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. 2023 Aug 12;13:13128. doi: 10.1038/s41598-023-40334-y

Figure 4.

Figure 4

Petrographic observations of the Second Member, Qixia Formation and Wulong section. (a) Bioclastic limestone (L1), moldic porosity (MO) and intraparticle porosity are filled with dolomite cement (Cd). The white dotted line represents Phase-I fracture (FR-1) filled with CC and alizarin red staining (Sp-5B, C9). (b) Fine dolomite (D1) is composed of anhedral and subhedral crystals with residual particle structure; intercrystal porosity (BC) developed and porosity was 8% (Sp-06, C9). (c) Medium dolomite (D2), obvious brecciation. The white dotted line represents Phase-II fracture (FR-2) filled with Py, Fl and CC (Sp-5A, C7). (d) The blue dotted line represents FR-1 and the white dotted line represents FR-2. The yellow dotted line represents Phase-III fracture (FR-3) which cuts across FR-2, Cd2 and CC while FR-2 cuts FR-1 (Sp-5A, C7). (e) Medium to coarse dolomite (D2). The white dotted line represents fractured plane light (Sp-07, C9). (f) Figure e displays dull-red luminescence under CL. The white dotted line represents the fracture (Sp-07, C9). (g) Fine dolomite (D1). The white dotted line represents the fracture plane light (Sp-07, C9). (h) Figure g displays the dull luminescence under CL. The white dotted line represents the fracture (Sp-07, C9).