Illinois State Academy of Science – since 1907
Uniting and expanding scientific interests for all in Illinois and beyond
Skip to content
  • Home
  • About
  • Commitment
  • Transactions
  • Awards
  • Donate
  • Annual Meeting
  • Join
  • Openings
  • My Account
  • Questions?
← [056-08]Experimental Replacement of Oolitic Limestone by Fluorite
[056-10]Differentiation of Some Pennsylvanian Underclays by Their Clay Mineral Composition →

[056-09]Contact Temperature of a Peridotite Dike with Pennsylvanian Shale Determined by Clay Mineral Alterations

Posted on March 23, 2016 by Transactions Editor Webmaster

Parham, Walter E.

Contact Temperature of a Peridotite Dike with Pennsylvanian Shale Determined by Clay Mineral Alterations

056-9-print

 

This entry was posted in 1963, Transactions and tagged Contact Temperature of a Peridotite Dike with Pennsylvanian Shale Determined by Clay Mineral Alterations, Parham. Bookmark the permalink.
← [056-08]Experimental Replacement of Oolitic Limestone by Fluorite
[056-10]Differentiation of Some Pennsylvanian Underclays by Their Clay Mineral Composition →
  • Search all Papers by Author, Title, or Year.

  • Login

     
     
    Forgot Password
  • Reset Password

    Click Here to reset your password


Illinois State Academy of Science – since 1907
Proudly powered by WordPress.
Exit mobile version