Synclines
Synclines are geological formations characterized by downward-folding rock layers shaped like a trough or a basin. These structures are part of the broader field of structural geology, where they typically form in compressional tectonic settings. In a syncline, the youngest rock layers are found in the center of the fold, gradually getting older towards the edges. Synclines often occur in association with anticlines, which are upward-folding structures, and together they contribute to the complex patterns of rock deformation seen in folded mountain ranges and other tectonically active regions. Studying synclines is crucial for understanding the geological history of an area, including processes like mountain building, sedimentary deposition, and the deformation of Earth's crust over millions of years.
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