Small-scale volcanic systems are the most widespread type of volcanism on Earth and occur
in all of the main tectonic settings. Most commonly, these systems erupt basaltic magmas …

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 …

Monogenetic volcanism produces small-volume volcanoes with a wide range of eruptive
styles, lithological features and geomorphic architectures. They are classified as spatter …

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 …

Monogenetic basaltic volcanism is characterised by a complex array of behaviours in the
spatial distribution of magma output and also temporal variability in magma flux and eruptive …

Monogenetic basaltic volcanism is characterised by a complex array of eruptive behaviours,
reflecting spatial and temporal variability of the magmatic properties (eg composition …

Small scale basaltic magmatic systems occur in all of the major tectonic environments of
planet Earth and are characteristically expressed at the Earth's surface as fields of small …

요 약이 연구는 2001 년부터 제주도 해발 600 m 이하 지역에서 시행된 100 여공의 시추공 지질
주상도 해석, 78 개시추공에서 획득된 686 개의 시추 코어와 74 개의 화산암류 노두 시료의 …

Monogenetic volcanic fields are commonly related to rifts and/or intraplate tectonic settings.
However, they are also less commonly recognised in subduction zones, including both front …

Abstract “Volcanic field” is a term commonly used to loosely describe a group of volcanoes.
Often, it is implicitly assumed that the volcanoes on a volcanic field are small, monogenetic …