Monogenetic basaltic volcanoes are the most common volcanic landforms on the continents.
They encompass a range of morphologies from small pyroclastic constructs to larger shields …

Neogene to Quaternary volcanic/magmatic activity in the Carpathian-Pannonian Region
(CPR) occurred between 21 and 0.1 Ma with a distinct migration in time from west to east. It …

Plate motion and associated tectonics explain the location of magmatic systems along plate
boundaries [1], however, they cannot give satisfactory explanations of the origin of intra …

ABSTRACT INTRODUCTION that are commonly, but not exclusively, small in eruptive
volume. Monogenetic volcanic fields commonly consist of large numbers of volcanic clusters …

Fragmentation processes in eruptions are commonly contrasted as phreatomagmatic or
magmatic; the latter requires only fragmentation of magma without external intervention, but …

Granitic and mafic magma pulses were sequentially accreted in the spectacularly exposed
shallow crustal Torres del Paine laccolith, in southern Patagonia. This 12.5 Ma pluton forms …

The ease at which exsolving volatiles can migrate though magma and outgas influences the
explosivity of a volcanic eruption. Volcanic rocks often contain discrete discontinuities …

Terra Nova, 23, 70–75, 2011 Abstract Continuous pyroclastic successions from
monogenetic volcanoes in the Jeju Island Volcanic Field (Korea) were targeted for detailed …

Shallow magmatic intrusions are prevalent in volcanic settings worldwide. Understanding
how these intrusions interact and influence their volcanic host rocks is therefore relevant to …

Tecuitlapa Maar, located in the eastern Central Volcanic Belt of Mexico, is a late Quaternary,
100-m-deep,> 1-km-diameter crater with an alignment of scoria cones, building in height to …