Figure 35. Evolution of LHC ratio "H" with maximum-attained subsurface temperature in sediments bearing Type II kerogen in various wells in North America. In this instance increase with temperature is linear.
Figure 35
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Figure 35. Evolution of LHC ratio "H" with maximum-attained subsurface temperature in sediments bearing Type II kerogen in various wells in North America. In this instance increase with temperature is linear. |