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A synclinorium is a geological term referring to a large-scale, compound flexure in the Earth's crust that has the shape of an inverted anticlinorium. Essentially, it's a major down-bending or trough-like structure within the Earth's crust. The term "synclinorium" is derived from "syncline," which describes a fold in rock strata that is concave upward. A synclinorium is a more complex version of this, often encompassing multiple smaller folds. The adjective form is "synclinorial," meaning relating to or resembling a synclinorium.123

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