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https://www.onepetro.org/conference-paper/OTC-23796-MS
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In contrast, the Kingak source rock is mostly clay shale that deforms plastically, and brittle lithologies generally are absent. These petroleum system elements (organic matter content, thermal maturity, and brittle lithology) were among the factors considered in estimating the probability thatoil and gas can be technically recovered from the source rocks, with results of 95 percent probability for the Shublik, 90 percent for the Brookian, and 40 percent for the Kingak (Houseknecht et al., 2012b).
The Kingak is poorly known beneath the southwestern North Slope because of an absence of well penetrations (Fig. 3). We infer that the best oiland gas potential in the Kingak occurs within the shale-oil and shale-gas AUs,respectively, and basinward from the shelf sequences in north-central NPRA(Fig. 3). However, the paucity of brittle facies in the lower Kingak Shale maylimit its reservoir quality everywhere.
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However as mentioned Ice 1 has classified the HRZ as more silaceous than clastic implying it will retain structure.
d.
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