Diamond is not a common rock-forming mineral (an exception being “diamondite”; see
Jacob and Mikhail 2022, this volume) nor a common crustal mineral (the exceptions being …

Abstract The Central Mediterranean region is one of the most important areas on Earth for
studying subduction-related potassic and ultrapotassic magmatism, derived from partial …

IGNEOUS ROCKS AND PROCESSES A practical introduction to igneous petrology for
students and practitioners The newly revised Second Edition of Igneous Rocks and …

Major and trace element, Sr–Nd–Pb–O isotope and mineral chemical data are presented for
post-collisional ultrapotassic, silicic potassic and high-K calc-alkaline volcanic rocks from …

This remarkable volume presents the first revision to the classification system of diamond-
bearing rocks in over eighty years. Presenting the latest mineralogical data, this book offers …

Written for students and professionals, this revised textbook surveys the mineral industry
from geological, environmental and economic perspectives. Thoroughly updated, the text …

The association of hotspots and flood basalts has long been recognized [eg, Morgan, 1971].
Fluid-dynamic models [eg, Griffiths, 1986; Griffiths and Campbell, 1990] have produced a …

High-Mg ultrapotassic volcanic rock occurrences of lamproitic affinity are exposed in
southwestern Anatolia, mostly within the Menderes Massif. From north to south the lamproitic …

Numerous dykes of ultramafic lamprophyre (aillikite, mela-aillikite, damtjernite) and
subordinate dolomite-bearing carbonatite with U–Pb perovskite emplacement ages of∼ 590 …

Cenozoic magmatic belt of central Iran originated as a continental arc in the early
Paleogene due to northeastward subduction of the Neo-Tethys lithosphere. In the Shahr e …