Includes bibliographical references.Eighteen Jurassic to Cretaceous South African kimberlites representative of group 1, group 11 and transitional varieties that have been emplaced through both the Archean Kaapvall craton (on-craton) and Proterozoic Namaqua-Natal belt (off-craton), have been selected for a comparative study aimed at characterising their geochemistry and source region compositions, as well as understanding the petrogenetic processes that have affected them. The petrography of the analysed kimberlites is similar to typical group 1 and group 11 kimberlites, characterised by deformed and anhedrarl olivine and phlogopite macrocrysts, with more subhedral to euhedral olivine and phlogopite phenocrysts and microphenocrysts, set in ...
There are more than 1000 known kimberlite occurrences scattered throughout southern Africa. These ki...
Bibliography: leaves 139-146.The Swartruggens (156 Ma) and Star (128 Ma) kimberlites are two Group I...
The petrology and geochemistry of some new occurrences of Mesoproterozoic diamondiferous hypabyssal-...
A research project submitted to the Faculty of Science, University of the Witwatersrand, Johannesbu...
We have carried out a mineralogical and geochemical study on two previously uncharacterized kimberli...
The petrogenesis of kimberlites is commonly obscured by interaction with hydrothermal fluids, includ...
The Du Toitspan kimberlite pipe located on the outskirts of Kimberley South Africa, is one four Cret...
The petrogenesis of kimberlites is commonly obscured by interaction with hydrothermal fluids, includ...
The petrogenesis of kimberlites is commonly obscured by interaction with hydrothermal fluids, includ...
The petrogenesis of kimberlites is commonly obscured by interaction with hydrothermal fluids, includ...
Olivine is the most abundant phase in kimberlites and is stable throughout most of the crystallizati...
Peridotitic garnet xenocrysts from 33 Group II and 29 Group I kimberlites have been used to map the ...
Olivine is the most abundant phase in kimberlites and is stable throughout most of the crystallizati...
The petrogenetic relationships of the different varieties of kimberlite in the De Beers Mine and Let...
Olivine is the most abundant phase in kimberlites and is stable throughout most of the crystallizati...
There are more than 1000 known kimberlite occurrences scattered throughout southern Africa. These ki...
Bibliography: leaves 139-146.The Swartruggens (156 Ma) and Star (128 Ma) kimberlites are two Group I...
The petrology and geochemistry of some new occurrences of Mesoproterozoic diamondiferous hypabyssal-...
A research project submitted to the Faculty of Science, University of the Witwatersrand, Johannesbu...
We have carried out a mineralogical and geochemical study on two previously uncharacterized kimberli...
The petrogenesis of kimberlites is commonly obscured by interaction with hydrothermal fluids, includ...
The Du Toitspan kimberlite pipe located on the outskirts of Kimberley South Africa, is one four Cret...
The petrogenesis of kimberlites is commonly obscured by interaction with hydrothermal fluids, includ...
The petrogenesis of kimberlites is commonly obscured by interaction with hydrothermal fluids, includ...
The petrogenesis of kimberlites is commonly obscured by interaction with hydrothermal fluids, includ...
Olivine is the most abundant phase in kimberlites and is stable throughout most of the crystallizati...
Peridotitic garnet xenocrysts from 33 Group II and 29 Group I kimberlites have been used to map the ...
Olivine is the most abundant phase in kimberlites and is stable throughout most of the crystallizati...
The petrogenetic relationships of the different varieties of kimberlite in the De Beers Mine and Let...
Olivine is the most abundant phase in kimberlites and is stable throughout most of the crystallizati...
There are more than 1000 known kimberlite occurrences scattered throughout southern Africa. These ki...
Bibliography: leaves 139-146.The Swartruggens (156 Ma) and Star (128 Ma) kimberlites are two Group I...
The petrology and geochemistry of some new occurrences of Mesoproterozoic diamondiferous hypabyssal-...