Review of explosive hydrovolcanism
Hydrovolcanism is a type of volcanism where magma and water interact either explosively or
non-explosively. The less frequently used term, hydromagmatism, includes all the processes …
non-explosively. The less frequently used term, hydromagmatism, includes all the processes …
Why deep-water eruptions are so different from subaerial eruptions
Magmas erupted in deep-water environments (> 500 m) are subject to physical constraints
very different to those for subaerial eruptions, including hydrostatic pressure, bulk modulus …
very different to those for subaerial eruptions, including hydrostatic pressure, bulk modulus …
Primary volcaniclastic rocks
We propose a classification scheme that unifies terminology for all primary volcaniclastic
deposits, assigns initial depositional mechanism as the basis for classifying them, and …
deposits, assigns initial depositional mechanism as the basis for classifying them, and …
Monogenetic volcanic fields: Origin, sedimentary record, and relationship with polygenetic volcanism
K Németh - What is a volcano, 2010 - books.google.com
ABSTRACT INTRODUCTION that are commonly, but not exclusively, small in eruptive
volume. Monogenetic volcanic fields commonly consist of large numbers of volcanic clusters …
volume. Monogenetic volcanic fields commonly consist of large numbers of volcanic clusters …
Sill morphology and comparison of brittle and non-brittle emplacement mechanisms
Magmatic sheet intrusions contribute significantly to the upper crustal magma transport
network. The emplacement mechanism of the magmatic sheets controls the final geometry of …
network. The emplacement mechanism of the magmatic sheets controls the final geometry of …
Large igneous provinces (LIPs) and metallogeny
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 …
can either drive or contribute to a variety of metallogenic systems. The relationships between …
Root zone processes in the phreatomagmatic pipe emplacement model and consequences for the evolution of maar–diatreme volcanoes
V Lorenz, S Kurszlaukis - Journal of Volcanology and Geothermal …, 2007 - Elsevier
The understanding of processes within the root zone of maar–diatreme volcanoes is
important for the interpretation of the geology, volcanology and even hazard assessment of …
important for the interpretation of the geology, volcanology and even hazard assessment of …
Geometry and controls on the development of igneous sill–related forced folds: A 2-D seismic reflection case study from offshore southern Australia
Emplacement of magma in the shallow subsurface can result in the development of dome-
shaped folds at the Earth's surface. These so-called “forced folds” have been described in …
shaped folds at the Earth's surface. These so-called “forced folds” have been described in …
Experimental modelling of shallow magma emplacement: Application to saucer-shaped intrusions
O Galland, S Planke, ER Neumann… - Earth and Planetary …, 2009 - Elsevier
Saucer-shaped dolerite and sandstone intrusions are common in sedimentary basins world-
wide. We have conducted a series of scaled experiments simulating the process of magma …
wide. We have conducted a series of scaled experiments simulating the process of magma …
Neogene-Quaternary volcanic forms in the Carpathian-Pannonian Region: a review
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 …
(CPR) occurred between 21 and 0.1 Ma with a distinct migration in time from west to east. It …