Abstract. This paper deals with the kimberlites and diamonds of the Ekati Diamond Mine, NWT, Canada, which lies in the central part of the canadian slave craton and is operated by the BHP Billiton Diamond Inc.. 150 kimberlites were discovered at Ekati and five of them are mined for diamonds. The most Ekati kimberlites are pipe-like bodies and their age range from 45 to 75 Ma. Only a few of the 150 kimberlites are economically useful. For that reason, they need to be drilled and sampled by particular methods. The Ekati property exhibits exceptional diamond grades. Diamonds are formed by carbon – and waterrich melts or by low density fluids. Especially, the diamonds of 13 kimberlites at Ekati were studied. Thereby, three developed regional as...
Kimberlites are a volumetrically minor component of the Earth’s volcanic record, but are very import...
Diamonds have been discovered in a variety of potassic ultramafic rocks including group-I and group-...
Tappert, Ralf; Stachel, Thomas; Harris, Jeffrey W.; Shimizu, Nobumichi; Brey, Gerhard P
A significant new kimberlite province, which hosts more than 150 kimberlite pipes and is centred in ...
This dissertation focuses on mantle compositions and processes. Mineral inclusions in diamonds from ...
Kimberlite was first reported in Saskatchewan in 1988. Subsequently, more kimberlite pipes have been...
Exploration for diamonds in West Greenland has experienced a major boost within the last decade foll...
The paper presents data on petrology, bulk rock and mineral compositions, and textural classificatio...
Analyses of mineral inclusions, carbon isotopes, nitrogen contents and nitrogen aggregation states i...
Diamonds can form in a number of different ways. Physical and chemical properties of diamonds classi...
Bibliography: pages 225-251.The hypabyssal quarry kimberlite is the most abundant phase at Monastery...
Diamonds and their inclusions from the Lace kimberlite (288 crystals ≤ 0.2 ct) are studied in order...
Abstract Kimberlite pipes K11, K91 and K252 in the Buffalo Head Hills, northern Alberta show an unus...
Includes bibliographical references.Eighty-five peridotitic and pyroxenitic xenoliths from the Arnie...
The Late Cretaceous (ca. 100 Ma) diamondiferous Fort a la Corne (FALC) kimberlite field in the Saska...
Kimberlites are a volumetrically minor component of the Earth’s volcanic record, but are very import...
Diamonds have been discovered in a variety of potassic ultramafic rocks including group-I and group-...
Tappert, Ralf; Stachel, Thomas; Harris, Jeffrey W.; Shimizu, Nobumichi; Brey, Gerhard P
A significant new kimberlite province, which hosts more than 150 kimberlite pipes and is centred in ...
This dissertation focuses on mantle compositions and processes. Mineral inclusions in diamonds from ...
Kimberlite was first reported in Saskatchewan in 1988. Subsequently, more kimberlite pipes have been...
Exploration for diamonds in West Greenland has experienced a major boost within the last decade foll...
The paper presents data on petrology, bulk rock and mineral compositions, and textural classificatio...
Analyses of mineral inclusions, carbon isotopes, nitrogen contents and nitrogen aggregation states i...
Diamonds can form in a number of different ways. Physical and chemical properties of diamonds classi...
Bibliography: pages 225-251.The hypabyssal quarry kimberlite is the most abundant phase at Monastery...
Diamonds and their inclusions from the Lace kimberlite (288 crystals ≤ 0.2 ct) are studied in order...
Abstract Kimberlite pipes K11, K91 and K252 in the Buffalo Head Hills, northern Alberta show an unus...
Includes bibliographical references.Eighty-five peridotitic and pyroxenitic xenoliths from the Arnie...
The Late Cretaceous (ca. 100 Ma) diamondiferous Fort a la Corne (FALC) kimberlite field in the Saska...
Kimberlites are a volumetrically minor component of the Earth’s volcanic record, but are very import...
Diamonds have been discovered in a variety of potassic ultramafic rocks including group-I and group-...
Tappert, Ralf; Stachel, Thomas; Harris, Jeffrey W.; Shimizu, Nobumichi; Brey, Gerhard P