鄂西黄陵背斜周缘震旦系灯影组白云岩成因分析
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李浩涵, 张聪, 李文正, 张春贺, 张远, 王梓, 陈维堃, 方镕慧
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Genetic analysis of dolomites in the Sinian Dengying Formation on the periphery of the Huangling anticline, western Hubei Province
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LI Hao-Han, ZHANG Cong, LI Wen-Zheng, ZHANG Chun-He, ZHANG Yuan, WANG Zi, CHEN Wei-Kun, FANG Rong-Hui
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表2 矿物含量与白云石有序度数据
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Table 2 Mineral content and dolomite ordering data
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序
号 | 样品
编号 | 矿物含量/% | 白云石
有序度 | | 方解石 | 白云石 | 石英 | 钾长石 | 斜长石 | | 1 | QLK-01 | 14 | 86 | / | / | / | 0.67 | | 2 | QLK-02 | / | 68 | 24 | 8 | / | 0.61 | | 3 | QLK-03 | / | 99 | 1 | / | / | 0.99 | | 4 | QLK-04 | 3 | 90 | 5 | / | 2 | / | | 5 | QLK-05 | / | 99 | / | / | 1 | / | | 6 | QLK-06 | 10 | 86 | 4 | / | / | / | | 7 | QLK-07 | / | 90 | 10 | / | / | 0.82 | | 8 | QLK-08 | / | 87 | 13 | / | / | 0.74 | | 9 | QLK-09 | 17 | 83 | / | / | / | 0.74 | | 10 | QLK-10 | / | 97 | / | 2 | 1 | / | | 11 | QLK-11 | 6 | 93 | / | / | 1 | / | | 12 | QLK-12 | / | 86 | 11 | 3 | / | 0.57 | | 13 | QLK-13 | / | 93 | / | 7 | / | / | | 14 | QLK-14 | 14 | 86 | / | / | / | 0.76 | | 15 | QLK-15 | / | 85 | / | 15 | / | 0.77 | | 16 | QLK-16 | / | 96 | 4 | / | / | / | | 17 | QLK-17 | / | 89 | 11 | / | / | / | | 18 | QLK-18 | / | 85 | 10 | / | 5 | / | | 19 | QLK-19 | / | 85 | 15 | / | / | 0.82 | | 20 | QLK-20 | / | 92 | / | 8 | / | 0.78 | | 21 | QLK-21 | / | 98 | / | 1 | 1 | 0.9 | | 22 | QLK-22 | / | 96 | 4 | / | / | 0.85 | | 23 | QLK-23 | / | 93 | 6 | 1 | / | 0.81 | | 24 | QLK-24 | / | 95 | 4 | 1 | / | 0.85 | | 25 | YX-01 | / | 100 | / | / | / | 0.9 | | 26 | YX-02 | / | 99 | 1 | / | / | 0.96 | | 27 | YX-03 | / | 89 | 1 | / | 10 | / | | 28 | YX-04 | / | 96 | 4 | / | / | 0.85 | | 29 | YX-05 | / | 96 | 2 | 2 | / | 0.83 | | 30 | YX-06 | 2 | 93 | / | 5 | / | 0.8 | | 31 | YX-07 | / | 90 | 10 | / | / | 0.84 | | 32 | YX-08 | 6 | 80 | 10 | 4 | / | 0.79 | | 33 | YX-09 | / | 91 | 5 | 3 | 1 | 0.82 | | 34 | YX-10 | / | 94 | 5 | 1 | / | 0.83 | | 35 | YX-11 | / | 94 | / | 5 | 1 | 0.84 | | 36 | YX-12 | / | 93 | 2 | 5 | / | 0.88 | | 37 | YX-13 | / | 99 | / | 1 | / | 0.97 | | 38 | YX-14 | / | 100 | / | / | / | 0.94 |
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