High-Temperature Hydrothermal Systems Induced from Shallow-Depth Magma Intrusions in Japan
摘要
Recently, many geothermal wells have encountered consolidated magma intrusions worldwide. These intrusions are likely geothermal heat sources. In this chapter, we consider the genetic relationships between the depth of the high-level magma intrusions and high-temperature hydrothermal systems in Japan, particularly from the viewpoint of the magma intrusion’s buoyancy.