Due to the size of its sand dunes, Cape Cod represents an active margin. (Cape Cod is an example of a passive margin rather than an active one.) This statement about active and/or passive margins is not true.
AMFTBs and the Mesozoic/Tertiary basins they are linked with are only found at the active borders of the circum-Pacific and Southeast Asia, and active margin they can be either intra oceanic arcs or continental volcanic arc systems. On the oceanward side of often-still-active arcs or else the inactive batholithic roots of past arcs, forearc basins are found. Behind the arcs are back-arc basins. Peneplaned, occasionally rifted basements that integrate with the protruding igneous rocks of the arc or else underlie them often underlie both basin types. The class of episutural basins, which includes both forearc and back-arc basins, is covered in Chapter 4 of Volume 1A of Roberts and Bally, as well as Tables 27.2 and 27.3 therein.
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