Geofluids / 2017 / Article / Tab 1 / Research Article
Multiphase Calcite Cementation and Fluids Evolution of a Deeply Buried Carbonate Reservoir in the Upper Ordovician Lianglitag Formation, Tahe Oilfield, Tarim Basin, NW China Table 1 Carbon and oxygen isotopic data of different stages of pore-filling calcite cement by in situ SIMS of Lianglitag Formation carbonates in the Tahe Oilfield.
Well Number Depth (m) Stage δ 18 O ( VPDB)2SE δ 13 C ( VPDB)2SE S106 1 5885.92 C1 −0.77 0.33 4.08 0.34 S106 2 5885.92 C1 −0.75 0.26 4.50 0.43 S106 3 5885.92 C1 −1.39 0.35 3.72 0.49 S106 4 5885.92 C1 −0.58 0.30 3.69 0.48 S106 5 5885.92 C1 −1.62 0.34 — — S106 6 5885.92 C1 −0.94 0.33 — — S106 7 5885.92 C1 −0.73 0.22 — — S106 8 5885.92 C1 −1.05 0.25 — — S106 9 5885.92 C1 −0.10 0.34 — — S106 10 5885.92 C1 −0.94 0.28 — — S106 11 5885.92 C1 −1.76 0.33 4.10 0.43 S106 12 5885.92 C1 −1.18 0.32 4.34 0.45 S106 13 5885.92 C1 −1.36 0.43 3.50 0.56 S106 14 5885.92 C1 −0.86 0.31 3.35 0.45 S106 15 5885.92 C1 −1.44 0.29 3.72 0.44 S106 16 5885.92 C1 −1.34 0.21 2.98 0.55 S106 17 5885.92 C1 −1.29 0.29 4.02 0.49 S106 18 5885.92 C1 −1.39 0.32 4.02 0.45 S106 19 5885.92 C2 −5.03 0.34 2.47 0.39 S106 20 5885.92 C2 −5.07 0.35 1.58 0.37 S106 21 5885.92 C2 −5.56 0.23 2.72 0.39 S106 22 5885.92 C2 −5.28 0.26 2.13 0.45 S106 23 5885.92 C1 −1.39 0.33 3.91 0.48 S106 24 5885.92 C1 −0.81 0.29 4.04 0.43 S106 25 5885.92 C1 −2.32 0.38 1.44 0.39 S110 1 6089.90 C6 −9.43 0.35 0.92 0.44 S110 2 6089.90 C6 −9.16 0.30 −0.88 0.70 S110 3 6089.90 C6 −9.69 0.29 0.13 0.42 S110 4 6089.90 C6 −9.14 0.28 — — S110 5 6089.90 C6 −9.19 0.29 0.91 0.39 S110 6 6089.90 C6 −9.47 0.43 −0.34 0.48 S110 7 6089.90 C6 −10.02 0.35 −0.12 0.42 S110 8 6089.90 C6 −9.54 0.26 0.48 0.36 S110 9 6089.90 C6 −9.40 0.26 0.57 0.48 T738 1 5893.10 C2 −2.56 0.19 — — T738 2 5893.10 C3 −8.23 0.25 −0.07 0.58 T738 3 5893.10 C3 −7.22 0.30 0.12 0.44 T738 4 5893.10 C2 −2.98 0.22 — — T738 5 5893.10 C2 −2.62 0.30 — — T738 6 5893.10 C5 −8.02 0.14 1.57 0.53 T738 7 5893.10 C5 −8.12 0.27 — — T738 8 5893.10 C5 −7.67 0.22 2.38 0.44 T738 9 5893.10 C2 −3.41 0.25 — — T738 10 5893.10 C4 −4.05 0.20 −0.10 0.58 T738 11 5893.10 C4 −4.49 0.22 −0.32 0.54 T738 12 5893.10 C5 −7.83 0.27 2.30 0.44 T738 13 5893.10 C5 −8.11 0.30 1.92 0.49 T738 14 5893.10 C2 −2.99 0.28 — — T738 15 5893.10 C2 −2.73 0.21 — — T738 16 5893.10 C2 −2.80 0.25 — — T738 17 5893.10 C4 −5.11 0.22 −0.03 0.31 T738 18 5893.10 C4 −4.35 0.27 — — T751 1 5838.00 C3 −7.10 0.26 2.75 0.62 T751 2 5838.00 C3 −6.50 0.28 3.33 0.44 T751 3 5838.00 C3 −8.14 0.28 1.61 0.45 T751 4 5838.00 C4 −2.83 0.35 2.05 0.47 T751 5 5838.00 C4 −3.42 0.34 2.52 0.51 T751 6 5838.00 C1 −3.62 0.38 — — T751 7 5838.00 C4 −4.07 0.30 2.80 0.50 T751 8 5838.00 C4 −2.29 0.37 — — T751 9 5838.00 C3 −7.82 0.34 3.17 0.51 T751 10 5838.00 Matrix −5.33 0.41 3.35 0.67 T751 11 5838.00 C3 −7.12 0.22 3.66 0.28 T751 12 5838.00 C3 −7.88 0.34 4.02 0.37 T751 13 5838.00 C4 −5.07 0.34 4.9 0.57 T751 14 5838.00 C3 −8.45 0.38 2.59 0.51 T751 15 5838.00 C3 −7.60 0.29 4.07 0.47 T751 16 5838.00 C3 −7.09 0.24 3.87 0.48 T751 17 5838.00 C4 −5.37 0.41 3.75 0.58 T751 18 5838.00 C4 −3.51 0.33 3.07 0.55 T751 19 5838.00 C3 −8.76 0.34 1.44 0.59 T751 20 5838.00 C4 −3.50 0.29 3.49 0.24 T751 21 5838.00 C3 −8.18 0.22 — — T751 22 5838.00 C2 −5.55 0.23 3.75 0.28 T751 23 5838.00 C1 −2.68 0.23 4.04 0.32 T904 1 5779.36 C6 −9.38 0.27 −3.88 0.32 T904 2 5779.36 C6 −10.38 0.26 1.70 0.44 T904 3 5779.36 C5 −8.26 0.24 1.72 0.43 T904 4 5779.36 C5 −7.75 0.28 2.10 0.43 T904 5 5779.36 C6 −9.49 0.27 1.20 0.48 T904 6 5779.36 C5 −7.37 0.22 1.48 0.42 T904 7 5779.36 C3 −8.06 0.27 1.90 0.53 T904 8 5779.36 C3 −7.63 0.19 3.34 0.62 T904 9 5779.36 C2 −4.66 0.28 0.71 0.51 T904 10 5779.36 C2 −5.98 0.39 2.91 0.59 T904 11 5779.36 C5 −6.38 0.28 1.54 0.47 T904 12 5779.36 C6 −11.00 0.38 0.60 0.46 T904 13 5779.36 C5 −5.40 0.20 0.56 0.47 T904 14 5779.36 Matrix −7.89 0.36 2.25 0.45 T904 15 5779.36 C2 −6.35 0.32 1.98 0.48 T904 16 5779.36 C3 −7.48 0.34 2.18 0.46 T904 17 5779.36 C3 −6.70 0.25 0.04 0.56 T904 18 5779.36 C5 −5.12 0.29 1.65 0.51 T904 19 5779.36 C5 −6.60 0.33 0.45 0.41 T904 20 5779.36 C3 −6.76 0.24 1.47 0.58