Dating Kimberlites: Methods and Emplacement Patterns Through Time

Diamond Exploration and Resource Evaluation of Kimberlites

Features of radioactive element distribution within the Arkhangelsk diamondiferous province: possible directions for development of isotope–radiogeochemical methods for kimberlite prospecting in complex landscape–geology and climate conditions of the subarctic zone

Kimberlite magmatism induced by west-dipping subduction of the North American plate

‘Premier’ evidence for prolonged kimberlite pipe formation and its influence on diamond transport from deep Earth

Competence and lithostratigraphy of host rocks govern kimberlite pipe morphology

After-coal diamonds: an enigmatic type of impact diamonds

Tracking sources of selected diamonds from Southern Africa based on carbon isotopic and chemical impurities

Inversion of airborne geophysics over the DO-27/DO-18 kimberlites — Part 3: Induced polarization

Inversion of airborne geophysics over the DO-27/DO-18 kimberlites — Part 1: Potential fields

Majorite-indicative ultradeep (>300 km) xenoliths with spinel associations from the Jagersfontein kimberlite, South Africa.

Early Permian diamond-bearing proximal eskers in the Lichtenburg/Ventersdorp area of the North West Province, South Africa

Parentage of Archean basement within a Paleoproterozoic orogen and implications for on-craton diamond preservation: Slave craton and Wopmay orogen, northwest Canada

3D magnetization inversion using fuzzy c -means clustering with application to geology differentiation

Using Microdiamonds in Kimberlite Diamond Grade Prediction: A Case Study of the Variability in Diamond Population Characteristics Across the Size Range 0.2 to 3.4 mm in Misery Kimberlite, Ekati Mine, NWT, Canada

Phase relations on the K 2 CO 3 -CaCO 3 -MgCO 3 join at 6 GPa and 900–1400 °C: Implications for incipient melting in carbonated mantle domains

Characterizing Kimberlite Dilution by Crustal Rocks at the Snap Lake Diamond Mine (Northwest Territories, Canada) using SWIR (1.90–2.36 μ m) and LWIR (8.1–11.1 μ m) Hyperspectral Imagery Collected from Drill Core