“…Being the main component of depositional OM, kerogen is often considered a part of the shale matrix framework and thus is directly subjected to the pressure exerted by overlying strata. , Although a high pore pressure and sealing ability can resist the pressure exerted by the overlying formation, compaction becomes more intense as the burial depth increases, and the strong physical–chemical structural changes that occur in shale make it difficult to identify the OM components. , Therefore, the kerogen morphology is generally incomplete and is characterized by poorly developed pores (Figure a), strong heterogeneity (Figure b), and an irregular shape (Figure c). However, the residual OM still maintains its biological structure, which has bands or a particular shape (Figure ), and shows different anisotropy strength in the compaction direction.…”