Early evolution of an extensional monocline by a propagating normal fault: 3D analysis from combined field study and numerical modeling

The Nopolo structure is located along the eastern margin of the Baja California peninsula and formed during the early stages (12–6 Ma) of development of the Gulf of California. The Nopolo structure is an ∼15-km-long series of two NW-striking, extensional monoclines produced by the upward propagation...

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Veröffentlicht in:	Journal of structural geology 2002-01, Vol.24 (4), p.651-669
Hauptverfasser:	Willsey, Shawn P, Umhoefer, Paul J, Hilley, George E
Format:	Artikel
Sprache:	eng
Schlagworte:	Extensional monocline Normal fault Upward propagation
Online-Zugang:	Volltext
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