Rock magnetic studies of Miocene volcanics in eastern Otago and Banks Peninsula, New Zealand: Comparison between Curie temperature and low temperature susceptibility behaviour

1988 ◽  
Vol 31 (2) ◽  
pp. 225-235 ◽  
Author(s):  
Graham J. Sherwood
2017 ◽  
Author(s):  
Alison R. Duvall ◽  
◽  
Camille Collett ◽  
Rebecca M. Flowers ◽  
Gregory E. Tucker ◽  
...  
Keyword(s):  

1992 ◽  
Vol 81 (7) ◽  
pp. 575-578 ◽  
Author(s):  
Suresh G. Mishra ◽  
Ramesh V. Pai

1989 ◽  
Vol 67 (11) ◽  
pp. 1942-1948 ◽  
Author(s):  
M. S. R. Cader ◽  
R. C. Thompson ◽  
F. Aubke

Magnetic susceptibility measurements to 4.2 K are reported forO2+[AsF6]−, Br2+[Sb3F16]−, and I2+[Sb2F11]−. The data are interpreted utilizing previous results from photoelectron spectroscopy, known crystal structures, magnetic studies on the superoxide ion and the ozonide ion, and in the case of O2+[AsF6]−, previous ESR studies. The magnetic properties of the three materials are quite different. Br2+[Sb3F16]− obeys Curie–Weiss law between 80 and 4 K: Cm = 0.49 ± 0.01 cm3 mol−1 K and 9 = −0.74 ± 0.01 K (with TIP = 120 × 10−6 cm3 mol−1). The magnetic moment decreases slightly from 2.04 μB at room temperature to 1.93 μB at 4 K. I2+[Sb2F11]− exhibits relatively strong antiferromagnetic coupling with a maximum in χM observed at −54 K. The magnetic moment (corrected for a TIP contribution of 68 × 10−6 cm3 mol−1) decreases from 1.92 μB at 124 K to 0.41 μB at 4 K. Experimental susceptibilities for this compound over the range 300–4 K have been compared to values calculated using three different theoretical models for extended chains of antiferromagnetically coupled paramagnetic species. O2+[AsF6]− exhibits Curie–Weiss behaviour over the range 60–2 K (Cm = 0.34 ± 0.01 cm3 mol−1 K, θ = −1.90 ± 0.01 K). The magnetic moment, uncorrected for TIP, varies from 1.63 μB at 80 K to 1.17 μB at 2 K, and the presence of weak antiferromagnetic coupling in this material is suggested. Keywords: magnetic susceptibilities, dihalogen cations, dioxygenyl cation, low temperature behaviour.


1975 ◽  
Vol 14 (3) ◽  
pp. 313-316 ◽  
Author(s):  
K.S.V.L. Narasimhan ◽  
M.J. Klein ◽  
R.A. Butera

Author(s):  
J. B. Wright

SummaryEarlier palaeomagnetic studies on the Dunedin volcano showed that a portion of the sequence is reversely or anomalously magnetized. Some of the rocks used for palaeomagnetic study were subsequently classified into groups according to their thermomagnetic behaviour (unpublished work).Cell dimensions and Curie-point curves have been measured for oxides separated from representative rocks of each group. The oxides are mostly homogeneous titanomagnetites containing between 40 and 55 mol. % of ulvöspinel, with a generally small degree of late low-temperature alteration. X-ray and thermomagnetic data also suggest that there was some early oxidation to titanomaghemite, probably during cooling.The thermomagnetic behaviour of rocks classified in the different groups is attributed to variable oxidation of the titanomagnetite during thermomagnetic treatment. The high Curie points of rocks used for palaeomagnetic studies may often be due merely to oxidation of titaniferous magnetite and not to nearly pure primary Fe3O4. Since there is insufficient oxidation in the lavas examined for any currently accepted self-reversal process to have been operative, the reversely magnetized part of the Dunedin sequence was probably erupted during a reversed polarity epoch, possibly between about 13 and 11 million years ago.The basanitic lavas contain minor amounts of chromiferous spinel, as inclusions in silicate phenocrysts and as cores to separate microphyric titanomagnetite; its significance is briefly discussed.


2005 ◽  
Vol 94 (10) ◽  
Author(s):  
D. P. Young ◽  
M. Moldovan ◽  
X. S. Wu ◽  
P. W. Adams ◽  
Julia Y. Chan

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