Thermochronology
Thermochronology
Thermochronology is a branch of geochronology that studies the thermal history of rocks and minerals. It involves determining the ages of rocks based on the closure temperature of specific isotopic systems. As rocks cool from high temperatures, radioactive isotopes decay at predictable rates, recording the time since they were last heated. This method helps geologists understand the thermal evolution of geological regions, the timing of tectonic events, and the rates of erosion and exhumation. Techniques such as fission track dating and (U-Th)/He dating are commonly used in thermochronology to reveal the geological processes shaping Earth's crust over millions to billions of years.
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