|
|
Petroleum geological conditions and exploration potential of Lower Paleozoic carbonate rocks in Gucheng Area, Tarim Basin, China
|
CAO Yinghui,WANG Shan,ZHANG Yajin,YANG Min,YAN Lei,ZHAO Yimin,ZHANG Junlong,WANG Xiandong,ZHOU Xiaoxiao,WANG Hongjiang
|
|
|
Table 2 Composition and carbon isotope composition of gas produced from Ordovician Yingshan Formation in the Gucheng area.
|
|
Well | Depth /m | Dry coefficient | Gas composition/% | δ13C/‰ | C1 | C2 | C3 | C4 | C5+ | N2 | CO2 | δ13C1 | δ13C2 | δ13C3 | GC6 | 6 169.0 | 0.997 | 90.7 | 0.25 | 0.015 | 0.002 | 0.29 | 4.26 | 4.71 | -33.6 | -37.6 | -34.9 | GC8 | 6 080.6 | 0.996 | 83.4 | 0.31 | 0.018 | 0.008 | 0.40 | 4.50 | 11.50 | -34.8 | -38.7 | | 0.995 | 82.9 | 0.34 | 0.020 | 0.020 | 0.38 | 4.60 | 11.90 | -35.1 | | | GC9 | 6 116.4 | 0.997 | 71.6 | 0.21 | 0.010 | 0 | 0.22 | 2.30 | 25.70 | -34.6 | -32.9 | -31.3 | 0.997 | 65.6 | 0.22 | 0.010 | 0 | 0.23 | 4.77 | 29.10 | -33.9 | | |
|
|
|