Absolute Geochronology
Absolute geochronology is a branch of geology that focuses on determining the precise ages of rocks and geological events in Earth's history. It relies on radiometric dating techniques such as uranium-lead, potassium-argon, and carbon-14 dating to measure the decay of radioactive isotopes within minerals. By analyzing the ratios of parent and daughter isotopes in rocks, geoscientists can calculate the absolute age of formations, volcanic eruptions, or fossil remains. This method provides crucial insights into the timing of geological processes, evolutionary events, and climate changes over millions to billions of years. Absolute geochronology plays a fundamental role in constructing the geological timescale and understanding Earth's past environments and evolutionary trends.
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