Abstract
Abstract Source rocks can be classified on the basis of shale resistivity ratio parameter [rSR = Rsh (normal) / Rsh (observed)]. High ratios (undercompacted shales) indicate poor source rocks, whereas low ratios (well-compacted shales) may be indicative of good source rocks. In undercompacted shales, oil was not pushed out of shales by associated water due to lack of compaction.
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