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  • Books  (36)
  • Washington, DC : United States Gov. Print. Off.  (32)
  • Berlin : Akad.-Verl.
  • Berlin [u.a.] : Langenscheidt
  • Cham :Springer International Publishing :
  • 2005-2009  (36)
Collection
  • Books  (36)
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Year
Branch Library
  • 1
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: S 90.0002(1744)
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: VII, 125 S. , Ill., graph. Darst., Kt. , 28 cm
    ISBN: 9781411319455
    Series Statement: U.S. Geological Survey professional paper 1744
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 2
    Call number: S 90.00002(1753
    In: Professional paper
    Description / Table of Contents: The Uncompahgre mining district, part of the Ouray mining district, includes an area of about 15 mi2 on the northwestern flank of the San Juan Mountains in southwestern Colorado from which ores of gold, silver, copper, lead, and zinc have had a gross value of $14 to 15 million.Bedrock within the district ranges in age from Proterozoic to Cenozoic. At least three major uplifts of the ancestral San Juan Mountains occurred during the Proterozoic and at the close of the Paleozoic and Mesozoic, respectively. The last event, known as the Laramide orogeny, locally was accompanied by extensive intrusion of igneous rocks.The principal ore deposits of the district were associated with crosscutting and laccolithic intrusions of porphyritic granodiorite formed during the Laramide orogeny. The ores were deposited chiefly in Paleozoic and Mesozoic sedimentary strata. Ore deposits range from low-grade, contact-metamorphic through pyritic base-metal bodies containing silver and gold tellurides and native gold to silver-bearing lead-zinc deposits.
    Type of Medium: Series available for loan
    Pages: IX, 107 S. + 7 Kt.-Beil. , Ill., graph. Darst., Kt. , 7 Kt.-Beil.
    ISBN: 9781411320857
    Series Statement: U.S. Geological Survey professional paper 1753
    Note: Erscheinungsjahr in Vorlageform:2008
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 3
    Call number: S 90.0002(1761)
    In: Professional paper
    Description / Table of Contents: The southern Española basin consists of a westward- and northward-thickening wedge of rift fill, composed primarily of Santa Fe Group sediments, that serves as an important aquifer for the city of Santa Fe and surrounding areas. Detailed aeromagnetic surveys were flown to better understand ground-water resources in this aquifer. This report presents a synthesis of these data with gravity data and other constraints. The interpretations were accomplished using qualitative interpretation, state-of-art data analysis techniques, and two- and three-dimensional modeling. The results depict the presence of and depth to many geologic features that have hydrogeologic significance, including shallow faults, different types of igneous units, and basement rocks. The results are presented as map interpretations, geophysical profile models, and a digital surface that represents the base and thickness of Santa Fe Group sediments, as well as vector files of some volcanic features and faults.
    Type of Medium: Series available for loan
    Pages: VI, 87 S. : Ill., graph. Darst. + 1 Kt.-Beil. , 1 CD-ROM
    ISBN: 9781411323650 , 1-411-32365-3
    Series Statement: U.S. Geological Survey professional paper 1761
    Classification:
    Regional Geology
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 4
    Call number: S 90.0002(1755)
    In: Professional paper
    Description / Table of Contents: We have used terrestrial cosmogenic nuclides (TCN) to establish the age of some of the most extensive Quaternary alluvial fans in Death Valley, California. These intermediate-age alluvial fans are most extensive on the western side of the valley, where tectonic deformation is considerably less pronounced than on the eastern side of the valley. These fans are characterized by a relatively smooth, densely packed desert pavement formed by well-varnished (blackened) clasts. These surfaces have been mapped as the Q2 gravel by previous workers and as unit Qai (intermediate age) by us. However, the intermediate-age gravels probably contain multiple subunits, as evidenced by slight differences in morphologic expression, soil formation, and inset geomorphic relations. The TCN technique used herein sums the cosmogenic 36Cl in approximately 2.5-meter-deep profiles through soil and host alluvium, thus avoiding some of the problems associated with the more typical surface-exposure dating of boulders or smaller clasts.
    Type of Medium: Series available for loan
    Pages: V, 44 S. : graph. Darst., Ill. ; 28 cm + 1 CD-ROM
    ISBN: 9781411321878
    Series Statement: U.S. Geological Survey professional paper 1755
    Classification:
    Regional Geology
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 5
    Call number: S 90.0002(1767)
    In: Professional paper
    Description / Table of Contents: Hydrogeologic setting -- Mine flooding and aftermath -- Flooding and formation of rubble chimneys -- Water-level recovery and migration of brine -- Interception of brine and saline water -- Geochemical modeling -- Inverse models -- Forward models -- Discussion of results from geochemical modeling -- Simulated migration of brine and saline water during recovery of water levels -- One-dimensional flow -- Three-dimensional flow -- Model design -- Model calibration -- Model results -- Discussion of results -- Simulated pumping of brine and saline water -- Model design -- Model results -- Model sensitivity -- Discussion of results -- Implications for future mitigation efforts -- Current conditions in the collapse area -- Considerations for future mitigation
    Type of Medium: Series available for loan
    Pages: VII, 51 S. , graph. Darst., Kt.
    ISBN: 9781411325029
    Series Statement: U.S. Geological Survey professional paper 1767
    Note: Erscheinungsjahr in Vorlageform:2009
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 6
    Monograph available for loan
    Monograph available for loan
    Berlin [u.a.] : Langenscheidt
    Call number: 22/M 13.0197 (1. Ex) ; 22/M 13.0197 (2. Ex) ; 22/M 13.0197 (3. Ex) ; 22/M 13.0197 (4. Ex) ; 22/M 13.0197 (5. Ex) ; 22/M 13.0197 (6. Ex) ; 22/M 13.0197 (7. Ex) ; 22/M 13.0197 (8. Ex) ; 22/M 13.0197 (9. Ex) ; 22/M 13.0197 (10. Ex) ; 22/M 13.0197 (11. Ex) ; 22/M 13.0197 (12. Ex) ; 22/M 13.0197 (13. Ex) ; 22/M 13.0197 (14. Ex) ; 22/M 13.0197 (15. Ex) ; 22/M 13.0197 (16. Ex) ; 22/M 13.0197 (17. Ex) ; 22/M 13.0197 (18. Ex) ; 22/M 13.0197 (19. Ex)
    Type of Medium: Monograph available for loan
    Pages: 280 S. , zahlr. Ill. , 2 CDs
    ISBN: 9783126060264
    Location: Reading room/gallery
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    Branch Library: GFZ Library
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  • 7
    Call number: S 90.0002(1730
    In: Professional paper
    Description / Table of Contents: The Gogebic iron range is an elongate belt of Paleoproterozoic strata extending from the west shore of Lake Gogebic in the upper peninsula of Michigan for about 125 km westward into northern Wisconsin. It is one of six major informally named iron ranges in the Lake Superior region and produced about 325 million tons of direct-shipping ore between 1887 and 1967. A significant resource of concentrating-grade ore remains in the western and eastern parts of the range.The iron range forms a broad, gently southward-opening arc where the central part of the range exposes rocks that were deposited somewhat north of the eastern and western parts. A fundamental boundary marking both the tectonic setting of deposition and the later deformation within the Penokean orogen lies fortuitously in an east-west direction along the range so that the central part of the range preserves sediments deposited north of that boundary, whereas the eastern and western parts of the range were deposited south of the boundary. Thus, the central part of the range provides a record of sedimentation and very mild deformation in a part of the Penokean orogen farthest from the interior of the orogen to the south. The eastern and western parts of the range, in contrast, exhibit a depositional and deformational style typical of parts closer to the interior of the orogen. A second fortuitous feature of the iron range is that the entire area was tilted from 40° to 90° northward by Mesoproterozoic deformation so that the map view offers an oblique cross section of the Paleoproterozoic sedimentary sequence and structures. Together, these features make the Gogebic iron range a unique area in which to observe (1) the lateral transition from deposition on a stable platform to deposition in a tectonically and volcanically active region, and (2) the transition from essentially undeformed Paleoproterozoic strata to their folded and faulted equivalents.
    Type of Medium: Series available for loan
    Pages: V, 44 S. + 1 Kt.-Beil. , Ill., graph. Darst., Kt. , 28 cm
    ISBN: 9781411319172
    Series Statement: U.S. Geological Survey professional paper 1730
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 8
    Call number: M 12.0043
    Type of Medium: Monograph available for loan
    Pages: 42 S. , graph. Darst., Kt.
    Series Statement: Forschungsberichte / Interdisziplinäre Arbeitsgruppen 20
    Classification:
    Geography and Geomorphology
    Branch Library: GFZ Library
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  • 9
    Series available for loan
    Series available for loan
    Washington, DC : United States Gov. Print. Off.
    Associated volumes
    Call number: S 90.0002(1650-E)
    In: Atlas of relations between climatic parameters and distributions of import trees and shrubs in North America
    In: Professional paper
    Type of Medium: Series available for loan
    Pages: CD-ROM
    Edition: Vers. 1.0
    Series Statement: 1650-E
    Classification:
    Historical Geology
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 10
    Call number: NBM 10.0378
    In: Professional paper
    Type of Medium: Non-book medium
    Pages: 1 CD-ROM , 12 cm
    ISBN: 9781411325012
    Series Statement: U.S. Geological Survey professional paper 1625-F
    Location: Reading room
    Branch Library: GFZ Library
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