The magmatic components of continental Large Igneous Provinces (LIPs) include flood
basalts and their plumbing system of giant mafic dyke swarms (radiating, linear, and the …

Many volcanoes are buried within Te Riu-a-Māui/Zealandia sedimentary basins. Based on a
large collection of seismic reflection and drillhole data, this paper outlines the morphology …

Our ability to investigate both the intrusive and extrusive parts of individual volcanoes has
evolved with the increasing quality of seismic reflection datasets. Today, new seismic data …

The Ecuadorian arc is composed of an unusually high number of volcanoes, organized as
along-arc alignments and across-arc clusters, in a relatively small area. Although several …

Abstract Four areas (Loriu, Lojamei, Muranachok-Muruangapoi, Kamutile Hills) of well-
developed Miocene-age dikes in the northern Kenya Rift (Turkana, Kenya) have been …

All existing bench and tunnel vein and fault structural data with identified mineral infill,
acquired in Chuquicamata, were georeferenced, digitized, and, according to their …

In this study, we investigated the extensional tectonics and post-rift magmatism in the
southern South China Sea (SCS) using a newly obtained seismic reflection profile, which …

Structure-magma interactions in rifts, particularly those associated with mantle plumes,
contain examples where structure predominantly controls magmatism and conversely …

The integration of surface observations and sub-surface data (wellbore and seismic) from
the orogenic front of the Malargüe fold-and-thrust belt allows us to study its kinematics and to …

We studied the structure, paleomagnetism, and magnetic fabric of Miocene granitoids
intruded along the left‐lateral, transpressional, Tonalá shear zone in Chiapas, southern …