Radioisotope Geochronology
Radioisotope geochronology is a crucial tool in geology and earth sciences, used to determine the age of rocks and geological events. By measuring the decay of radioactive isotopes in minerals, such as uranium-lead or potassium-argon systems, scientists can calculate the absolute ages of rocks and geological formations. This technique helps unravel the timelines of geological processes like mountain building, volcanic eruptions, and the formation of minerals. Radioisotope geochronology provides essential insights into Earth's history, allowing researchers to piece together the sequence of events that have shaped our planet over millions to billions of years. It is foundational in understanding geological processes and their impact on Earth's evolution and environment.
Myint Win Bo
Toronto Metropolitan University , Canada
Leonid Anisimov
Volgograd State University, Russian Federation
Shozo Yanagida
Osaka University, Japan
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