The microwave frequency method

被引:4
|
作者
Walton, Derek [1 ]
Boehnel, Harald N. [2 ]
机构
[1] McMaster Univ, Dept Phys & Astron, Hamilton, ON L8S 4M1, Canada
[2] Univ Nacl Autonoma Mexico, Ctr Geociencias, Queretaro 76230, Mexico
基金
加拿大自然科学与工程研究理事会;
关键词
palaeointensities; overprints; microwaves; dating;
D O I
10.1016/j.pepi.2008.02.012
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We present new results showing that when sufficient microwave power is employed the grains carrying the natural remanent moment (NRM) that are able to absorb microwaves reach their blocking temperature in less than 10 ms, and the sample temperature at the end of this very short time has only increased by about 30 degrees C. We also show that because large gaps exist in the spin-wave frequency of small particles, some grains are unable to absorb because they are too small, and others because they are too large. A large number of results have been published, that were obtained using frequencies close to 14 GHz, using what has been called the microwave Thellier method. However, as Biggin has pointed out [Biggin, AJ., et al., 2007. A comparison of a quasi-perpendicular method of absolute palaeointensity determination with other thermal and microwave techniques. Earth Planet. Sci. Lett. 257,564-5811 the microwaves constitute a marginal improvement on thermal methods, with the attendant alteration problems. We wish to propose a radically new method here, the microwave frequency method, where the microwave frequency is varied, selectively magnetizing and demagnetizing grains of different sizes thereby keeping the sample temperature so low that alteration is avoided completely. (C) 2008 Elsevier B.V. All rights reserved.
引用
收藏
页码:145 / 148
页数:4
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