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Titlebook: Energy Dispersive Spectrometry of Common Rock Forming Minerals; Kenneth P. Severin Book 2004 Springer Science+Business Media Dordrecht 200

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發(fā)表于 2025-3-21 18:19:31 | 只看該作者 |倒序?yàn)g覽 |閱讀模式
書(shū)目名稱Energy Dispersive Spectrometry of Common Rock Forming Minerals
編輯Kenneth P. Severin
視頻videohttp://file.papertrans.cn/311/310228/310228.mp4
圖書(shū)封面Titlebook: Energy Dispersive Spectrometry of Common Rock Forming Minerals;  Kenneth P. Severin Book 2004 Springer Science+Business Media Dordrecht 200
描述."This book came about because of my poor memory: it is amazing how quickly and easily an experienced electron microscopist/mineralogist can identify minerals with an Energy Dispersive Spectrometer (EDS). It is also amazing how long it takes someone who is not good at mineralogy to search through a mineralogy text, trying to match the peaks on their unknown spectrum with the chemical formula of some mineral. After the mineral is finally identified, it is easy to identify other specimens of similar composition as EDS spectra have very distinctive patterns. For me, however, as I move between projects, it is easy to forget the patterns. After several episodes of having to relearn the spectra of some all too common rock forming minerals, I decided that a book of EDS ‘flashcards’ would be useful - a catalogue of the minerals that are commonly found in rocks. In addition, why not make a key? This would save a fair amount of time for those who are less experienced mineralogists, but, for whatever reason, use an Energy Dispersive Spectrometer to identify minerals."..Ken Severin...Providing a very basic introduction to Electron Microscopy and Energy Dispersive Spectrometry, the book’s impor
出版日期Book 2004
關(guān)鍵詞EDS spectra; electron microprobe; rock forming minerals; electron microscopy; mineral; mineralogy; economi
版次1
doihttps://doi.org/10.1007/978-1-4020-2841-0
isbn_softcover978-94-017-5126-1
isbn_ebook978-1-4020-2841-0
copyrightSpringer Science+Business Media Dordrecht 2004
The information of publication is updating

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沙發(fā)
發(fā)表于 2025-3-21 22:19:44 | 只看該作者
https://doi.org/10.1007/978-1-4020-2841-0EDS spectra; electron microprobe; rock forming minerals; electron microscopy; mineral; mineralogy; economi
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發(fā)表于 2025-3-22 02:34:17 | 只看該作者
978-94-017-5126-1Springer Science+Business Media Dordrecht 2004
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Modeling of Shallow Foundation Dynamics present. The height of each peak from a single element will be present in approximately the ratios listed in Table 2.1. If the beam energy is sufficient, look for K lines in addition to the lower energy L lines, or L lines in addition to the M lines. As an example, the gold Mα peak at 2.123 keV is
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Functioning of the Soil System,. In cases where the mineral is a member of a solid solution series the spectrum is labeled as being ‘end member rich,’ e.g. Pyrope rich Garnet (page 49) although the end member formula is given. The microscopist can estimate the approximate pyrope percentage based on relative Mg, Ca, and Fe peak he
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Energy Dispersive Spectrometry of Common Rock Forming Minerals
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Energy Dispersive Spectrometry of Common Rock Forming Minerals978-1-4020-2841-0
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Formation, Degradation, and Mapping,lo electron-volts (keV), and it can produce that spectrum from a micron-sized sample that has had only minimal preparation. Modern software makes interpreting the spectra fairly simple and investigators can obtain a qualitative, or even semiquantitative elemental analysis of their sample in short or
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