Genesis of calcite vein in basalt and its effect on reservoir quality: A case study of the Carboniferous in the east slope of Mahu sag, Junggar Basin, NW China
XIA Lu,CAO Yingchang,BIAN Baoli,LIU Hailei,WANG Xiaoxue,ZHAO Yiwei,YAN Miaomiao
Fig. 3. XRF scanning results of core samples in Madong area. (a) At 3877.13 m in Well Ma 201, basalt, Ti content distribution, bright Ti-rich strips are dislocated, see the photo of the corresponding rock sample in Fig. 2b; (b) at 3877.13 m in Well Ma 201, Ca content distribution, Ca is rich in fractures and pores; (c) at 3877.13 m in Well Ma 201, Mn content distribution, Mn is rich in fractures; (d) at 4678.90 m in Well Madong 3, photo of basalt sample; (e) at 4678.90 m in Well Madong 3, Ca content distribution, Ca is rich in fractures and pores; (f) at 4678.90 m in Well Madong 3, Mn content distribution, the distribution of Mn is irregular and the fracture edge is relatively rich in Mn; (g) at 4634.70 m in Well Madong 3, photo of andesite sample; (h) at 4634.70 m in Well Madong 3, Ca content distribution, Ca is rich locally in fractures; (i) at 4634.70 m in Well Madong 3, Mn content distribution, the distribution of Mn is limited in the fractures; (j) at 5334.10 m in Well Xiayan 2, photo of basalt sample, the sampling location is shown in Fig. 2d; (k) at 5334.10 m in Well Xiayan 2, Ca content distribution, Ca is rich in fractures; (l) at 5334.10 m in Well Xiayan 2, Mn content distribution, Mn is rich in lower part of horizontal fractures.