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首页> 外文期刊>New Zealand journal of geology & geophysics >Coal rank, coal type, and marine influence in the north Taranaki coalfields, New Zealand
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Coal rank, coal type, and marine influence in the north Taranaki coalfields, New Zealand

机译:新西兰北部塔拉纳基煤田的煤位,煤类型和海洋影响

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A few coal seams in the thin early Miocene Maryville Coal Measures have been mined in the relatively minor north Taranaki coalfields: Mokau, Ohura, Tangarakau, Waitewhena, and Aria. Generally accepted as sub-bituminous, the coals are discussed in terms of the Rank(S_r) classification to identify more closely the variations of coal type and coal rank. The use of a mineral-matter- and sulphur-free basis for the analyses is made necessary by the generally moderate to high sulphur contents. The range of volatile matter is 15%, and of calorific value is 1500 Btu/lb (= 3.5 MJ/kg specific energy). In the most closely explored coalfield, Mokau, c. 450 coal analyses from up to 5 seams in 130 drillholes over an area of c. 65 km~2 have been used. Analyses from 27 seam sections in Tatu Mine (Tangarakau Coalfield) come from an area of c. 2.5 km~2. Analyses from a few mines in Waitewhena and Aria Coalfields, and from widely spaced drillholes in Waitewhena, Ohura, and Tangarakau Coalfields, provide additional data. In Mokau Coalfield, a detailed pattern of lateral rank variation is demonstrated within a Rank(S_r) range from 6.6 to 8.1. The rate of lateral rank variation, up to 1.5 Rank(S_r)/km, is too rapid to result from depth of burial variation. The rank variation is tentatively ascribed to localised differential heating as a result of fluid movement up faults during minor disruption of the downwarping basin at the end of Miocene sedimentation when the coal ranks were imprinted. Such disruption may have produced the older north-trending faults; the dominant younger east-northeast-trending faults are likely to have formed during uplift after the rank pattern was established. The lower ranks over most of the region are considered to indicate the general depth of burial, c. 1.7 km, but a regional decrease in rank along the eastern margin and in the northeast at Aria indicates a probable regional decrease in thickness of the former cover to c. 1.25 km.
机译:在塔拉纳基北部相对较小的煤田,较薄的中新世马里维尔早期煤系中已经开采了一些煤层:莫考,奥胡拉,坦加拉考,怀特韦纳和阿里亚。煤通常被认为是次烟煤,将根据Rank(S_r)分类对煤进行讨论,以更紧密地识别煤类型和煤等级的变化。由于硫含量通常中等到高,因此有必要使用不含矿物质和硫的基础进行分析。挥发性物质的范围是15%,热值是1500 Btu / lb(= 3.5 MJ / kg比能)。在最受勘探的煤田莫考c。在c区域的130个钻孔中,最多5个煤层进行450份煤分析。已经使用了65 km〜2。塔图矿(Tangarakau Coalfield)的27个煤层剖面的分析来自c区。 2.5公里〜2。来自Waitewhena和Aria Coalfields的一些矿山,以及Waitewhena,Ohura和Tangarakau Coalfields的大间距钻孔的分析提供了其他数据。在Mokau Coalfield中,在6.6至8.1的Rank(S_r)范围内证实了横向秩变化的详细模式。横向等级变化率高达1.5 Rank(S_r)/ km,该速率太快而无法由埋葬变化深度引起。等级变化暂时归因于局部差异加热,这是由于在中新世沉积末期当煤阶被印记时,向下翘曲盆地的轻微破坏期间流体向上运动的断层所致。这种破坏可能产生了较旧的向北断裂。确定等级模式后,在隆升过程中可能形成了较年轻的东西东向断裂。在该地区大部分地区,较低的等级被认为表明了一般的墓葬深度,c。 1.7 km,但是沿Aria的东部边缘和东北部的区域等级减小表明前盖厚度可能减小到c。 1.25公里

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