Abstract
Palaeomagnetic analysis of Mesozoic pelagic
sediments of the island of Misool, northeast Indonesia,
showed that a large part of the sediments
have very low initial remanence intensities.
Progressive demagnetization both with alternating
magnetic fields and with heating yielded
characteristic remanence directions in two formations:
the Waaf Formation of Santonian age
revealed the following data: D = 318.10, I
... read more