Research Article
Applications of Vitrinite Anisotropy in the Tectonics: A Case Study of Huaibei Coalfield, Southern North China
Table 4
Calculated results of RIS parameters, Huaibei coalfield.
| Region | Coal number | Coal seam | DT | R
st | R
am | R
ev | | / | | Axis ratio | | | / | / | / |
| Region A | TYM03 | 8 | BD | β14.43 | 0.05 | 0.90 | 0.24 | 0.24 | 1.07 | 1.23 | 1.31 | 0.33 | TYM04 | 8 | BC | 1.06 | 0.04 | 0.90 | 0.19 | 0.19 | 1.11 | 1.11 | 1.23 | 0.96 | TYM06 | 10 | BC | β20.43 | 0.03 | 0.82 | 0.13 | 0.15 | 1.03 | 1.15 | 1.18 | 0.20 | TYM07 | 10 | BC | β0.05 | 0.02 | 0.75 | 0.07 | 0.09 | 1.05 | 1.05 | 1.10 | 0.95 | XTM01 | 7 | BC | 2.52 | 0.04 | 0.99 | 0.23 | 0.20 | 1.12 | 1.12 | 1.26 | 1.04 | XTM02 | 7 | BD | 14.66 | 0.03 | 1.03 | 0.14 | 0.12 | 1.10 | 1.04 | 1.14 | 2.49 | XTM06 | 7 | DS | β6.05 | 0.03 | 1.06 | 0.16 | 0.14 | 1.06 | 1.10 | 1.16 | 0.64 | XTM07 | 7 | BC | β4.73 | 0.02 | 1.05 | 0.12 | 0.11 | 1.05 | 1.07 | 1.13 | 0.71 |
| Region B | LHM02 | 7 | DS | β12.79 | 0.03 | 1.23 | 0.18 | 0.13 | 1.04 | 1.11 | 1.16 | 0.41 | LHM03 | 7 | DS | 17.42 | 0.06 | 1.31 | 0.38 | 0.24 | 1.23 | 1.07 | 1.32 | 2.93 | LHM04 | 9 | BD | β9.73 | 0.02 | 1.38 | 0.17 | 0.12 | 1.04 | 1.08 | 1.13 | 0.51 | LHM05 | 9 | BD | 2.89 | 0.05 | 2.70 | 0.72 | 0.23 | 1.15 | 1.14 | 1.31 | 1.04 | LHM09 | 9 | BD | β3.89 | 0.04 | 1.29 | 0.30 | 0.21 | 1.10 | 1.15 | 1.26 | 0.70 | LHM12 | 10 | BD | 12.26 | 0.02 | 1.16 | 0.14 | 0.11 | 1.08 | 1.04 | 1.13 | 2.08 | LHM14 | 10 | BD | β4.52 | 0.03 | 1.34 | 0.33 | 0.22 | 1.10 | 1.16 | 1.28 | 0.67 | LHC01* | β | β | 25.69 | 0.04 | 1.21 | 0.24 | 0.18 | 1.19 | 1.02 | 1.21 | 9.98 | HZM03 | 10 | BC | 15.63 | 0.03 | 1.75 | 0.30 | 0.15 | 1.13 | 1.05 | 1.18 | 2.65 | HZM04 | 10 | BC | β21.15 | 0.02 | 1.94 | 0.19 | 0.09 | 1.02 | 1.09 | 1.10 | 0.19 | HZM10 | 8 | DS | 18.44 | 0.01 | 2.57 | 0.15 | 0.06 | 1.05 | 1.01 | 1.06 | 3.63 | HZC02* | β | β | β1.14 | 0.04 | 1.31 | 0.29 | 0.20 | 1.11 | 1.13 | 1.25 | 0.84 | HZC03* | β | β | 6.18 | 0.05 | 1.27 | 0.32 | 0.22 | 1.15 | 1.12 | 1.28 | 1.29 | BSC04* | β | β | 21.95 | 0.05 | 2.27 | 0.53 | 0.20 | 1.21 | 1.04 | 1.25 | 5.01 | BSC05* | β | β | 4.55 | 0.05 | 2.22 | 0.58 | 0.23 | 1.15 | 1.13 | 1.30 | 1.16 |
| Region C | LLM03 | 8 | BC | β7.01 | 0.04 | 0.98 | 0.18 | 0.17 | 1.07 | 1.12 | 1.21 | 0.59 | LLM05 | 8 | BC | β11.51 | 0.07 | 0.72 | 0.24 | 0.29 | 1.10 | 1.28 | 1.41 | 0.40 | LLM07 | 10 | BC | β6.37 | 0.05 | 0.85 | 0.21 | 0.22 | 1.10 | 1.17 | 1.28 | 0.60 | LLM08 | 10 | BD | β8.05 | 0.02 | 0.79 | 0.08 | 0.10 | 1.04 | 1.07 | 1.11 | 0.58 | LLM10 | 8 | BC | 11.71 | 0.06 | 0.94 | 0.27 | 0.25 | 1.20 | 1.11 | 1.33 | 1.84 | YZM11 | 3 | BC | β12.87 | 0.05 | 1.54 | 0.37 | 0.21 | 1.07 | 1.19 | 1.27 | 0.38 | YZM14 | 3 | BC | β15.35 | 0.04 | 1.55 | 0.32 | 0.19 | 1.05 | 1.17 | 1.23 | 0.32 | YZM16 | 3 | BC | β4.68 | 0.06 | 1.56 | 0.53 | 0.29 | 1.14 | 1.23 | 1.41 | 0.63 | STM01 | 3 | BD | β21.59 | 0.05 | 1.39 | 0.32 | 0.21 | 1.03 | 1.22 | 1.26 | 0.17 | STM02 | 3 | BC | β20.95 | 0.05 | 1.28 | 0.31 | 0.22 | 1.04 | 1.24 | 1.29 | 0.18 | STM03 | 3 | BD | 23.20 | 0.08 | 1.37 | 0.54 | 0.31 | 1.38 | 1.06 | 1.46 | 5.57 | STC06* | β | β | β3.00 | 0.05 | 1.35 | 0.33 | 0.22 | 1.11 | 1.15 | 1.28 | 0.74 |
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*Data complied from [18] except for the coal seam and deformation type of these four samples. Abbreviations: BD: brittle-ductile transition; DS: ductile shear; BC: brittle crush; DT: deformation type; : maximum reflectance; : intermediate reflectance; : minimum reflectance; : bireflectance, β; K: Flinnβs parameter, (-)/(-), where = ln (), = ln (), = ln (); : RIS anisotropy magnitude, ; β style, 30-arctan (/); : reflectance of equivalent volume isotropic RIS, ; where = /() + [ + 1/3 cos 30Β°] Γ tan 30Β° β 1/2, = [/() β 1/3] Γ cos 30Β°.
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