Three-Dimensional Morphology and Connectivity of Organic Pores in Shale from the Wufeng and Longmaxi Formations at the Southeast Sichuan Basin in China

<div>Graptolite photographs and energy spectrum of the Wufeng-Longmaxi Formation shale in the southeast Sichuan Basin. The fragment is graphitic, that is, mainly composed of carbon. The fragment is encased in clay minerals and carbonate minerals.</div>

Geofluids

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Figure 4

Figure 4: Three-Dimensional Morphology and Connectivity of Organic Pores in Shale from the Wufeng and Longmaxi Formations at the Southeast Sichuan Basin in China 

Figure 4 | Three-Dimensional Morphology and Connectivity of Organic Pores in Shale from the Wufeng and Longmaxi Formations at the Southeast Sichuan Basin in China 