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Degassing structures in volcaniclastic kimberlite: Examples from southern African kimberlite pipes
Journal of Volcanology and Geothermal Research, 2008Kimberlite pipes are commonly filled with a distinctive structureless facies termed volcaniclastic kimberlite (previously also termed Tuffisitic Kimberlite Breccia, TKB), which constitutes a thorough mix of both juvenile material and lithic clasts derived from all stratigraphic levels.
Gernon, TM, Sparks, RSJ, Field, M
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The Geophysical Signature Of The Marsfontein Kimberlite Pipe
7th SAGA Biennial Technical Meeting and Exhibition, 2001The M1 kimberlite pipe is located on the farm Marsfontein near Potgietersrus in the Northern province. With a surface area of roughly 0.5ha, this is by no means an insignificant diamond deposit. Over 1.8 million carats were recovered from the start of the project in 1998 to the end of 2000.
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3rd SAGA Biennial Conference and Exhibition, 1993
The primary purpose of this study was to identify geophysical methods that were cheap, quick, readily available for use which would yield an indicative response over a known kimberlite. The following methods were selected for assessment: ground magnetics, self potential, radiometrics, horizontal loop electromagnetic (HLEM), and very low frequency (VLF)
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The primary purpose of this study was to identify geophysical methods that were cheap, quick, readily available for use which would yield an indicative response over a known kimberlite. The following methods were selected for assessment: ground magnetics, self potential, radiometrics, horizontal loop electromagnetic (HLEM), and very low frequency (VLF)
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Improvements in Search Techniques to Detect Kimberlite Pipes
81st EAGE Conference and Exhibition 2019, 2019Summary A review is made of traditional methods that have proven popular in aiding exploration for diamonds. Simple pattern recognition technique can be used to locate kimberlite pipes that have a magnetic response. Gravity tensor gradients have also started to be used.
D. FitzGerald, T. Meyer
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XENOLITHS OF HORNBLENDITES FROM THE UDACHNAYA KIMBERLITE PIPE
Russian Geology and Geophysics, 1995Based on study of structural characteristics of mineralogy and chemistry of hornblendite xenoliths from the Udachnaya Kimberlite Pipe, we have recognized pyroxene, pyroxene-plagioclase, monomineral, and mica varieties. The reaction relationships of amphibole with relict pyroxene suggest metasomatic nature of hornblendites.
A. A. Lunegov, A. I. Kiselev
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Eclogite clinopyroxenes from the kimberlite pipes of Yakutia
Lithos, 1968The kimberlite pipes of Yakutia contain a number of rare xenoliths of deep seated origin (corundum eclogites, grospydites and diamond bearing eclogites). The chemistry of the clinopyroxenes from each of these rock types is distinctive. The pyroxenes of corundum eclogites and grospydites are aluminium rich, while a high Na 2 O content is characteristic ...
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Serpentinization of Olivine in a Kimberlite Pipe Udachnaya
2023V. K. Marshintsev +2 more
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