首页> 外文OA文献 >Geologi am dan pencirian geomekanik batuan formasi Crocker untuk kesesuaian sebagai bahan binaan di kawasan Penampang-Inanam
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Geologi am dan pencirian geomekanik batuan formasi Crocker untuk kesesuaian sebagai bahan binaan di kawasan Penampang-Inanam

机译:地质学家am dan pencirian geomechanic batuan formasi crocker untuk kesesuaian sebagai bahan binaan di kawasan penampang-Inanam

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摘要

"The study area is located in Kota Kinabalu area which is along Inanam to Penampangudcovering an area approximately about 100 kilometre square and bounded by the latitudeud05°53'N to 05°57'N and longitude 116°05'E to 116°11'E. The objectives of this researchudare to study the geologicabl ackgrounda nd producel atest geologicalm ap, to analyser ockudgoemechanicsc haracterizationin perspectiveo f rock aggregatet ests on study area andudto assess the suitability of rocks in study area as potential construction materials. Theudstudy consists of the Crocker Formation and the Quartemary Alluvium. The CrockerudFormation aged from Late Eocene to Early Miocene consists of four rock units include grey shale, red shale, thick sandstone and interbedded sandstone with shale. From petrographic analysis, quartz is the dominant mineral in sandstone that is 58%-59% followed by matrix compound that is 21%-23%. Other compound are rock fragment 10%- 17% and feldspar about 4%-8%. Structural geology analysis of the lineamen shows the direction of tectonismi s Northwest- Southeast.I n geomechanicste st such as point load test, Los Angeles abrasion test, aggregate impact value and 10% fines value show sandstone sample that is Ki is the toughest followed by the slake durability test and aggregate crushing value shows sandstone sample that is H2 is the toughest and the uniaxial compression strength show that sandstone sample that is Si is the toughest. All the tests give values that can be implement on the standard of Public Work Department and suitable to be used as construction materials.
机译:“研究区域位于亚那南(Inanam)至Penampang的亚庇(Kota Kinabalu)地区,发现大约100平方公里的地区,并以北纬ud05°53'N至05°57'N和东经116°05'E为界116°11'E。这项研究的目的是要研究地质基础和生产测试地质学,以分析研究区域岩石聚集体的岩石岩石力学力学特性,并 ud以评估岩石在研究区域的适用性。研究的对象包括克罗克组和四方冲积层,从始新世晚期到中新世早期的克罗克组由四个页岩单元组成,分别是灰色页岩,红色页岩,厚砂岩和夹层砂岩和页岩。分析表明,石英是砂岩中的主要矿物,占58%-59%,其次是基质化合物,占21%-23%;其他化合物是岩石碎屑,占10%-17%,长石约占4%-8%。线形的分析表明构造方向是西北-东南方向。在点荷载试验,洛杉矶磨蚀试验,总冲击值和10%细度值等地质力学试验中,Ki砂岩样品最坚硬,其次是碱土耐久性试验和骨料破碎值表明,H2砂岩样品最坚硬,单轴压缩强度表明Si砂岩样品最坚硬。所有测试给出的值均可以按照公共工作部门的标准执行,并且适合用作建筑材料。

著录项

  • 作者

    Mohd Taufik Khalid;

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  • 年度 2014
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  • 原文格式 PDF
  • 正文语种 en
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