File:M102Ch1Fg4.jpg

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SE2 (a) and BSE1 (b) image of a cross section of a shale rock. Note that the contrast between carbonate (ca) and silica (si) grains is much higher in BSE1; the topographical information is greater in the SE2 image (OM-associated nanopores are not visible in BSE1). From AAPG Memoir 102, Chapter 1, Huang et al., 2013, DOI: 10.1306/13391699M1023580.

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current21:56, 14 August 2014Thumbnail for version as of 21:56, 14 August 20141,492 × 746 (1.74 MB)Molyneux (talk | contribs)SE2 (a) and BSE1 (b) image of a cross section of a shale rock. Note that the contrast between carbonate (ca) and silica (si) grains is much higher in BSE1; the topographical information is greater in the SE2 image (OM-associated nanopores are not visib...

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