Fluid interaction mechanism and diagenetic reformation of basement reservoirs in Beier Sag, Hailar Basin, China
LI Juan,WEI Pingsheng,SHI Lanting,CHEN Guangpo,PENG Wei,SUN Songling,ZHANG Bin,XIE Mingxian,HONG Liang
Table 1 Data sheet of carbon-oxygen isotope composition test of carbonate filling in basement fractures of Beier Sag.
Sample No. Well No. Depth/m Lithology Analytical minerals δ18O/‰ δ13C/‰
1 B12 1 706.10 Fine sandstone containing tuff and calcium Calcite vein -23.53 -5.63
2 B12 1 705.70 Tuffaceous fine sandstone Calcite vein -23.11 -3.51
3 B16b2 1 864.10 Tuff Calcite vein -23.93 -4.30
4 B16b2 1 875.70 Tuff Calcite vein -18.51 -4.36
5 B30 2 205.20 Slightly-cataclastic carbonation silty mudstone Marble vein -8.32 -0.32
6 B38 2 555.48 Cataclastic tuff Calcite vein -17.78 -11.03
7 B38 2 559.40 Cataclastic tuff Calcite vein -25.34 -4.18
8 B38 2 487.83 Cataclastic chloritization tuff Calcite vein -23.32 -1.78
9 B40 2 362.80 Cataclastic andesitic tuff Calcite vein -24.88 -3.84
10 B40 2 367.30 Andesitic tuff Calcite vein -26.73 -3.79
11 B40 2 377.80 Cataclastic andesitic tuff Calcite vein -23.39 -3.48
12 B40 2 361.30 Cataclastic andesitic tuff Calcite vein -26.14 -4.11
13 D216 1 929.25 Calciferous siltstone Calcite vein -23.35 -4.31