Organoporosity Evaluation of Shale: A Case Study of the Lower Silurian Longmaxi Shale in Southeast Chongqing, China
Figure 2
The transformation ratio of oil and gas generated from organic matter at different temperatures and heating rates. (a) The transformation ratio of oil generated from kerogen of Xiamaling Shale. (b) The transformation ratio of gas generated from kerogen of Xiamaling Shale. (c) The transformation ratio of gas generated from oil cracking.
