The structural geology of a portion of the Matchless amphibolite belt west of Windhoek select="/dri:document/dri:meta/dri:pageMeta/dri:metadata[@element='title']/node()"/>
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| dc.contributor.author | Ray J. | en_US |
| dc.date.accessioned | 2013-07-02T14:10:28Z | |
| dc.date.available | 2013-07-02T14:10:28Z | |
| dc.date.issued | 1984 | en_US |
| dc.identifier.uri | http://hdl.handle.net/11070.1/4328 | |
| dc.description.abstract | Abstract by author: | en_US |
| dc.description.abstract | This paper describes the results of an investigation into the deformed amphiboles of a small part of the Matchless Member and surrounding Kuiseb schists some 10km west of Windhoek. Four phases of deformation were identified | en_US |
| dc.description.abstract | Pressure solution processes were active during the first phase (Dl) to produce the dominant north-east, south-west trending spaced cleavage (S1). Extreme shortening accompanied this event. Subsequent thrusting produced complex F2-folding patterns, boundinage structures and transposition. Dl and D2 are axial planar. Later D3 crenulations and D4 kinking produced non penetrative structures | en_US |
| dc.format.extent | 46 p | en_US |
| dc.format.extent | ill | en_US |
| dc.format.extent | 29 cm | en_US |
| dc.language.iso | eng | en_US |
| dc.title | The structural geology of a portion of the Matchless amphibolite belt west of Windhoek | en_US |
| dc.type | thesis | en_US |
| dc.identifier.isis | F013-199601110003373 | en_US |
| dc.description.degree | Johannesburg | en_US |
| dc.description.degree | South Africa | en_US |
| dc.description.degree | University of the Witwatersrand | en_US |
| dc.description.degree | B Sc Hons | en_US |
| dc.masterFileNumber | 2652 | en_US |
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