Chronostratigraphy is a branch of geology that involves the study and correlation of rock layers (strata) based on their age or time relationships. It aims to establish a chronological framework for Earth's history by dividing geological time into distinct units called chronostratigraphic units. These units are defined based on the presence of specific fossils, rock types, or other markers that reflect particular intervals of time. Chronostratigraphic units range from the smallest, such as beds and formations, to larger units like periods and eras. This discipline is crucial for understanding the sequence of events in Earth's geological past and is essential for tasks ranging from dating rock sequences to reconstructing ancient environments and climates.
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