Abstract Most magmatic Ni–Cu–PGE sulphide deposits occur within long-lived magma
pathways fed by high degree partial melts of the mantle. Holistic mineral-system analysis for …

Magma is transported and stored in the crust mostly through networks of planar structures
(intrusive sheets), ranging from vertical dykes to inclined sheets and horizontal sills, and …

The structure of upper crustal magma plumbing systems controls the distribution of
volcanism and influences tectonic processes. However, delineating the structure and …

The movement of magma through the shallow crust and the impact of subsurface sill
complexes on the hydrocarbon systems of prospective sedimentary basins has long been …

Over the last few decades, significant advances in using geophysical techniques to image
the structure of magma plumbing systems have enabled the identification of zones of melt …

Numerous challenges for petroleum exploration exist within basins containing sequences of
intrusive and extrusive rocks, ranging from seismic imaging to drilling. One poorly …

Tectono-metallogenic systems are geological systems that link geodynamic and tectonic
processes with ore-forming processes. Fundamental geodynamic processes, including …

The interaction between magmatic and extensional processes related to the formation of
rifted margins has been and still is highly debated. The interpretation of magmatic additions …

Emplacement of magma in the shallow subsurface can result in the development of dome-
shaped folds at the Earth's surface. These so-called “forced folds” have been described in …

Application of 3D seismic reflection data to igneous systems in sedimentary basins has led
to a revolution in the understanding of mafic sill complexes. However, there is considerable …