Among the rocks used to produce heat-insulating and acoustic building materials, volcanic water-containing glassy rocks are increasingly being used. A feature of volcanic water-containing glasses is their ability to expand during heat treatment. Besides perlite, other volcanic glasses known by various names also have this special feature: obsidian, pitchstone, vitrophire, and others. The common property of all these rocks, which determines their expanding power, is the content of water in them, being in various forms of linkage. The main role in the process of their pore formation during bloating belongs to water and various gases located in closed pores. Obsidian is expanded at temperatures of 1050...11500C. The lowest average density of 2...
The concentration of dissolved volatile species in silicic pyroclasts, especially that of water, can...
Obsidian Dome is a 550-650 year old, 1.5 by 1.8 km extrusion of high silica rhyolite situated along ...
Obsidian pyroclasts are commonly preserved in the fall deposits of explosive silicic eruptions. Rece...
Obsidian is silicic volcanic glass that has undergone minimal crystallization, and has been document...
Today, the decline in soil fertility progress, therefore, special attention paid to the search for n...
Color poster with text, images, maps, and graphs (Spring 2009)Supervolcano eruptions represent some ...
This thesis contains a detailed investigation of volatiles within subglacially erupted rhyolites fro...
Volcanic eruptions are driven by magma buoyancy caused by volatiles exsolving to form a separate gas...
Structures formed with ground perlite, a natural volcanic glass, activated with NaOH solutions, are ...
The effect of temperature and viscosity on the kinetics of bubble growth was measured for a natural ...
Spatial heterogeneities in the dissolved water content within volcanic glasses are generated by diff...
Obsidian flow emplacement is a complex and understudied aspect of silicic volcanism. Of particular i...
Obsidian pyroclasts are common in deposits from silicic sub-Plinian eruptions and can record pre- an...
The ranges in intensity and style of volcanic eruptions, from highly explosive Plinian eruptions to ...
abstract V14A-07 INVITEDInternational audienceInsight into the formation conditions of obsidian lava...
The concentration of dissolved volatile species in silicic pyroclasts, especially that of water, can...
Obsidian Dome is a 550-650 year old, 1.5 by 1.8 km extrusion of high silica rhyolite situated along ...
Obsidian pyroclasts are commonly preserved in the fall deposits of explosive silicic eruptions. Rece...
Obsidian is silicic volcanic glass that has undergone minimal crystallization, and has been document...
Today, the decline in soil fertility progress, therefore, special attention paid to the search for n...
Color poster with text, images, maps, and graphs (Spring 2009)Supervolcano eruptions represent some ...
This thesis contains a detailed investigation of volatiles within subglacially erupted rhyolites fro...
Volcanic eruptions are driven by magma buoyancy caused by volatiles exsolving to form a separate gas...
Structures formed with ground perlite, a natural volcanic glass, activated with NaOH solutions, are ...
The effect of temperature and viscosity on the kinetics of bubble growth was measured for a natural ...
Spatial heterogeneities in the dissolved water content within volcanic glasses are generated by diff...
Obsidian flow emplacement is a complex and understudied aspect of silicic volcanism. Of particular i...
Obsidian pyroclasts are common in deposits from silicic sub-Plinian eruptions and can record pre- an...
The ranges in intensity and style of volcanic eruptions, from highly explosive Plinian eruptions to ...
abstract V14A-07 INVITEDInternational audienceInsight into the formation conditions of obsidian lava...
The concentration of dissolved volatile species in silicic pyroclasts, especially that of water, can...
Obsidian Dome is a 550-650 year old, 1.5 by 1.8 km extrusion of high silica rhyolite situated along ...
Obsidian pyroclasts are commonly preserved in the fall deposits of explosive silicic eruptions. Rece...