Antiforms
Antiforms are geological structures characterized by an upward convex shape, typically found in folded rock formations. They are part of the broader category of anticlines, where layers of rock fold upwards into an arch-like structure. Antiforms often result from compressional forces in the Earth's crust, such as those occurring during tectonic plate collisions or mountain-building processes. These structures are crucial in understanding the deformation history of a region, as they can indicate the direction and intensity of past geological forces. Geologists study antiforms to decipher the complex processes that have shaped the Earth's crust over millions of years, providing insights into the evolution of landscapes and the distribution of natural resources such as oil and gas deposits.
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