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The most notable area that correlates with major tectonic activity is around the Big Sandy Field that accounts for over 8 0 % of all gas production from Devonian shales. The Warfield anticline passes through the Big Sandy Field and extends northeast into West Virginia. The Arches Fork anticline parallels the Warfield anticline about 20 miles to the northeast. Considerable fracturing in the subsurface parallels the axis of these anticlines. The direction of greatest tectonic stress is generally in a direction of North 45° East, across eastern Kentucky and western West Virginia moving in a northerly direction along the Rome Trough (Fig.

5r Time (years) Fig. 18. History match analysis of cumulative production for well No. 09. Fracture perpendicular to lens; effective fracture length is 200 ft. Unconventional Natural Gas 43 (iii) H o w many lenses, including those not encountered at the wellbore, can a fracture of specified length be expected to penetrate? Each of these assumptions was based on analysis of the available data, as described in what follows. 3. Key Technical Adaptations a. Adjustment for Effective Fracture Length. The simulations of Well N o .

Union Almond A (ft) interval (ft) Net pay Gross (ft) Depth 21-625 9-20 Nature o f pay Lenticular Lenticular Lenticular Otd) In situ gas perm. 2 25 6900-9100 500 43-156 43-156 25-75 Blanket 160-170 Ft. , 4000-6000 ft. ^Canyon lenses are very large relative to the drainage area and substantially broader than the other lenticular formations. G 33 34 V. Kuuskraa and Sonora Basins. By contrast the lenticular basins, with much more of the in-place resource, have seen relatively little development. Even in these basins, the drilling target has tended to the blanket-type pays to the exclusion of the lenticular zones.

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