In this study we compare three pairs of conjugate rifted margins that are often referred to as
archetypes of rift systems. Despite numerous differences, a remarkable first-order structural …

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 …

Abstract The Palaeocene–Eocene Thermal Maximum (PETM) was a global warming event
of 5–6° C around 56 million years ago caused by input of carbon into the ocean and …

Seismic interpretations are, by definition, subjective and often require significant time and
expertise from the interpreter. We are convinced that machine-learning techniques can help …

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

Abstract A 200,000-yr interval of extreme global warming marked the start of the Eocene
epoch about 55 million years ago. Negative carbon-and oxygen-isotope excursions in …

The end of the Permian period is marked by global warming and the biggest known mass
extinction on Earth. The crisis is commonly attributed to the formation of the Siberian Traps …

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 …

The climate change in the Toarcian (Early Jurassic) was characterized by a major
perturbation of the global carbon cycle. The event lasted for approximately 200,000 years …