Paleomagnetic results from the eastern Caliente-Enterprise zone, southwestern Utah: Implications for initiation of a major Miocene transfer zone

Author:

Petronis Michael S.,Holm Daniel K.,Geissman John W.,Hacker David B.,Arnold Billie J.

Publisher

Geological Society of America

Subject

Stratigraphy,Geology

Reference94 articles.

1. Akimoto S. , 1962, Magnetic properties of FeO-FeOa-Ti0 system as a basis of rock magnetism: Journal of the Physical Society of Japan, v. 17, Supplement Bi, p. 706.

2. Alva-Valdivia L.M. Goguitchaichvili A. Urrutia Fucugauchi J. Caballero-Miranda C. Vivallo W. , 2001, Rock magnetism and ore microscopy of the magnetite-apatite ore deposit from Cerro de Mercado, Mexico: Earth, Planets, and Space, v. 53, p. 181–192.

3. Anderson R.E. Mehnert H.H. , 1979, Reinterpretation of the history of the Hurricane fault in Utah, in Newman G.W. Cook H.D. , eds., 1979 Basin and Range Symposium and Great Basin Field Conference: Denver, Colorado, Rocky Mountain Association of Geologists, p. 145–166.

4. Low-Angle (Denudation) Faults, Hinterland of the Sevier Orogenic Belt, Eastern Nevada and Western Utah

5. The Caliente-Enterprise Zone, southeastern Nevada and southwestern Utah

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