龙永煤田吕风矿区童子岩组第三段煤岩层对比分析

本文主要对龙永煤田吕风矿区下二叠统童子岩组第三段煤系地层岩性、古生物特征进行了分析研究，归纳出可操作性的对比方法，对未来矿井开采和邻区矿区的勘探具有一定的指导意义。     

九寨黄龙民用机场土石方挖方区岩石分级与爆破方法的研究

九寨黄龙民用机场土石方挖主要是卵砾石岩层。对该区卵砾石层进行了分级，并分别不同地形地质条件对爆破形式和爆破方法进行了论证，提出了该区应以平洞硐室爆破为主，并给出了相应的爆破参数。     

弱含水地层青山组火山岩地下水分布规律及解决缺水问题探讨

白垩系青山组火山岩是弱含水岩层,但在有利的岩性与构造的作用下,可以形成相对富水地段,通过物探固定小MN装置测深法与地质分析相结合,已打出一批好机井,从而解决了该区严重缺水问题。     

Breakdown of lawsonite subsequent to peak UHP metamorphism in the Dabie terrane and its implication for fluid activity

Abundant occurrences of quartz vein within eclogites in the Dabie-Sulu orogen provide us an opportunity to study metamorphic fluid flow during subduction and exhumation of continental crust. It is, however, usually short of petrological constraints on pressure and temperature of vein formation. This study focuses on kyanite-quartz veins within Iow-T/high-P eclogite in the Dabie terrane that contain unique polycrystalline aggregates, interpreted as pseudomorphs after porphyroblasts of lawsonite. Coesite pseudomorphs were found for the first time in garnet from eclogite, resulting in a revised estimate of peak P-T conditions at 670℃ and 3.3 GPa for the eclogite. This indicates a stability field at graphite/diamond transition, thus upgrading the HP unit to a UHP unit. Neither foliation texture, undulose extinction of quartz nor coesite were observed in quartz veins,although the peak P-T conditions were estimated the same as that in host eclogite in light of thermodynamic calculation based on mineral assemblage in kyanite-quartz veins.Therefore, the formation of the kyanite-quartz veins as wellas the breakdown of lawsonlte into the kyanite-quartz-zoisite assemblage took place during exhumation subsequent to the peak UHP conditions. In this regard, the continental subduction not only brought the water of water-bearing mineral such as lawsonite into the deep mantle, but also released the water from the mineral during exhumation.     

高位顺层钻孔瓦斯抽放数值模拟

针对八连城煤矿19号煤层62.1%~71.6%的瓦斯来源于采空区的问题,提出高位顺层钻孔抽放采空区瓦斯的治理方案.基于关键层理论和"O"形圈理论,分析了采空区上覆岩层裂隙形态,对瓦斯在其中的运移规律进行了研究,认为在上覆岩层采动裂隙中瓦斯流动符合达西定律.利用商业软件COMSOL-Multiphysics对瓦斯抽放进行了数值模拟,直观展示了瓦斯抽采时的瓦斯分布状态.模拟结果表明瓦斯抽放有效降低了瓦斯压力,给现场瓦斯抽放提供了理论依据,具有重要的实践意义.     

弹性地基双跨梁的受力和变形分析

条带开采或利用歼石充填置换条带煤柱开采技术是实现绿色开采的重要技术。考虑到两侧煤体和中间煤柱（或回填柱）的弹性,采场上覆岩层中关键层的力学模型应简化为两端为半无限弹性地基支承、中间有弹性支座的多跨梁,利用弹性地基梁理论,推导了中间有一个弹性支座的弹性地基双跨梁的内力及变形方程的解析解,分析了梁的最大弯矩值及其位置与梁的跨度、相对刚度和载荷之间的关系。     

双裂隙复合岩层单轴压缩力学性质及损伤机理离散元模拟

针对存在内部裂隙的软硬互层复合岩层力学特性展开研究,采用PFC2D建立层状复合岩层离散元模型,通过对完整复合岩层试验细观参数进行校准并验证其宏观特性,研究分析平行双裂隙复合岩层的岩桥倾角与层理倾角对力学特性与破坏模式的影响,得出双裂隙复合岩层的5类最终破坏模式,揭示裂纹演化规律及位移场变化。研究结果表明：双裂隙复合岩层峰值强度随岩桥倾角增加呈现先减小后增加的趋势,而随层理倾角θ增大表现为“U”型变化规律;与完整试样相比,双裂隙复合岩层峰值强度降低4.4%～42.0%;双裂隙复合岩层破坏模式主要分为5种类型,分别为轴向张拉破坏(Ⅰ型)、穿层理剪切破坏(Ⅱ型)、穿层理拉伸破坏(Ⅲ型)、沿层理面滑移破坏(Ⅳ型)、沿岩层拉伸破坏(Ⅴ型);试样的破坏模式在θ=0°～45°时随岩桥倾角增加从Ⅰ型转变为Ⅱ型最后转变为Ⅲ型破坏模式,在θ=60°～75°和θ=90°时分别表现为Ⅳ型和Ⅴ型破坏模式;在θ=0°～45°时,翼裂纹垂直于主裂隙起裂,随岩桥倾角增大,翼裂纹沿岩桥倾角偏转并扩展成宏观破裂面,导致试样最终被破坏;在θ=60°～75°时,裂纹在层理面扩展形成宏观滑移面,导致试样破坏;在θ=90°时裂纹...     

坪湖矿岩溶洞探测及其采动作用下的概化模型

为更好地研究煤层开采对岩溶塌陷的影响,保护岩溶地区地质环境.本文对坪湖矿区阳坑村下的岩溶洞进行了探测分析,根据岩溶洞与主采煤层的相对位置,分别建立了采动作用下上覆岩溶洞塌陷的4种概化模型,并根据概化模型对采动引起岩溶塌陷的原因进行了分析.根据所建立的岩溶洞塌陷概化模型对坪湖矿井田范围内1#和6#塌陷坑塌陷机理进行分析,其塌陷原因是岩溶洞处于岩层弯曲下沉过程中的拉伸区域以及岩溶洞上方覆盖层较薄引起的.本文的研究为在喀斯特地区进行煤炭资源的地下开采,预防采场上方覆岩溶塌陷提供了理论依据.