Titlebook: Origin of Thermoremanent Magnetization; Proceedings of AGU 1 David J. Dunlop Conference proceedings 1977 Center for Academic Publications J

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書目名稱Origin of Thermoremanent Magnetization影響因子(影響力)




書目名稱Origin of Thermoremanent Magnetization影響因子(影響力)學(xué)科排名




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書目名稱Origin of Thermoremanent Magnetization讀者反饋




書目名稱Origin of Thermoremanent Magnetization讀者反饋學(xué)科排名

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Domain Structure of Titanomagnetites and Its Variation with Temperature, less than —40°C in the central to more than 70°C in the marginal zones of the crystals was found by observing the variation of the domain structure with temperature. The effect is explained by the different degree of maghemitization. TRM production in fields of 35 Oe revealed that the direction of

指數(shù)

The Demagnetization Field of Multidomain Grains,simply to the shape of the grain, no theoretical study of . has previously been completed. It is shown in this paper that. monotonically increases with increase in remanence in multidomain grains. Although . can be approximated by a constant in the limit of small displacements of domain walls from t

justify

牢騷

aerobic

The Preparation, Characterization and Magnetic Properties of Synthetic Analogues of Some Carriers ostem prepared by oxidation of Fe.Mg.Ti.O.(0<δ<0.35). The following properties were determined: unit cell edge, Curie temperature, thermomagnetic behaviour, saturation magnetization, isothermal remanence and coercive force. The introduction of Al, Mg and vacancies into titanomagnetites reduces satura

Jargon

Reduction of Hematite to Magnetite under Natural and Laboratory Conditions,tite occurs when the experiment is perfomed in vacuum but not when it is performed in air 2) the reduction is arrested when the sample is heated in air before the vacuum run. In addition, we have found that the reduction is controlled by backstreaming vacuum pump oils, which buffer the atmosphere in

十字架

myalgia

Thermal Overprinting of Natural Remanent Magnetization and K/Ar Ages in Metamorphic Rocks,ingle geological unit. We trace the steps necessary to resolve and date such magnetic overprints in three studies of intensely metamorphosed rocks from the Grenville Province of the Canadian Precambrian Shield. First, it is shown that the various components may be associated with different rock-form

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