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geosynclinal volcanism

Geosyncline — In geology, geosyncline is a term still occasionally used for a subsiding linear trough that was caused by the accumulation of sedimentary rock strata deposited in a basin and subsequently compressed, deformed, and uplifted into a mountain range … Wikipedia
Plate tectonics — The tectonic plates of the world were mapped in the second half of the 20th century … Wikipedia
Andean Geosyncline — Linear trough in the Earth s crust in which rocks were deposited in South America in the Mesozoic Era (248–65 million years ago) and Cenozoic Era (65 million years ago to the present). A complex history of volcanism, uplift, block faulting, and… … Universalium
Geology of the North Sea — Contents 1 Tectonic structure 2 Precambrian 3 Finnmarkian, Athollian, Caledonian Orogenies … Wikipedia