Eine Milliarde Jahre geologischer Entwicklung am NW-Rand des Kalahari Kratons select="/dri:document/dri:meta/dri:pageMeta/dri:metadata[@element='title']/node()"/>
DSpace Repository
JavaScript is disabled for your browser. Some features of this site may not work without it.
| dc.contributor.advisor | Weber K | en_US |
| dc.contributor.advisor | Hansen BT | en_US |
| dc.contributor.author | Nagel Rudolf | en_US |
| dc.date.accessioned | 2013-07-02T14:10:35Z | |
| dc.date.available | 2013-07-02T14:10:35Z | |
| dc.date.issued | 1999 | en_US |
| dc.identifier.uri | http://hdl.handle.net/11070.1/4388 | |
| dc.description.abstract | English abstract provided by author: | en_US |
| dc.description.abstract | Finally, the Hartelust ignimbrite represents the youngest volcanic phase (609+8-15Ma, zircon age) of the Khomas trough. From the stratigraphic classification of the Hartelust ignimbrite to the base of the Kuiseb formation it is apparent that the Matchless Member of the Damara sequence must be seen as being older than the Kuiseb formation | en_US |
| dc.language.iso | ger | en_US |
| dc.subject | Geology | en_US |
| dc.subject | Tectonics | en_US |
| dc.subject | Geochronology | en_US |
| dc.title | Eine Milliarde Jahre geologischer Entwicklung am NW-Rand des Kalahari Kratons | en_US |
| dc.type | thesis | en_US |
| dc.identifier.isis | F004-199299999999999 | en_US |
| dc.description.degree | Göttingen | en_US |
| dc.description.degree | Germany | en_US |
| dc.description.degree | Georg-August Universität | en_US |
| dc.description.degree | Ph D | en_US |
| dc.masterFileNumber | 2708 | en_US |
Files in this item
| Files | Size | Format | View |
|---|---|---|---|
|
There are no files associated with this item. |
|||