Abstract
The Mesohellenic Trough is a 130 km long and about 30 km wide subsiding area which contains a thick sequence of well exposed Late Cenozoic post-orogenic sediments. This intermontane basin, located at the contact between the Apulian and Pelagonian collided margins, provides a good example of the characteristics needed to study the chronology of late orogenic intracontinental structures.
Cite
CITATION STYLE
Doutsos, T., Koukouvelas, I., Zelilidas, A., & Kontopoulos, N. (1994). Intracontinental wedging and post-orogenic collapse in the Mesohellenic Trough. In Active Continental Margins — Present and Past (pp. 257–275). Springer Berlin Heidelberg. https://doi.org/10.1007/978-3-662-38521-0_5
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