Abstract
Klootwijk, C.T., 1974. Palaeomagnetic data from the Precambrian Gwalior Traps, Central
India. Tectonophysics, 21: 181-195.
From alternating-field and thermal demagnetization studies on two dolerite “Traps” in
the Gwalior Series (Central India), dated at 1830 f200 m.y., three different palaeomagnetic
directions could be distinguished. The characteristic magnetization component,
which is considered as the primary magnetization, has
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