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1)  Ordovician limestone karstic water
奥灰岩溶水
1.
1 shaft minefield belongs to an area with structurally medium complexity,while the direct mine water filling sources are atmospheric precipitation,surface water,coal measures sandstone fissure water,gob water,structure water(through faults and subsided columns),indirect source is Ordovician limestone karstic water.
安家岭井工矿一号井田地质构造中等复杂区;矿床充水直接充水水源为大气降水和地表水、煤系砂岩裂隙水、老窑水、构造水(通过断层和陷落柱),间接充水水源为奥灰岩溶水。
2.
Thoroughly analyzed Ordovician limestone karstic water water-bearing strata,recharging,runoff and discharging conditions,development and utilization status quo,and probed into vertical changing pattern of Ordovician limestone karstic water as well.
根据铜川新区的地层、构造及水文地质特征,对其奥灰岩溶水的含水岩性,补给、径流、排泄条件,水质特征,富水性及开发利用现状作了深入分析,总结了该区奥灰岩溶水的垂向变化规律,为合理开发利用奥灰岩溶水提出建议。
2)  Ordovician limestone karst water
奥灰岩岩溶水
3)  Ordovician limestone karst
奥灰岩溶
4)  ordovician and cambrian limestone groundwater
奥-寒灰岩水
5)  Ordovician karstic water
奥陶系岩溶水
1.
Evaluation of Shaozhuang-Shuangmiao water site Quaternary pore water and Cambro-Ordovician karstic water environmental quality status quo were based on single constituent comprehensive evaluation.
按照单项组分、综合评价法,对邵庄—双庙水源地第四系孔隙水和寒武—奥陶系岩溶水环境质量现状进行了评价。
6)  ordviian system lime rock watery strata
奥陶系灰岩含水层
补充资料:奥水
1.古水名。在今河南省泌阳﹑遂平县境。
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