Re-Os Evidence Used to Link Regional Mineralization Processes to the Chesapeake Bay Bolig’s Impact in the Northeastern United States

Rhenium-Osmium (Re-Os) isotope measurements of sulfide minerals from 10 occurrences that span a radial distance of over 200 Km serve to geochemically link epithermal mineralization in Pennsylvania to an Eocene event. The most likely geologic event that could have influenced the area during the Eocene is the Chesapeake Bay impact event. The significance of the discovery is twofold: to date no epithermal mineralization has been linked to the Chesapeake Bay impact nor has the process been clearly identified throughout the region. The results effect road construction plans for Pennsylvania, Maryland, and Virginia near the meteor impact site because mineralization could occur in any age strata that lie along fracture traces identified in this contribution.

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  • Supplemental Notes:
    • This document was sponsored by the U.S. Department of Transportation, University Transportation Centers Program.
  • Corporate Authors:

    Juniata College

    1700 Moore St
    Huntingdon, PA  United States  16652

    Mid-Atlantic Universities Transportation Center

    Pennsylvania State University
    201 Transportation Research Building
    University Park, PA  United States  16802-4710

    Research and Innovative Technology Administration

    1200 New Jersey Avenue, SE
    Washington, DC  United States  20590
  • Authors:
    • Mathur, Ryan
    • Gold, David P
    • Ellsworth, Chad J
    • Doden, Arnold G
    • Wilson, Marc
    • Ruiz, Joaquin
    • Scheetz, Barry E
  • Publication Date: 2010-10

Language

  • English

Media Info

  • Media Type: Web
  • Edition: Final Report
  • Features: Figures; References; Tables;
  • Pagination: 17p

Subject/Index Terms

Filing Info

  • Accession Number: 01472494
  • Record Type: Publication
  • Report/Paper Numbers: PSU-2008-05
  • Contract Numbers: DTRT07-G-0003
  • Files: UTC, NTL, TRIS, ATRI, USDOT
  • Created Date: Feb 19 2013 8:47AM