Chronostratigraphy is a branch of geology that focuses on the study and correlation of rock layers based on their age. It involves organizing rock strata into units of time called chronostratigraphic units, which include eons, eras, periods, epochs, and ages. These units are defined based on characteristic rock layers and fossil assemblages found globally, allowing geologists to establish a chronological framework for Earth's history. Chronostratigraphy plays a crucial role in understanding the sequence of geological events, the evolution of life forms, and the Earth's dynamic processes over millions of years. By correlating chronostratigraphic units across different regions, geologists can reconstruct past environments and climates, track tectonic movements, and predict the potential distribution of natural resources.
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
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Oscar Andres Cuanalo Campos, Universidad Popular Autónoma del Estado de Puebla, Mexico
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Martina Gaglioti, LIPU, Italy
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Ali Almohammed, Pandit Deendayal Energy University, India