By Neal R. O’Brien, Roger M. Slatt (auth.)
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1 mm. Plane light. GRAY SHALE FORMATION (U. Lias, Jurassic) Port Mulgrave, Yorkshire, England. This thin-section shows a coarser material filling burrows and the swirled nature of lamination. Burrows are the lighter areas. Obviously this rock was originally laminated and laminae were disrupted during bioturbation. 1 mm. Plane light. GRAY SHALE FORMATION ( Lias, Jurassic) Port Mulgrave, Yorkshire, England. This sample shows coarser material filling burrows and the swirled nature of lamination. The burrows are the lighter colored areas.
EDGE-FACE /// \\y// FACE-FACE EDGE-EDGE References: Bennett et al. (1979), Van Olphen (1963), O'Brien (1987). 26 CANN I G ELECTRON MICRO COpy DE CRIPTIONS·RANDOM PARTICLE ORIENTATION I N MUDSTONE c A B D 27 27 FABRIC VARIATIONS IN ORGANIC RICH SHALES A. ORGANIC HASH - MECCA QUARRY SHALE MEMBER (Linton Formation, Pennsylvanian) Park County, Indiana. 3%. Scale = 10 JUn. Even though preferred orientation dominates, organic rich shale microfabrics revealed by the SEM do vary. This section illustrates four main types of microfabric found in an SEM analysis of over 100 organic rich shales from various stratigraphic positions and sedimentary environments.
There is no attempt here to propose an organic shale classification, but only to clarify analysis of organic rich shales by supplying suitable descriptive terminology. This analysis may be of value to those undertaking studies of hydrocarbon production potential of organic rich shales. B. ORGANIC-CLAYEY - ROOF SHALE SPRINGFIELD COAL MEMBER (petersburg Formation, Pennsylvanian) Vanderburg County, Indiana. 2%. Scale = 10 JUn. C. CLAYEY - GENESEO MEMBER (Genesee Formation, Upper Devonian) Seneca County, New York.
Argillaceous Rock Atlas by Neal R. O’Brien, Roger M. Slatt (auth.)