Seitenhistorie

 Mongolia

| !mong_scen_1500.jpg|thumbnail! | | !mong_dune_macro_1400.jpg|thumbnail! |
| _replace this with the caption to image above_ \\
{table-cell:width=30%}
{table-cell} | Glass bead is 200 µ in diameter |

| *Location:* \\ | Zuun mod Elstei, 50 km east of Ulaanbaatar, Mongolia; E 107°28'55.1"; N 47°47'27.5"

 |
| *Depositional facies:* \\ | _replace this with text about the dep facies_ |
| *Provenance:* \\ | Mix of (1) granitoid plutonic rocks and (2) low-medium-grade metasedimentary (schist, marble) and possibly metavolcanic

 rocks |
| *Composition:* \\ | Mix of translucent - transparent quartz with pink feldspar, white marble and grey-green low-grade metamorphic rocks (schists); possibly also higher-grade metamorphic rocks involved.

 Few heavy minerals, including

 garnets |
| *Texture:* | Characteristic eolian texture: Medium grained (mL-MU; mean ca. 350 µ), well sorted, depending on mineralogy poorly to well rounded. Characteristic polished, matted ("frosted") grain surfaces typical of eolian transport

 |
h6. Petrographic thin section:
| *Description:* | _insert here short description of thin section_ |

| _insert here a bright field image_ | _insert here short description of thin section_ | _insert here a dark field image_ |
| Bright field | | Dark field |

| *Sample number* | heubeck0142 |
| *Collector* | Dr. Ochirbat Batkhishig, Institute of Geography, Mongolian Academy of Sciences, Mongolia | 
| *Date of sampling* | January, 2008 |

h6. Comments:

Characteristic eolian texture: Medium grained (mL-MU; mean ca. 350 µ), well sorted, depending on mineralogy poorly to well rounded. Characteristic polished, matted ("frosted") grain surfaces typical of eolian transport


_replace this text with link to daughter page with additional data_





.