TEXTURES OF ORTHOPYROXENITES FROM THE BURGERSFORT BULGE OF THE EASTERN BUSHVELD COMPLEX, REPUBLIC OF SOUTH AFRICA
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dc.contributor.author | Williams E. | |
dc.contributor.author | Boudreau A.E. | |
dc.contributor.author | Boorman S. | |
dc.contributor.author | Kruger F.J. | |
dc.date.accessioned | 2024-10-19T07:54:32Z | |
dc.date.available | 2024-10-19T07:54:32Z | |
dc.date.issued | 2006 | |
dc.identifier | https://www.elibrary.ru/item.asp?id=51187530 | |
dc.identifier.citation | Contributions to Mineralogy and Petrology, 2006, 151, 4, 480-492 | |
dc.identifier.issn | 0010-7999 | |
dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/46011 | |
dc.description.abstract | A suite of 30 samples was collected from the Burgersfort bulge area of the eastern Bushveld Complex for a detailed quantitative textural study. The studied section represents a stratigraphic column approximately 1,000 m thick, of mainly orthopyroxenites from the lower zone (LZ) and lower critical zone. Crystal size distribution (CSD) plots and quantitative fabric analyses reveal a history of crystal aging and compaction, as evident from the loss of smaller-sized crystals and the development of foliation with little evidence of mineral lineation. Compared with the thicker section from Jagdlust (~80 km north), the LZ orthopyroxenites at Burgersfort are consistently finer grained. Foliation is equally well developed at both locations and is consistent with a relatively thin compaction zone at the top of the mush column. Grain size is largely a function of local cooling history with a grain size growth exponent estimated to be between 2.0 and 3.4. | |
dc.subject | BUSHVELD COMPLEX | |
dc.subject | IGNEOUS TEXTURES | |
dc.subject | IGNEOUS COMPACTION | |
dc.title | TEXTURES OF ORTHOPYROXENITES FROM THE BURGERSFORT BULGE OF THE EASTERN BUSHVELD COMPLEX, REPUBLIC OF SOUTH AFRICA | |
dc.type | Статья | |
dc.identifier.doi | 10.1007/s00410-006-0072-9 |
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