149 research outputs found

    The Eichstädt meteorite, a historical fall in Bavaria from 1785 -revisited

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    第6回極域科学シンポジウム[OA] 南極隕石11月16日(月) 国立極地研究所1階交流アトリウ

    Diabasic/basaltic shergottites NWA 480/1460 and NWA 5029: magnetic properties indicate launch-pairing.

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    第2回極域科学シンポジウム/第34回南極隕石シンポジウム 11月17日(木) 国立国語研究所 2階講

    Comparing the magnetic signatures of Neuschwanstein (EL6) and E-chondritic lithologies of Almahata Sitta (polymict ureilite).

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    第2回極域科学シンポジウム/第34回南極隕石シンポジウム 11月17日(木) 国立国語研究所 2階講

    News on the Machtenstein H5 ordinary chondrite

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    第6回極域科学シンポジウム[OA] 南極隕石11月16日(月) 国立極地研究所1階交流アトリウ

    Almahata Sitta Meteorite: Combination of Raman Spectroscopy and ElectronMicroprobe analysis within the ureilitic lithologies.

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    第2回極域科学シンポジウム/第34回南極隕石シンポジウム 11月17日(木) 国立国語研究所 2階講

    New Results of Micro Raman Spectroscopy and Magnetism on Martian Meteorites.

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    第3回極域科学シンポジウム/第35回南極隕石シンポジウム 11月29日(木)、30日(金) 国立国語研究所 2階講

    Mineralogy and crystallography of vein metals in the Almahata Sitta ureilite.

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    第2回極域科学シンポジウム/第34回南極隕石シンポジウム 11月18日(金) 国立国語研究所 2階講

    Magnetotransport properties of iron microwires fabricated by focused electron beam induced autocatalytic growth

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    We have prepared iron microwires in a combination of focused electron beam induced deposition (FEBID) and autocatalytic growth from the iron pentacarbonyl, Fe(CO)5, precursor gas under UHV conditions. The electrical transport properties of the microwires were investigated and it was found that the temperature dependence of the longitudinal resistivity (rhoxx) shows a typical metallic behaviour with a room temperature value of about 88 micro{\Omega} cm. In order to investigate the magnetotransport properties we have measured the isothermal Hall-resistivities in the range between 4.2 K and 260 K. From these measurements positive values for the ordinary and the anomalous Hall coefficients were derived. The relation between anomalous Hall resistivity (rhoAN) and longitudinal resistivity is quadratic, rhoAN rho^2 xx, revealing an intrinsic origin of the anomalous Hall effect. Finally, at low temperature in the transversal geometry a negative magnetoresistance of about 0.2 % was measured
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