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

Several correlation methods are used to estimate data and equation-of-state parameters that
permit calculation of standard state thermodynamic properties at high pressures and …

Platinum-group element (PGE) deposits in the Bushveld Complex and other layered
intrusions form when large, incompletely solidified magma chambers undergo central …

The major element composition of plagioclase, pyroxene, olivine, and magnetite, and whole-
rock 87Sr/86Sr data are presented for the uppermost 2· 1 km of the layered mafic rocks …

The Panzhihua intrusion is one of the largest layered intrusions that hosts huge stratiform Fe‐
Ti oxide layers in the central part of the Emeishan large igneous province, SW China. Up to …

Layering is a common feature in mafic and ultramafic layered intrusions and generally
consists of a succession of layers characterized by contrasted mineral modes and/or mineral …

Concentration patterns of platinum-group elements (PGE) in the Lower, Critical and Main
Zones of the Bushveld Complex are modelled by a process of metal collection by …

Abstract The Bushveld Complex, a layered mafic intrusion in South Africa, shows extreme
vertical differentiation in terms of mineral compositions and modal proportions from dunite to …

The platinum-group element (PGE) contents of the upper portions of the Bushveld Complex
were investigated with three questions in mind:(a) In natural systems does magnetite …

The Baima layered intrusion is located in the central part of the Emeishan Large Igneous
Province (ELIP). The N–S striking intrusion is~ 24km long and~ 2km thick and dips to the …