1) Tonger mine
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通二井田
1.
Based on these works, the structure characteristics are forecasted in north unmined area of Tonger mine.
通过井下地质调查,论述了通二井田地质构造发育特征及煤层断裂展布规律,表明已采区中、小型煤层断层的展布具有分区性和方向性等特点,并就层滑断裂引起煤层变薄与增厚进行了研究,在此基础上,对北部 (深部 )未采区进行了构造预测。
2) Tongle minefield
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通乐井田
1.
Because of igneous rock intrusion,rocks in the Tongle minefield have higher hardness thus caused serious bit damage.
由于岩浆岩的侵入,通乐井田地层的硬度大,钻头损伤严重。
3) Guoerzhuang mining district
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郭二庄井田
1.
The geological structures formed in Yanshannian movement in Guoerzhuang mining district are researched based on exploration data, mining data, and the data acquired from metal systems.
运用勘探、矿井开采、冶金系统收集的地质资料,从岩浆活动、褶皱断裂构造和地层间的相互切割关系入手,对燕山期的郭二庄井田地质构造作了论述,并对含煤地层的燕山早期岩浆活动进行了研究。
4) Mayidong No.2 minefield
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马依东二井田
5) well
[英][wel] [美][wɛl]
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井田
1.
The great undulating of soleplate of the third coal layer in Wangping well field badly influence exploiting disposal and excavating coal laneway.
针对王坪井田3号煤层底板起伏变化大,严重影响开拓及采煤巷道布置的现状,利用趋势面分析的方法,分析了井田内的构造展布规律。
6) mine field
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井田
1.
Relationship between thickness changes and structural stress in seam of Shanxi Group,Mowo mine field;
磨窝井田山西组煤层厚度变化与构造应力关系
2.
Analysis on the coal characteristics of Mayidong mine field;
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马依东井田煤质特征浅析
3.
Based on the introduction of Suqiao mine field's hydrogeological features as geographical environment,the features of water-bearing formation,and penetrative features of fault,this paper analyzes in detail the water filling factors.
在介绍苏桥井田自然地理环境和岩层含水性,断层的导水性等水文地质特征的基础上,较详细地分析了矿床充水因素,并对该井田的±0m水平和-200m水平的涌水量进行了预测,为矿山开采提供水文地质依据。
补充资料:端石井田砚(清初)
传为著名画家高凤翰旧藏,上有高氏等五名人刻铭,16.5厘米见方,规矩整齐,为端石文物精品。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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