Abstract The Wudalianchi Volcano Field (WDF) is a typical intraplate volcano in northeast
China with generation mechanism not yet well understood. As its last eruption was around …

Abstract The Central Andes is a key global location to study the enigmatic relation between
volcanism and plutonism because it has been the site of large ignimbrite-forming eruptions …

Abstract The Central Andes are unique in the global system of subduction zones in that a
significant, high-altitude plateau has formed above a subduction zone. In this region, both …

The Yanggao geothermal field, located in the north of the Datong Basin, and close to the
Datong Volcanic Group, the geothermal field is affected by deep faults and vigorous tectonic …

Abstract The Kusatsu-Shirane volcano is a Quaternary andesitic-to-dacitic active volcano
located on the central Honshu Arc. The volcano is known to have had repeated phreatic …

In active volcanic arcs such as the Andean volcanic mountain belt, magmatically sourced
fluids are channeled through the brittle crust by faults and fracture networks. In the Andes …

The relationship between subduction in convergent margins, crustal structures and
magmatism is crucial to understand processes such as the type and frequency of volcanic …

Abstract The Main Ethiopian Rift is part of the East African Rift with its unique geological
setting as an active continental breakup zone. The Main Ethiopian Rift includes a number of …

Preferential fluid pathways along regional fault systems are crucial for the spatial localization
of volcanic and geothermal manifestations. Differences in electric properties of fluids and …

One of the major problems in the volcanic surveillance is how data from several techniques
can be correlated and used to discriminate between possible precursors of volcanic …