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 …

An existing magma chamber is normally a necessary condition for the generation of a large
volcanic edifice. Most magma chambers form through repeated magma injections …

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 …

Igneous intrusions feature in many sedimentary basins where hydrocarbon exploration and
production is continuing. Owing to distinct geophysical property contrasts with siliciclastic …

The Vietnamese margin forms a key region to the understanding of escape tectonics and the
development of the South China Sea (SCS). The existing geological reconstructions of the …

Polygonal fault systems (PFS) are widely developed along many continental margin basins
and some interior cratonic and foreland basins. They are networks of small normal faults that …

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 …

Temporal and spatial changes in volcano morphology and internal architecture can
determine eruption style and location. However, the relationship between the external and …