The total magnetic composition of a rock sample can be revealed by a stepwise
demagnetization. Hence these progressive demagnetizations are the most valuable bases in …

The results of a detailed magnetostratigraphic and biostratigraphic study of late Pliocene to
early Pleistocene marine marl sequences from the Monte Singa and Crotone areas in …

Rock magnetic parameters are often used to recognize variations in the original magnetic
mineralogy and for normalizing purposes in palaeointensity studies. Incipient weathering, …

The natural remanent magnetizations of 35 samples from five quarries in the Permian traps
from the Exeter region were carefully examined. A considerable number of the samples …

Alternating field (af) demagnetization has proved to be a very reliable technique for separating
the magnetization components of rock samples. The method is subject to errors caused …

A well‐dated, high‐resolution record of climatic change is presented for the late Pliocene
Mediterranean. Principal component analysis on abundances of 14 planktonic foraminiferal …

The method presented is based on monitoring changes in the coercivity spectrum of an
isothermal remanent magnetization (IRM) during stepwise thermal demagnetization. The …

Two paleomagnetic studies of the Lisbon basalts by ND Watkins and A. Richardson and by
R. Van der Voo bearing on the problem of the rotation of the Iberian Peninsula have lately …

PALAEOMAGNETIC data from Middle Tertiary rocks have not decisively shown any rotation
of Sardinia 1 . Rocks of Permian age, which seemed most suitable for detecting rotations of …

Six Upper Miocene marine clay sections on Crete (Greece) have been subjected to a detailed
magnetobiostratigraphic analysis. Six correlatable polarity zones are recognized and …