"In this well-illustrated book, Hildebrand expands upon his model for the development of the North American Cordillera detailed in Special paper 457. Starting with an overview of Cordilleran geology he goes on to provide an in depth look at how the Rubian ribbon continent was assembled. He integrates the complex geology of the Cordillera into an actualistic model involving arc magmatism, arc-continent collision, slab failure magmatism, and transcurrent motion in both Rubia and the western North American margin. While much of the focus is on the assembly of the Rubian ribbon continent, Hildebrand explores its interactions with North America during the Sevier and Laramide events and concludes that North America was the lower plate in both"--Provided by publisher.
Ramos-Velázquez, E., Calmus, T., Valencia, V., Iriondo, A., Valencia-Moreno, M., and Bellon, H., 2008, ... R.P., Shimizu, N., Norman, M.D., and Applegate, G.S., 1999, Reaction between slab-derived melts and peridotite in the mantle ...
Hamilton, W., 1969, Reconnaissance geologic map of the Riggins quadrangle, west-central Idaho: U.S. Geological Survey, ... Lund, K., 2004, Geology of the Payette National Forest and Vicinity, WestCentral Idaho: U.S. Geological Survey ...
86, no. B11, p. 10,365–10,386, https:// doi.org/10.1029/JB086iB11p10365. Bickford, M., Van, W., and Zietz, I., 1986, Proterozoic history of the midcontinent region of North America: Geology, v. 14, no. 6, p.
This book discusses not only the important geologic features of each region in California, but also the complex geologic four-dimensional puzzle of how California was assembled, beginning over 2 billion years ago.
Within the Sonora segment to the south, break-off magmatism was also prevalent. Both the Canadian and Sonoran segments have abundant porphyry copper mineralization temporally and spatially associated with the break-off...
Geological Society America, Field Guide 4, pp.1–55. Snavely, P.D., 1987. Tertiary geologic framework, neotectonics, and petroleum potential of the Oregon-Washington continental margin. In: Scholl, D.W., Grantz, A., and Vedder, J.G., ...
Steep crustal-scale faults, having their origins in the Late Archean and Early Proterozoic and trending NE-SW, which define the fundamental block lithospheric structure of the North American craton, are seen...
This volume pre-sents the state of knowledge of the physical geography and geology of this unglaciated region in the otherwise-glaciated Midwest with contributions written by Knox prior to his passing in 2012 and by numerous of his for-mer ...
The papers in this volume are an impressive tribute to the depth and breadth of Bill Dickinson's contributions to the geosciences.
(a) Dark redbeds and lighter eolian sandstones comprise the Cutler Group in Southeastern Utah along upper Glen Canyon. The uppermost Permian sandstone forms the bench atop the foreground mesa at right. In the background, Triassic and ...