1 edition of Geology of an alpine-type peridotite in the Mount Sorenson area, east-central Alaska found in the catalog.
Geology of an alpine-type peridotite in the Mount Sorenson area, east-central Alaska
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Get this from a library. Geology of an alpine-type peridotite in the Mount Sorenson area, east-central Alaska: a petrologic and structural study of a large ultramafic body in the Yukon-Tanana Upland. [Terry E C Keith; Geological Survey (U.S.),;].
Buy Gelogy of an Alpine-Type Peridotite in the Mount Sorenson Area, East-Central Alaska on FREE SHIPPING on qualified orders. Geology of an alpine-type peridotite in the Mount Sorenson area, east-central Alaska (DLC) (OCoLC) Material Type: Document, Government publication, National government publication, Internet resource: Document Type: Internet Resource, Computer File: All Authors / Contributors: Terry E C Keith; Geological Survey (U.S.).
MS Book and Mineral Company. Geology and Mining History of Alaska I - Federal Publications PP A / Keith, T. C., / GEOLOGY OF AN ALPINE-TYPE PERIDOTITE IN THE MOUNT SORENSON AREA, EAST-CENTRAL ALASKA,pb, 9 pages, 4 figs., 1 table, $ 4. PP A / Keith, T. C., / GEOLOGY OF AN ALPINE-TYPE PERIDOTITE IN THE MOUNT SORENSON AREA, EAST-CENTRAL ALASKA,pb, 9 pages, 4 figs., 1 table, $ 4 PP B / Pomeroy, J.
/ MASS MOVEMENT IN TWO SELECTED AREAS OF WESTERN WASHINGTON COUNTY, PENNSYLVANIA,pb, 17 pages, frontispiece and 14 figs., $ 5. Geology of an Alpine - Type Peridotite in the Mount Sorenson Area, East-Central Alaska (United States Geological Survey Professional Paper A).
Keith, Terry E. C., Helen L. Foster, Robert L. Foster, E. Post and W. Lehmbeck. Home; 06 Geology Soils and Vegetation; 06 Geology Soils and Vegetation.
Ma | Author: Rivdhal Saputra | Category: Magma, Mantle (Geology), Basalt, Rock. In interior and northern Alaska, the Omineca-Selwyn belt consists of large plutons of mid-Cretaceous granite and lesser syenite and granodiorite that occur in an elongate trend that extends from east-central to west-central Alaska, the Seward Peninsula, and St.
Lawrence Island. Introduction. The Himalayan–Tibetan orogen is the youngest and the most spectacular of all the continent–continent collisional belts on the Earth (e.g., Yin and Harrison, ).This extraordinarily large and complex amalgamated belt is considered to have been built through the closure of the Tethys Ocean between two great landmasses: Laurasia in the north and Gondwana to the south since Cited by: Phanerozoic Tectonic Evolution of the Circum-North Pacific By Warren J.
Nokleberg,1 Leonid M. Parfenov,2 James W.H. Monger,3 Ian O. Norton,4 Alexander I. Khanchuk,5 David B. Stone,6 Christopher R. Scotese,7 David W. Scholl,1 and Kazuya Fujita8.
Full text of "Monthly catalog of United States government publications" See other formats. Crustal Cross Sections from the Western North American Cordillera and Elsewhere: Implications for Tectonic and Petrologic Processes Edited by Robert B.
Miller Department of Geology San José State University San José, California USA Arthur W. Snoke Department of Geology and Geophysics Department East University Avenue. This terrane has long been accepted as the last crustal block to be accreted with Eurasia prior to its collision with the northward drifting Indian continent in the Cenozoic.
Thus, the Lhasa terrane is the key for revealing the origin and evolutionary history of the Himalayan–Tibetan orogen.