- Electron probe microanalysis EPMA
Reed, 1993, p 219 UW- Madison Geology 777 Iterations of Matrix Correction UW- Madison Geology 777 Start with the X-ray Intensities of EACH element i, of the unknown divided by the standard (= K-ratio) Calculate a ZAF correction for the unknown element i, using the previously (step 6) calculated compostion
- Electron probe microanalysis EPMA
UW- Madison Geology 777 C = JEOL SXES (Soft x-ray Emission Spectrometer) D= Traditional WDS with 60 Å 2d synthetic difractor “pseudocrystal” EDS behavior with WDS resolution… UW- Madison Geology 777 With variable spacing grating groves and a CCD, a range of X-ray energies is able to be detected simultaneously
- Whitman College
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- PowerPoint Presentation
Other mismatches of geology and climate included distinctive fossil ferns (Glossopteris) discovered in now-polar regions, and the occurrence of glacial deposits in present-day arid Africa, such as the Vaal River valley of South Africa
- PowerPoint Presentation
Introduction to Powerpoint Brad Jordan Bucknell Geology Bucknell Geology Physiographic Map of Pennsylvania Rip it right off the Web but be careful of copyright violations!
- Powerpoint Presentation Physical Geology, 10 e
Atoms, Elements, and Minerals Physical Geology 13 e, Chapter 2 Tim Horner CSUS Geology Department Minerals A mineral is a naturally occurring, inorganic, crystalline solid, which is physically and chemically distinctive
- PLATE TECTONICS - dentonisd. org
http: geology com nsta transform-plate-boundaries shtml Plates Move Side By Side - ***SHIFTING This is called Transform Boundary – Transform boundaries neither create nor consume crust
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