Layered intrusions are fossilized natural laboratories that historically have constrained many
fundamental principles of igneous petrology. Layered intrusions are typically stratiform …

This chapter focuses on S in porphyry-type ore deposits, layered-mafic-intrusion-hosted ore
bodies, and magmatic sulfide deposits. Porphyry-type ore deposits, eg, Bingham Canyon …

The importance of externally derived sulfur in the genesis of sulfide-rich, magmatic Ni-Cu-
(platinum group element [PGE]) deposits remains a key, yet unresolved, issue. Calculations …

Abstract The Bushveld Complex formed by the crystallization of successive injections of
magma, which were sufficiently closely spaced in time that each previous magma had not …

Large igneous provinces (LIPs) represent significant reservoirs of energy and metals that
can either drive or contribute to a variety of metallogenic systems. The relationships between …

Empirical equations to predict the sulfur content of a mafic magma at the time of sulfide
saturation have been developed based on several sets of published experimental data. The …

Abstract The Sept Iles layered intrusion (Quebec, Canada; 564 Ma) is a large plutonic body
with a diameter of 80 km and a thickness of 6 km made up from its base to top of a layered …

In the present paper, we have compiled data on 565 layered and differentiated igneous
intrusions globally, documenting their (i) location,(ii) age,(iii) size,(iv) geotectonic setting,(v) …

Most deposits of platinum group elements (PGE), chromite, and vanadiferous magnetite
occur in mafic intrusions. Several represent some of the most laterally continuous and …

This publication summarizes the results of petrologic studies aimed at the development and
appli-cation of computer models simulating equilibrium and fractional crystallization in …