Regional Metamorphism
Regional metamorphism is a geological process that occurs over large areas typically associated with tectonic plate collisions or mountain-building events. It involves high pressures and temperatures, altering the mineralogy, texture, and structure of rocks. Commonly found in regions with significant crustal deformation, such as convergent plate boundaries or collision zones, regional metamorphism can create rocks like schist, gneiss, and marble from pre-existing sedimentary, igneous, or metamorphic rocks. This process can also cause the alignment of minerals into foliation, reflecting the directional pressure during metamorphism. Regional metamorphism provides valuable insights into Earth's tectonic history and the processes shaping its 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