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         Faults Geology:     more books (100)
  1. Geology of Mexico: Celebrating the Centenary of the Geological Society of Mexico (Special Paper (Geological Society of America))
  2. Faults and Subsurface Fluid Flow in the Shallow Crust (Geophysical Monograph)
  3. Active faults of Pakistan: Map sheets and inventories (Special publication)
  4. Late Cenozoic Xianshuihe-Xiaojiang, Red River, and Dali Fault Systems of Southwestern Sichuan and Central Yunnan, China (Special Paper (Geological Society of America))
  5. An Excursion Guide to the Moine Geology of the Scottish Highlands by I. Allison, F. May, 1988-02
  6. It's Your Fault: The San Jacinto Valley Faults by K. Scott Bullock, 1992
  7. Exhumation Associated With Continental Strike-Slip Fault Systems (Special Paper (Geological Society of America))
  8. Active Tectonics of the Devils Mountain Fault and Related Structures, Northern Puget Lowland and Eastern Strait of Juan De Fuca Region, Pacific (U.S. Geological Survey Professional Paper, 1643)
  9. Structural Geology in Reservoir Characterization (Special Publication No. 127) by M. P. Coward, S. Daltaban, et all 1998-01-01
  10. The Geometry of Normal Faults (Geological Society Special Publication) by A. M. Roberts, G. Yielding, 1991-01
  11. Earthquake Proof Design and Active Faults
  12. The Seismogenic Zone of Subduction Thrust Faults (MARGINS Theoretical and Experimental Earth Science Series)
  13. Seismic Interpretation of Contractional Fault-Related Folds: An AAPG Seismic Atlas (AAPG Studies in Geology) by John H. Shaw, 2004-08-01
  14. The Internal Structure of Fault Zones: Implications for Mechanical & Fluid-Flow Properties - Special Publication no 299 by Geological Society Publishing House, 2008-07-15

21. Structural Geology: Faults, Folds, And Fabrics
800 AM1200 PM, Colorado Convention Center C109. Structural geology faults,Folds, and Fabrics. John G. Solum and Alexander P. Bump, Presiding.
http://gsa.confex.com/gsa/2002AM/finalprogram/session_3329.htm
Session No. 13 Sunday, October 27, 2002 8:00 AM-12:00 PM, Colorado Convention Center: C109 Structural Geology: Faults, Folds, and Fabrics John G. Solum and Alexander P. Bump, Presiding Paper # Start Time 8:00 AM HANGINGWALL-TO-DETACHMENT TRANSITION AT A THIN-SKINNED EXTENSIONAL DETACHMENT FAULT IN THE EASTERN BLACK WARRIOR BASIN, ALABAMA : GROSHONG, Richard H. Jr and CATES, Luke M., Department of Geological Sciences, The Univ of Alabama, Tuscaloosa, AL 35487-0338, rhgroshong@cs.com 8:15 AM CHARACTER OF DEFORMATION ADJACENT TO THE SAN ANDREAS FAULT, DURMID HILL, CA : WOJTAL, Steven F., Oberlin, OH 44074, steven.wojtal@oberlin.edu. 8:30 AM TRANSIENT VERSUS LONG-TERM STRAIN ACCUMULATION ON THE BLACKWATER FAULT, EASTERN CALIFORNIA SHEAR ZONE : OSKIN, Michael E., Institute for Crustal Studies, Univ of California, Santa Barbara, 1140 Girvetz Hall, Santa Barbara, CA 93106, oskin@crustal.ucsb.edu. 8:45 AM 1.1 MA MELT PULSES IN PSEUDOTACHYLYTE FROM THE ALPINE FAULT, NZ : VAN DER PLUIJM, Ben A., Geological Sciences, Univ of Michigan, 2534 CC Little Building, Ann Arbor, MI 48109-1063, vdpluijm@umich.edu, WARR, Laurence N., Geologisch-Paläontologisches Institut, Ruprecht-Karls-Universität, Heidelberg, Germany, PEACOR, Donald R., Geological Sciences, Univ of Michigan, Ann Arbor, MI 48109, and HALL, Chris M., Geological Sciences, Univ of Michigan, 4534 CC Little Building, Ann Arbor, MI 48109-1063 9:00 AM FABRICS AND AGE OF CLAY GOUGE IN THE MOAB FAULT, UTAH, USA

22. STRUCTURAL GEOLOGY AND TECTONICS OF THE FRANKLIN MOUNTAINS, WEST TEXAS
STRUCTURAL geology AND TECTONICS OF THE FRANKLIN MOUNTAINS, WEST TEXAS. We describethe kinematics and geometry of faults within the range to constrain the
http://gsa.confex.com/gsa/2002AM/finalprogram/abstract_45716.htm
Paper No. 191-20 Presentation Time: 8:00 AM-12:00 PM STRUCTURAL GEOLOGY AND TECTONICS OF THE FRANKLIN MOUNTAINS, WEST TEXAS WU, Kaiwen and ANDRONICOS, Chris L., Department of Geological Sciences, Univ of Texas at El Paso, 500 W. University Ave, El Paso, TX 79968, wu@geo.utep.edu 2002 Denver Annual Meeting (October 27-30, 2002)
Session No. 191Booth# 119
Tectonics (Posters) II

Colorado Convention Center: Exhibit Hall
8:00 AM-12:00 PM, Wednesday, October 30, 2002

23. Faults
Strikeslip faults Movement along strike-slip faults is horizontal. Returnto Physical geology Online page. Return to Physical geology GSAMS page.
http://www.dc.peachnet.edu/~pgore/geology/geo101/faults.htm
Faults
Pamela J. W. Gore
Georgia Perimeter College
Definition:
A fault is a crack in the Earth's crust along which movement has occurred.
Animation by Charlie Watson, Seismo-Watch Types of faults:
  • Dip-slip faults
    Movement along dip-slip faults is vertical; one side moves up and the other side moves down.
  • Normal fault
  • Reverse fault
  • Thrust fault - a low angle reverse fault
    Normal Faults
    Cambrian Kinsers Formation
    Thomasville Quarry, Pennsylvania Horst and graben terrane, seen in the Basin and Range Province of the western U. S., is dominated by normal faults. Compare with photo above.
    Thrust fault,
    Pennsylvanian Crab Orchard Mountain Group,
    near Ozone, Tennessee, Route 40/75 eastbound.
  • Strike-slip faults Movement along strike-slip faults is horizontal.
  • Left-lateral strike-slip fault
  • Right-lateral strike-slip fault How do you tell which is which?
    Look across the fault to the other side.
    Did it move to the LEFT or to the RIGHT?
    Return to Physical Geology Online page Return to Physical Geology GSAMS page Return to Georgia Geoscience On-line This page created by Pamela J. W. Gore pgore@gpc.peachnet.edu
  • 24. Death Valley Geology Gallery - Faults
    Death Valley National Park geology Image Gallery faults. Badwater Spring andfault Photo by Martin Miller. Black Mountain front Photo by Martin Miller.
    http://wrgis.wr.usgs.gov/docs/parks/deva/galfaults.html
    Death Valley National Park
    Geology Image Gallery - Faults
    Badwater Spring and fault
    Photo by Martin Miller
    Black Mountain front
    Photo by Martin Miller
    Black Mountains wineglass canyon
    Photo by Martin Miller
    Boundary Canyon Fault
    Photo by Martin Miller
    Faulted cinder cone
    Photo by Martin Miller Hanaupah fault scarp Photo by Martin Miller Hanaupah fault and Telescope peak Photo by Martin Miller Springs at base of fan Photo by Martin Miller Normal fault Photo by Martin Miller Death Valley geology Death Valley National Park Geology field trip ... NPS Park Geology Tour home This site is a cooperative endeavor of the US Geological Survey Western Earth Surface Processes Team and the National Park Service Please share your comments and suggestions with us! mmoreno@usgs.gov http://www.nature.nps.gov/grd/usgsnps/deva/galfaults.html This page was last updated on 6/1/00

    25. SanGIS: GENERALIZED GEOLOGY AND FAULTS (Map DPLU0015)
    GENERALIZED geology AND faults. Map Number DPLU0015. Map Title GENERALIZED geologyAND faults. Map Purpose Differentiate geologic formation and fault locations.
    http://www.sangis.org/sangis/mapgal/dplu0015/
    GENERALIZED GEOLOGY AND FAULTS
    Map Number: Map Title: GENERALIZED GEOLOGY AND FAULTS Map Purpose: Differentiate geologic formation and fault locations Date Created: Map Scale: no scale Map Size: 44" x 34" Creating Agency: County DPLU Map Contents: Faults and geologic formations in the San Diego County Update Frequency: N/A Removal Date: Description: Map showing the various geologic types and identifying fault
    locations of San Diego County
    Home About SanGIS Map Gallery Interactive Maps ... Contact Us

    26. UCD Geology: GEL 20 - Faults And Earthquakes
    GEL 20 geology of California faults and Earthquakes . Dipslip faults.A. Normal Yellowstone, 1959; Fairview Peak, 1954; Dixie Valley
    http://www-geology.ucdavis.edu/~GEL20/W99_moores/handouts/faults.html
    GEL 20: Geology of California
    "Faults and Earthquakes"
    Dip-slip Faults
    A. Normal
  • Yellowstone, 1959
  • Fairview Peak, 1954
  • Dixie Valley, Nevada, 1954
  • Klamath Falls, CA, Sept, 1993
  • India, Sept. 1993 B. Thrust (Reverse)
  • Alaska, 1964
  • Chile, 1960
  • Armenia, 1988
  • Coalinga, 1983
  • Winter-Vacaville-Davis, 1892
  • Eureka-Seattle, 1700
  • Whittier, 1987
  • Northridge, 1994
    Strike-slip Faults
  • San Andreas, 1857
  • San Andreas, 1906
  • Hayward 1836, 1868(?)
  • Big Bear, Landers, 1994
    Oblique-slip Faults
  • Loma Prieta, 1989
  • Hyougo-kan Nanbu (Kobe) 1995 Return to GEL 20 Home page
  • 27. Structural Geology Notebook - Tear Faults
    The tear faults may be a result of drastic lateral changes when the Reference Twiss,Robert J. and Moores, Eldridge M.; Structural geology WH Freeman and
    http://maps.unomaha.edu/Maher/geo330/sandbox/tina3.html
    TEAR FAULTS Reference : Twiss, Robert J. and Moores, Eldridge M.; Structural Geology W. H. Freeman and Company, 1992, pp 103 and 113. Above can be seen a small tear fault that linkgs the backthrust with the irregular thrust front. Tina Alder 3/27/97

    28. Descriptive Structural Geology Of Faults
    8 faults and faulting in van der Pluijm Marshak, 1997, Earth Structure An introduction to structural geology and tectonics. McGraw-Hill.
    http://maps.unomaha.edu/Maher/GEOL3300/week2/fault.html
    Description of faults Readings:
    • Scholz, C. H., 1987, Wear and gouge formation in brittle faulting; Geology, v. 15, p. 493-495. This is an introduction to the scaling of various fault parameters.
    This figure is from a core drilled into basement rocks of South Carolina and shows a pseudotachylite injection vein (red arrow), a pseudotachylite slip surface with secondary associated, high angle oblique microfaults (violet arrow), and a chloritized fault breccia (yellow arrow). The slip here is parallel to the gneissic layering. Notebook terms for week 2
    • strike and dip
    • hanging wall and footwall
    • cutoff lines
    • net slip, dip slip, strike-slip
    • piercing points
    • dextral vs. sinistral
    • fault breccia, gouge, flinty crush rock, pseudotachylites
    • breccias as polygenetic
    • mylonites
    • fault scarps
    • striae, slickensides
    • dilatancy
    • drag folds
    • types of fault terminations
    • fault recognition criteria in the field
    • Andersonian classification
    • fault reactivation.
    Fault geometry:
    • idealized as a plane with a vector of slip in it and offset and truncated layers.
      • strike and dip of fault plane.

    29. Major Faults & High-Strain Zones | The Geology Of Virginia
    Valley Ridge faults. Lowangle thrust faults of Alleghanian age (~300 Ma). Mesozoicfaults. Brittle normal faults of Mesozoic age (~200 Ma). CB- DR-,
    http://www.wm.edu/geology/virginia/faults.html
    faults Low-angle thrust faults of Alleghanian age (~300 Ma).
    BR-
    CC-
    HV-
    N-
    NM-
    Sa-
    SP-
    Blue Ridge fault system
    Copper Creek fault
    Hollston Valley fault Narrows fault North Mountain fault Saltville fault Staunton-Pulaski fault Blue Ridge high-strain zone Reverse ductile high-strain zones of Precambrian to Alleghanian age (~700 to ~300 Ma). F- R- Q- Fries zone Rockfish Valley zone Quaker Run zone Piedmont high-strain zones Reverse and strike-slip ductile high-strain zones of Taconic to Alleghanian age (~450- ~300 Ma). Many faults reactivated during Mesozoic. B- BC- CP- Ho- Hy- MR- NC- S- Sh- Brookneal zone Bowens Creek fault Central Piedmont zone Hollister zone Hylas zone Mountain Run zone Nutbush Creek zone Spotsylvania zone Shores melange zone Mesozoic faults Brittle normal faults of Mesozoic age (~200 Ma).

    30. Structural Geology
    How rocks deform, and why, is the study of structural geology. Involves nearsurface to deep crustal processes. 396). Break slip faults (Monroe; fig.
    http://jersey.uoregon.edu/~mstrick/RogueComCollege/RCC_Lectures/Structural.html
    Revised 9 / 01 (Monroe 4th ed.)
    Structural Geology - Chapter 13
    Stress, Geologic Structures, and Deformation of the Crust
    Including... Introduction Introduction to crustal stress Directed stress and crustal deformation Geologic structures ... Directed stress and plate tectonics
    Introduction Before we start, we need to review the following: There are 2 main earth elevations Above and below sea level There are 2 main earth processes Construction and Destruction Tectonics and surface weathering Over the course of geologic time these 2 are in balance There are 2 main igneous rocks Basalt and granite All three of these are inter-related (DESCRIBE) What we are studying tonight is the reality of tectonics DEFINE: Tectonics Tectonics: the study of earth processes which result in the creation and deformation of magma and rock Constructional processes My favorite part of geology (really should save to last!!) Some are real flashy: get some videodisc frames Volcanoes Earthquakes All involve stress at varying degrees of intensity Mt. St. Helens - good example of stress at the surface

    31. North Cascades Geology: Forming Depressions Along Faults
    in the fault planes that open up gaps in the crust, or to have the faults discontinuousbut arranged in an en echelon pattern. USGS geology in the Parks home
    http://www.aqd.nps.gov/grd/usgsnps/noca/sb11faultbasins.html
    North Cascades National Park:
    Forming depressions along faults Diagramatic map showing how horizontal movement on faults can produce depressions that fill with sediment.
    One way to get extension or stretching of the crust while blocks of crust are sliding past each other along large faults is to have irregularities in the fault planes that open up gaps in the crust, or to have the faults discontinuous but arranged in an en echelon pattern North Cascades geology home North Cascades National Park home
    Geology field trip
    Site contents ... NPS Park Geology Tour home This site is a cooperative endeavor of the
    US Geological Survey Western Earth Surface Processes Team

    and the National Park Service
    Please share your comments and suggestions with us!
    mmoreno@usgs.gov
    http://www.nature.nps.gov/grd/usgsnps/noca/sb11faultbasins.html
    This page was last updated on 12/1/99 Material in this site has been adapted from a new book, Geology of the North Cascades: A Mountain Mosaic by R. Tabor and R. Haugerud, of the USGS and published by

    32. Our Hoosier State Beneath Us: Structural Geology: Faults Of Southwestern Indiana
    Recent mapping by the Indiana Geological Survey has located many of the bedrock faultsin southern Indiana and Our Hoosier State Beneath Us Structural geology
    http://www.indiana.edu/~librcsd/etext/hoosier/SG-02.html
    Faults of Southwestern Indiana (SG-02)
    Earthquakes were probably common in southwestern Indiana when several ancient faults that are found in the bedrock were formed, but no modern earthquakes are known to have been associated with them. Even more intense earthquakes in that region have been related to the New Madrid, Missouri, seismic zone, a major area of earthquake activity in the midcontinent region of North America. In 1811-12 three major earthquakes, centered in that area, were among the greatest in recorded history. The recurrence of such earthquakes could have disastrous consequences in Indiana. Recent mapping by the Indiana Geological Survey has located many of the bedrock faults in southern Indiana and has shown that they have been inactive in recent times. Increased knowledge of these structures will also help in exploring for and developing coal and petroleum that are associated with these faulted rocks. Our Hoosier State Beneath Us: Structural Geology

    33. USDA Forest Service Pacific Southwest Region
    Forest geology Structure, faults and Folds BACK. CONTENTS Forest geologyby Tom Dibblee Geologic Structure, faults and Folds BACK.
    http://www.r5.fs.fed.us/lospadres/ecosystem/geology/forest_geology/forest_geo_st
    @import url(http://www.fs.fed.us/r5/global-websites/styles/screen.css); Skip navigation Forest Service National Links Forest Service Home Employment Fire and Aviation International Forestry Just for Kids Maps and Brochures Passes and Permits Photo and Video Gallery Publications Recreational Activities Research and Development State and Private Forestry
    Pacific Southwest Region
    Pacific Southwest Home About Us Contact Us Current Conditions ... Contact Web Manager Pacific Southwest Region
    1323 Club Drive
    Vallejo, CA 94592
    TTY: 707.562.9130
    Error 404 File not found
    The requested URL was not found on this server. The page you are looking for might have been removed, had its name changed, or is temporarily unavailable. Please try the following: Please address questions and comments to: Public Affairs The Pacific Southwest Region manages the National Forests in California and assists the State and Private forest landowners in California, Hawaii and the U.S. Affiliated Pacific Islands.

    34. USDA Forest Service Pacific Southwest Region
    geology Geohazards Earthquakes faults BACK. CONTENTS GeohazardsEarthquakes Faulting BACK. Earthquakes and faults. A fault
    http://www.r5.fs.fed.us/lospadres/ecosystem/geology/geohazards/earthquakes.html
    @import url(http://www.fs.fed.us/r5/global-websites/styles/screen.css); Skip navigation Forest Service National Links Forest Service Home Employment Fire and Aviation International Forestry Just for Kids Maps and Brochures Passes and Permits Photo and Video Gallery Publications Recreational Activities Research and Development State and Private Forestry
    Pacific Southwest Region
    Pacific Southwest Home About Us Contact Us Current Conditions ... Contact Web Manager Pacific Southwest Region
    1323 Club Drive
    Vallejo, CA 94592
    TTY: 707.562.9130
    Error 404 File not found
    The requested URL was not found on this server. The page you are looking for might have been removed, had its name changed, or is temporarily unavailable. Please try the following: Please address questions and comments to: Public Affairs The Pacific Southwest Region manages the National Forests in California and assists the State and Private forest landowners in California, Hawaii and the U.S. Affiliated Pacific Islands.

    35. Page Not Found
    faults in the Bryant Watershed. faults are breaks in the rock wheremovement of the rocks has occurred. Black lines represent faults.
    http://www.watersheds.org/blue/earth/faults.htm
    We're sorry, the page you are looking for could not be found. Due to the restructuring of our site, it may have moved to a new location. If you typed in the url, be sure the address is typed correctly. Search for the page with keywords. Use the search box in the navigation bar above. The navigation bar has links to the main areas on our site. View our site map to find a listing of the topics we have to offer. If you are unable to find what you're looking for, e-mail webkeeper@watersheds.org

    36. Page Not Found
    Geologic map of the Bryant Watershed area. Black lines represent faults. Colorsrepresent different rock formations. Back to Rock Structures faults.
    http://www.watersheds.org/blue/earth/faults01a.htm
    We're sorry, the page you are looking for could not be found. Due to the restructuring of our site, it may have moved to a new location. If you typed in the url, be sure the address is typed correctly. Search for the page with keywords. Use the search box in the navigation bar above. The navigation bar has links to the main areas on our site. View our site map to find a listing of the topics we have to offer. If you are unable to find what you're looking for, e-mail webkeeper@watersheds.org

    37. Figure F3. Simplified Regional Geology, Including Offshore Faults And Depocenter
    Figure F3. Simplified regional geology, including offshore faults and depocenters.Small circles locate active volcanoes, including Mt. Lamington (L), Mt.
    http://www-odp.tamu.edu/publications/180_SR/synth/s_f3.htm
    Figure F3. Simplified regional geology, including offshore faults and depocenters. Small circles locate active volcanoes, including Mt. Lamington (L), Mt. Victory (V), and Dawson Strait (D). The dashed line locates the landward boundary of oceanic crust, and the thin double lines locate the spreading axes. Ticks on normal faults indicate the downthrown side; triangles on reverse faults, the upthrusted side. Islands include Amphlett (A), D'Entrecasteaux (DE), Egum Atoll (E), Lusancay (LC), Misima (MI), Trobriand (T), and Woodlark (W). M = Moresby Strait, MR = Moresby rift, MS = Moresby Seamount.

    38. Geology - North Carolina (1:250,000) Faults - Western North Carolina
    1986 Ending_Date 19981201 Source_Currentness_Reference Data creation and editdates Source_Citation_Abbreviation geology faults, CGIA Source_Contribution
    http://www.lib.ncsu.edu/stacks/gis/regional/westnc/metadata/cgia83/landres/wgeo2
    Geology - (1:250,000) Faults - Western North Carolina
    Metadata also available as - [ Parseable text
    Metadata:
    Citation:
    Originator: NCSU Center for Earth Observation Title:
    Geology - North Carolina (1:250,000) Faults - Western North Carolina
    Shape file
    Raleigh, NC Publisher: NCSU Libraries
    NCSU Libraries is responsible for this data set
    online mapping at: online metadata at: original metadata at:
    Description:
    Abstract:
    The North Carolina Department of Environment, Health, and Natural Resources, Division of Land Resources, NC Geological Survey, in cooperation with the North Carolina Center for Geographic Information and Analysis, developed the GIS data set version of the Geology of North Carolina. The data represents the digital equivalent of the official State Geology map (1:500,000-scale), but was digitized from (1:250,000-scale) base maps. This file contains the line attributes which identify faults in North Carolina. The geologic formation id is the only attribute present. There are two additional files which accompany this layer, formations and dikes. These should be used together with the faults layer. All three files come together. (Refer to the cross references section for more detail on the formations and dikes). The NCSU Center for Earth Observation created this clipped coverage consisting of the 24 westernmost counties of North Carolina.
    Purpose:
    This data was created to assist governmental agencies and others in making resource management decisions through use of a Geographic Information System (GIS). This clipped coverage was created for use in conjunction with the Western North Carolina Region Data System.

    39. GIS Lookup: Geology
    National Atlas geology faults (decorated), USGS, Line, Shapefile, 17m, 2001,US. National Atlas geology - faults (undecorated), USGS, Line, Shapefile, 17m,2001, US.
    http://www.lib.ncsu.edu/stacks/gis/themes/term0145.html

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    SEE ALSO : Narrower Terms: Dikes Faults Geologic Formations Coasts ... Subsurface Hydrography
    Click on Title to See Full Record Title Source Type Format Scale Date Coverage Geologic Regions of North Carolina NCDENR Polygon ARC/INFO NC CGIA: Hydrogeology: NC Piedmont and Blue Ridge NCCGIA Polygon ARC/INFO Chesapeake Watershed Lithogeochemical Map: Lithogeochemical Map Units USGS Polygon Chesapeake Watershed Chesapeake Watershed Lithogeochemical Map: Sulfide Deposits USGS Polygon Chesapeake Watershed Chesapeake Watershed Lithogeochemical Map: Geologic Map Units USGS Polygon Chesapeake Watershed National Atlas: Generalized Geologic Map of the Conterminous US USGS Polygon Shapefile Conterminous US Lithochronologic Units and Mineral Deposits: Lithology USGS Polygon Shapefile/e00/SDTS Appalachian Region Quaternary Sediments: Miscellaneous Geologic Point Features USGS Point Shapefile/SDTS/e00 n/a North-Central US Lithochronologic Units and Mineral Deposits: Normal Thrusts USGS Line Shapefile/e00 Appalachian Region Mineral Resources: Igneous Rocks PLUTO USGS Polygon Shapefile n/a US USGS: Geology USGS Polygon E00/DLG Conterminous US USGS: Legend USGS Text E00/DLG Conterminous US South Carolina Piedmont and Blue Ridge: Geology USGS Polygon Shapefile/e00

    40. Zeal.com - United States - New - Library - Sciences - Earth & Environment - Geol
    A great resource for United States New - Library - Sciences - geology- Seismology - faults. Find the web's best sites, add websites
    http://www.zeal.com/category/preview.jhtml?cid=1144552

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