Tectonically-driven underfilled–overfilled cycles, the middle Cretaceous in the northern Cordilleran foreland basin

It is shown that the middle Cretaceous succession in the northern Cordilleran foreland basin consists of several-million-year tectonically-driven cycles comprising two components: strata deposited in an underfilled basin with a prominent forebulge zone and strata deposited in an overfilled basin lac...

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Veröffentlicht in:	Sedimentary geology 2011-01, Vol.233 (1), p.15-27
1. Verfasser:	Yang, Yongtai
Format:	Artikel
Sprache:	eng
Schlagworte:	Basins Cordillera Deposition Erosion Foreland basin Middle Cretaceous Migration Mountains Overfilled Sediments Strata Subsidence Tectonic cycle Underfilled
Online-Zugang:	Volltext
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