Geoscience and exploration of the Argyle, Bunder, Diavik and Murowa diamond deposits / Геологическое изучение месторождений алмазов Аргайл, Бандер, Диавик и Мурова (Главы 1-17 и 19-20)

Tectonic and Structural Controls on Diamondiferous Kimberlite and Lamproite and Their Bearing on Area Selection for Diamond Exploration

Argyle Deposit

The Discovery of the Argyle Pipe, Western Australia: The World’s First Lamproite-Hosted Diamond Mine

Evaluation of the AK1 Deposit at Argyle Diamond Mine

The Geology of the Argyle (AK1) Diamond Deposit, Western Australia

Nature of the Mantle Beneath the Argyle AK1 Lamproite Pipe: Constraints from Mantle Xenoliths, Diamonds, and Lamproite Geochemistry

Argyle Diamonds: How Subduction Along the Kimberley Craton Edge Generated the World’s Biggest Diamond Deposit

The Unique Nature of Argyle Fancy Diamonds: Internal Structure, Paragenesis, and Reasons for Color

Bunder Deposit

The Bunder Diamond Project, India: Discovery of the Saptarshi Lamproite Pipes

The Bunder Diamond Project, India: Geology, Geochemistry, and Age of the Saptarshi Lamproite Pipes

A Study of Garnet and Chromian Spinel Xenocrysts from the Atri South Ultramafic Intrusion, Bundelkhand Craton, India

Diamonds from the Atri South Pipe, Bunder Lamproite Field, India, and Implications for the Nature of the Underlying Mantle

Diavik Deposit

Exploration History and Discovery of the Diavik Diamond Deposits, Northwest Territories, Canada

Evaluation of the Diavik Diamond Deposit

Geology, Mineral Chemistry, and Structure of the Kimberlites at Diavik Diamond Mine: Indicators of Cluster-Scale Cross-Fertilization, Mantle Provenance, and Pipe Morphology

The Diamondiferous Mantle Root Beneath the Central Slave Craton

Diamonds from the Diavik Mine: From Formation Through Mantle Residence to Emplacement

Murowa Deposit

Discovery of the Murowa Kimberlites, Zimbabwe

Geology, Structure, and Radiometric Age Determination of the Murowa Kimberlites, Zimbabwe

Characteristics and Origin of the Mantle Root Beneath the Murowa Diamond Mine: Implications for Craton and Diamond Formation

Diamonds from the Murowa Kimberlites: Formation Within Extremely Depleted and Metasomatized Zimbabwean Peridotitic Subcontinental Mantle