology , *LIMESTONE , *FERROMAGNETISM - Abstract
High coercivity but low unblocking (LB) temperature components (∼80–100°C) demonstrate that goethite is the principal carrier of the natural remanent magnetization (NRM) in Jurassic and Cretaceous limestone from the Jaisalmer basin (Rajasthan, NW India). Goethite-bearing components (declination= 359.9°, inclinationsites) plot close to the present day field direction. High unblocking (HB) components (declination= 172.0°, inclinationsites) are carried by haematite, mostly with reverse polarity directions, but undoubtedly not primary. This remagnetization event, mostly within a period of reverse magnetic polarity, occurred after 35 Ma and before 780 000 yr (the last known reversal). Only palaeomagnetic data from a single Cretaceous site (declination= 302.0°, inclinationsamples) has potentially preserved a primary magnetization (carried by normal polarity magnetite); if correct, this site substantiates a mid-southerly palaeolatitude for India during mid-Aptian times (∼117 Ma). [ABSTRACT FROM AUTHOR]
- Published
- 2005
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