Abstract Large Igneous Provinces (LIPs) can have a significant global climatic effect as
monitored by sedimentary trace and isotopic compositions that record paleo …

Late Mesozoic mafic igneous rocks are widespread across the Arctic region, and are
collectively referred to as the High Arctic Large Igneous Province (HALIP). In Svalbard the …

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 …

We review the numerous experimental studies dedicated to unravelling the physics and
dynamics of various parts of a volcanic plumbing system. Section 1 lists the model materials …

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 …

Understanding the dynamics of continental Large Igneous Provinces (LIPs) relies on precise
dating of basaltic rocks. LIP research has traditionally focused on dating lavas, often …

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 …

Large volumes of greenhouse gases such as CH4 and CO2 form by contact metamorphism
of organic-rich sediments in aureoles around sill intrusions in sedimentary basins …

Quantification of fluid generation during contact metamorphism of shale is important for the
understanding of metamorphic processes, fluid flow in sedimentary basins and perturbations …

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 …