10.2 SEDIMENTARY BASINS CLASSIFIED AND DESCRIBED
489
Fig. 10.17.-- Continued
commonly understood by most geologists, and documented a model with several case
histories. Aubouin's studies, largely based on the Hellenide fold belt of the eastern
Mediterranean, divided troughs into several tectonomorphic zones. A stable foreland
on the craton passes laterally into a shallow trough termed the miogeosynclinal furrow.
489
Fig. 10.17.-- Continued
commonly understood by most geologists, and documented a model with several case
histories. Aubouin's studies, largely based on the Hellenide fold belt of the eastern
Mediterranean, divided troughs into several tectonomorphic zones. A stable foreland
on the craton passes laterally into a shallow trough termed the miogeosynclinal furrow.