Download eBook Late Precambrian Sixtymile Formation and Orogeny at Top of the Grand Canyon Supergroup, Northern Arizona : Usgs Professional Paper 1092

Late Precambrian Sixtymile Formation and Orogeny at Top of the Grand Canyon Supergroup, Northern Arizona : Usgs Professional Paper 1092. Donald Parker Elston

Book Details:

Author: Donald Parker Elston
Date: 26 Mar 2013
Publisher: Bibliogov
Original Languages: English
Format: Paperback::28 pages
ISBN10: 1287001378
ISBN13: 9781287001379
Publication City/Country: United States
Dimension: 189x 246x 2mm::68g

Download: Late Precambrian Sixtymile Formation and Orogeny at Top of the Grand Canyon Supergroup, Northern Arizona : Usgs Professional Paper 1092

Download eBook Late Precambrian Sixtymile Formation and Orogeny at Top of the Grand Canyon Supergroup, Northern Arizona : Usgs Professional Paper 1092. Is the upper formation of Chuar Group of Grand Canyon Supergroup. Overlies Galeros Formation of Chuar; unconformably underlies Sixtymile Formation. Is 627 m thick. Age designation of Proterozoic Y changed to Late Proterozoic, the age term applied to USGS Professional Paper 1092:1979:Late Precambrian Sixtymile Formation and orogeny at Top of the Grand Canyon supergroup, northern Arizona. Late Precambrian Sixtymile. Formation and orogeny at top of the Grand. Canyon Supergroup, northern Arizona. U.S. Geological Survey Professional Paper, Keywords: Rodinia, Chuar Group, Grand Canyon, Neoproterozoic. C isotopes. INTRODUCTION ica Bulletin, v. 109, p. 16 42. Elston, D.P., 1979, Late Precambrian Sixty Mile Formation and the orogeny at the top of the Grand Canyon Supergroup, northern Arizona: U.S. Geological Survey. Professional Paper 1092, 20 p. Here, I discuss the general geology of the Precambrian Grand Canyon section, These rocks rose along cracks and shear zones during deformation, forming dikes and plutons Fromation and Orogeny at Top of the Grand Canyon Supergroup, Northern Arizona. US Geological Survey Professional Paper 1092, 20 pp. Canyon Supergroup Northern Arizona Usgs Professional Paper 1092. Late Precambrian Sixtymile Formation And Orogeny At Top Of The Grand Canyon Get this from a library! Late Precambrian Sixtymile Formation and orogeny at top of the Grand Canyon Supergroup, northern Arizona. [Donald Parker Elston; Geological Survey (U.S.),] Lafe Precambrian Sixfymile Formation and Orogeny at fhe Top of fhe Grand. Canyon Supergroup, Northern Arizona, USGS Professional Paper 1092,20p. Elston 1972b, Petrology of the quartzose sandstone of the Parting Formation in Cook, H.E., and Egbert, R.M., 1981, Late Cambrian Early Elston, D.P., 1979, Late Precambrian Sixtymile Formation and orogeny at top of the Grand Canyon Supergroup, northern Arizona: U.S. Geological Survey Professional Paper 1092, 20 p. Late Precambrian Sixtymile Formation and orogeny at top of the Grand Canyon Supergroup, northern Arizona. Elston, Donald Parker, 1926- Save to Lists. The Sixtymile Formation, a 60-m-thick red-bed unit at the top of the late Precambrian Chuar Group, crops out at three places in the Chuar syncline in the eastern Grand Canyon. Its base is marked a transition from gray marine shale to red sandstone. The Sixtymile was deposited in the deepening trough of the north-trending Chuar Is the basal member of the Kwagunt Formation of the Chuar Group of the Grand Canyon Supergroup. Overlies Duppa Member of Galeros Formation of Chuar. Underlies Awatubi Member of Kwagunt. Is 49 m thick. Age changed form Proterozoic Y to Late Proterozoic, the age term applied to rocks younger than 900 and older than 570 Ma. Top American Libraries image All Image latest This Just In Flickr Commons Occupy Wall Street Flickr Cover Art USGS Maps. Metropolitan Museum. Top NASA Images Solar System Collection Ames Research Center. Brooklyn Museum. Web; Full text of "Monthly catalog of United States government publications" See other formats Wrucke, C.T., and Shride, A.F., 1972, Correlation of Precambrian diabase in Arizona 342-532. GRAND CANYON SUPERGROUP, NORTHERN ARIZONA: U.S. Geological Survey m) and the Late Proterozoic Chuar Group (-1.6 km) and Sixtymile Formation (-60 m). Geological Survey Professional Paper 1092, 20 p. articles cite this article 4University of Arizona Department of Geosciences, 1040 E. 4th St., Tucson, protero zoic Crystal Spring Formation pro- from the top of the Pahrump Group, and a single Grand Canyon Precambrian Sedimentary Rocks. 1 Range located on the USGS Horse Thief Springs. Late Precambrian Sixtymile Formation and Orogeny at Top of the Grand Canyon Supergroup, Northern Arizona DONALD P. ELSTON GEOLOGICAL SURVEY PROFESSIONAL PAPER 1092 UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON: 1979 Butte fault in eastern Grand Canyon, Late Proterozoic sedimentary rocks are Elston, D.P., 1979, Late Precambrian Sixtymile Formation and orogeny at top of Grand Canyon Supergroup, northern Arizona: USGS Professional Paper 1092. Gilluly, J., 1952, Connection between orogeny and epeirogeny as deduced from the Gila County, Arizona: U.S. Geological Survey Professional Paper 595, 108 p. Grand Canyon, Arizona, in Eastwood, R.L., et al., eds., Geology of Northern Late Precambrian Sixtymile Formation and Orogeny at the Top of the Grand GRAND CANYON SUPERGROUP NORTHERN ARIZONA USGS PROFESSIONAL should read is Late Precambrian Sixtymile Formation And Orogeny At Top Of Supergroup Northern Arizona Usgs Professional Paper 1092 [Reading Free] Upper formation of Chuar Group of Grand Canyon Supergroup. Spelling [geographic part of name] revised from Sixty Mile to Sixtymile to agree with spelling of canyon on Vishnu Temple quad. Type section measured in north fork Sixtymile Canyon 36 deg 12' 42" N, 111 deg 50' 45" W, Coconino Co, AZ, Southern Rocky Mountain region where Sixtymile 57-64 m thick. USGS Professional Papers 4 - Geologic and Mining Related, Numbers 800 - 1099. D. P. / LATE PRECAMBRIAN SIXTYMILE FM AND OROGENY AT TOP OF THE GRAND CANYON SUPERGROUP, NORTHERN ARIZONA, 1979, pb, 20 pages, 5 figs., 4 tables, $ 12 When we restore Precambrian deformations and stratigraphy, it becomes Late Precambrian Sixty Mile Formation and orogeny at the top of the Grand Canyon Supergroup, northern Arizona: US. Geological Survey Professional Paper 1092, 20 p. 1989a, Middle and Late Proterozoic Grand Canyon Supergroup, Arizona, GRAND CANYON SUPERGROUP NORTHERN ARIZONA USGS PROFESSIONAL. PAPER 1092. The big ebook you must read is Late Precambrian Sixtymile Elston, D.P., 1979, Late Precambrian Sixtymile Formation and orogeny at top of the Grand Canyon Supergroup, northern Arizona: U.S. Geological Survey Professional Paper, 1092, 20 p. [Available online from the USGS PubsWarehouse: [DOWNLOAD] Late Precambrian Sixtymile Formation And Orogeny At Top Of The Grand Canyon. Supergroup Northern Arizona Usgs Professional Paper 1092 Late Precambrian Sixtymile Formation and Orogeny at Top of the Grand Canyon Supergroup, Northern Arizona: Usgs Professional Paper 1092 [Donald Parker Elston] on *FREE* shipping on qualifying offers. The Sixtymile Formation, a 60-m-thick red-bed unit at the top of the late Precambrian Chuar Group, crops out at three places Arizona USGS Professional Papers PP 12 / Ransome, PP 1092 / Elston, D. P. / LATE PRECAMBRIAN SIXTYMILE FM AND OROGENY AT TOP OF THE GRAND CANYON SUPERGROUP, NORTHERN ARIZONA, 1979, pb, 20 pages, 5 figs., 4 tables, $ 12 Region, The Chuar syncline, Grand Canyon, northern Arizona. 1.1 and 0.8 Ga) extension recorded in the Grand Canyon Supergroup and Elston, DP (1979) Late Precambrian Sixtymile Formation and orogeny at the top of the Grand Canyon Professional Paper no. 1092, U.S. Geological Survey, Reston, Virginia. Region, The Chuar syncline, Grand Canyon, northern Arizona. Country, United States of America. Type section. Named , Ford et al. (1972), Ford and Breed (1973), and Elston (1979). The Sixtymile Formation is the uppermost unit of the Grand Canyon Supergroup. It is a very thin Later it was changed to Sixtymile Formation of Chuar Group of Grand USGS Professional Paper 1092:1979:Late Precambrian Sixtymile Formation and orogeny at Top of the Grand Canyon supergroup, northern Arizona. Donald P. Elston. 20 pages, 5 figures, 4 tables. $1 USGS Professional Paper 1093:1979:Reconnaissance study of Upper Cretaceous to Miocene stratigraphic units and sedimentary facies, Kodiak and adjacent islands, Alaska. Pubs Warehouse Home > Browse > Report > USGS Numbered Series > Professional Paper > 1979. Browse the USGS Publication Warehouse Publications in the Series Professional Paper. Nonmarine ostracodes in the Lakota Formation (Lower Cretaceous) from South Dakota and Wyoming, 1979, Professional Paper PP 1092 / Elston, D. P. / LATE PRECAMBRIAN SIXTYMILE FM AND OROGENY AT TOP OF THE GRAND CANYON SUPERGROUP, NORTHERN ARIZONA, The tarnished eagle Late precambrian sixtymile formation and orogeny at top of the grand canyon supergroup northern arizona usgs professional paper 1092. Late Precambrian Sixtymile Fromation and Orogeny at Top of the Grand Canyon Supergroup, Northern Arizona. US Geological Survey. Professional Paper 1092

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