Layered intrusions are fossilized natural laboratories that historically have constrained many
fundamental principles of igneous petrology. Layered intrusions are typically stratiform …

The Dallol volcano and its associated hydrothermal field are located in a remote area of the
northern Danakil Depression in Ethiopia, a region only recently appraised after decades of …

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

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 surface and internal structure of Ceres show evidence of a global process of aqueous
alteration, indicating the existence of an ocean in the past. However, it is not clear whether …

Venus's past climate evolution is uncertain. General circulation model simulations permit a
habitable climate as late as∼ 0.7 Ga, and there is suggestive—albeit inconclusive …

Seismic reflection data and field observations have revealed the presence of voluminous
igneous sill complexes emplaced into organic-rich shale formations in sedimentary basins …

Mafic sills of the Central Atlantic Magmatic Province (CAMP) in Brazil are temporally linked
to the end-Triassic extinction (ETE), one of the largest mass extinctions of the Phanerozoic …

Thick evaporite masses (bedded and halokinetic) dominated by the mineral halite, are
currently mined using conventional solution mining techniques. After excavation, the …

Abstract The central High Atlas (Morocco) constitutes a diapiric province that hosts a
complex array of elongated diapirs and minibasins that formed during the Lower Jurassic rift …