WebSep 21, 2012 · Cleat orientation commonly controls the direction of mining with major development paralleling the face cleat. Previous researchers have categorized the origin of cleat as endogenetic, relating the origin of cleat to compaction and coalification, and exogenetic, relating the origin of cleat to tectonic forces. WebFeb 1, 1998 · One coal-bed surface showed the expected result that cleat systems are well connected, due to systematic development of butt cleats extending from one face cleat to …
Interaction of Cleat-Matrix on Coal Permeability from …
WebSep 21, 2012 · Cleat orientation commonly controls the direction of mining with major development paralleling the face cleat. Previous researchers have categorized the origin … WebNatural fractures in coal can be divided into two general types: cleat and shear structures. Cleat has been studied for more than a century, yet the mechanisms of cleat formation … taxi company woodbridge
Stress-Dependent Deformation and Permeability of a Fractured Coal …
WebSep 14, 2009 · Coal is a naturally fractured reservoir where the natural fractures or cleats influence the reservoir permeability. Coal cleat originates as a result of either physical and chemical changes during ... Webcoal are called "cleat" and are analogous to joints in other rock types. Cleat in coal occurs as two fracture sets oriented at approximately 90" to each other. One cleat is usually … WebAug 1, 1993 · The cleats in coal beds and joints in the outcrop rocks in the four coal fields were formed by tectonic forces. Cleat and joint characteristics, such as smooth, planar, or slickensided surfaces; regularity of spacing; continuity of orientation over a large areal extent: plumose structures; and the presence of gouge zones suggest a regional ... the christ candle reading