Changeset 2255
- Timestamp:
- May 12, 2016 2:29:32 PM (7 years ago)
- Location:
- Tutorials/StackingFaults-II
- Files:
-
- 1 deleted
- 3 edited
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Tutorials/StackingFaults-II/Stacking faults II.htm
r2253 r2255 15 15 <o:Author>Von Dreele</o:Author> 16 16 <o:LastAuthor>Von Dreele</o:LastAuthor> 17 <o:Revision> 3</o:Revision>18 <o:TotalTime> 45</o:TotalTime>17 <o:Revision>5</o:Revision> 18 <o:TotalTime>65</o:TotalTime> 19 19 <o:Created>2016-05-12T18:40:00Z</o:Created> 20 <o:LastSaved>2016-05-12T1 8:55:00Z</o:LastSaved>20 <o:LastSaved>2016-05-12T19:17:00Z</o:LastSaved> 21 21 <o:Pages>1</o:Pages> 22 <o:Words>1 08</o:Words>23 <o:Characters> 622</o:Characters>24 <o:Lines> 5</o:Lines>25 <o:Paragraphs> 1</o:Paragraphs>26 <o:CharactersWithSpaces> 729</o:CharactersWithSpaces>22 <o:Words>154</o:Words> 23 <o:Characters>878</o:Characters> 24 <o:Lines>7</o:Lines> 25 <o:Paragraphs>2</o:Paragraphs> 26 <o:CharactersWithSpaces>1030</o:CharactersWithSpaces> 27 27 <o:Version>15.00</o:Version> 28 28 </o:DocumentProperties> 29 29 </xml><![endif]--> 30 <link rel=dataStoreItem href="Stacking%20faults%20II_files/item00 10.xml"31 target="Stacking%20faults%20II_files/props0 11.xml">30 <link rel=dataStoreItem href="Stacking%20faults%20II_files/item0006.xml" 31 target="Stacking%20faults%20II_files/props007.xml"> 32 32 <link rel=themeData href="Stacking%20faults%20II_files/themedata.thmx"> 33 33 <link rel=colorSchemeMapping … … 1162 1162 class=SpellE>tetrahedra</span> on the other. The layers stack with an offset to 1163 1163 ideally form a triclinic C1 lattice (<span class=SpellE>Bish</span> & Von 1164 Dreele, 1989, Clay & Clay Min. 37, 289-296) for a sample of the most ordered 1165 form of kaolinite from Keokuk, Iowa. Kaolinites from other locations evidently have 1166 stacking faults so that the peaks are displaced, have peculiar shapes and are 1167 above a varying background. For the exercise we provide a laboratory 1168 Bragg-Brentano pattern of Keokuk kaolinite and a less ordered one from Georgia. 1169 </p> 1164 Dreele, 1989, Clay & Clay Min. 37, 289-296) for a sample of the most 1165 ordered form of kaolinite from Keokuk, Iowa. Kaolinites from other locations 1166 evidently have stacking faults so that the peaks are displaced, have peculiar 1167 shapes and are above a varying background. For the exercise we provide a 1168 laboratory Bragg-Brentano pattern of Keokuk kaolinite and a less ordered one 1169 from Washington County, Georgia (Clay Minerals Society Standard KGa-1b) 1170 collected with <span class=SpellE>CuKa</span> radiation on a Bruker instrument 1171 and thus in the Bruker RAW file format. The KGa-1b sample contains a small 1172 amount of <span class=SpellE>anatase</span> (TiO<sub>2</sub>) and the Keokuk 1173 kaolinite has some <span class=SpellE>dickite</span> (different ordered stacking 1174 of kaolinite layers).</p> 1170 1175 1171 1176 </div> -
Tutorials/StackingFaults-II/Stacking faults II_files/filelist.xml
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