Crustal And Mantle Rheology
Crustal And Mantle Rheology
Crustal and mantle rheology explores the mechanical behavior of Earth's outer and deeper layers, crucial for understanding geological processes. The crust, varying from 5 to 70 km thick beneath continents and oceans, exhibits brittle behavior near the surface, but deeper zones can deform ductilely over time due to heat and pressure. Conversely, the mantle, extending to about 2,900 km deep, undergoes plastic flow due to high temperatures and pressure, influencing tectonic plate movements and volcanic activity. Studying rheology helps geologists model earthquakes, mountain building, and magma generation, vital for comprehending Earth's dynamic evolution and resource formation processes.
Committee Members
Myint Win Bo
Toronto Metropolitan University , Canada
Leonid Anisimov
Volgograd State University, Russian Federation
Shozo Yanagida
Osaka University, Japan Geology 2023 Speakers
Martina Gaglioti
LIPU, Italy
Maria Vicenta Esteller Alberich
Universidad Autónoma del Estado de México, Mexico
Oscar Andres Cuanalo Campos
Universidad Popular Autónoma del Estado de Puebla, Mexico
Arun K Shandilya
Dr HSG University Sagar, India
Title : Geotechnical ground investigation
Myint Win Bo, Toronto Metropolitan University , Canada
Title : Simultaneous Global Climate Change "Heat Waves" and microwave and radio-wave from Solar Flares
Shozo Yanagida, Osaka University, Japan
Title : How subsurface waters record the earth’s history
Leonid Anisimov, Volgograd State University, Russian Federation
Title : Landslides.Rainfall one of the main triggering factors in the mountainous regions of Puebla, Mexico.
Oscar Andres Cuanalo Campos, Universidad Popular Autónoma del Estado de Puebla, Mexico
Title : Geo Education exploratory learning sessions on field and underwater
Martina Gaglioti, LIPU, Italy
Title : Linking between color and element concentration for Fluorite: An optical spectroscopic approach
Ali Almohammed, Pandit Deendayal Energy University, India