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https://doi.org/10.1130/0091-7613(2002)030<0955:mctbsi>2.0.co;2
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Cite Journal: Geology |  Publication Date: Jan 1, 2002 |
 Citations: 6 |
In a similar vein to what Dana posited for Hall's geosynclinal theory for the origin of mountain belts—that it presented “a theory for the origin of mountains with the origin of mountains left out” (p. 55, King, 1977)—[Terry et al. (2001)][1] promote the presence of a Cretaceous-Tertiary (K-
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