巴基斯坦信德省下印度河盆地煤层气资源概况

Adeel Nazeer, S. HabibShah, Abbasi Sa, Solangi Sh, N. Ahmad
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引用次数: 2

摘要

巴基斯坦是一个能源匮乏和不发达的国家,但它拥有广泛的低质量煤炭资源。近年来,由于粉河流域(PRB)商业煤层气活动的增长,低煤阶煤层气(CBM)的同期模型发生了巨大变化。CBM模型仍在不断发展,因为CBM评价概念是基于经过验证和测试的商业活动的陡峭学习曲线。煤是一种不同寻常的岩性,它既是一种很好的烃源岩,又是一种很好的储集岩。在印度Cambay盆地也发现了具有商业储量的煤层气资源。坎贝盆地和粉河盆地(PRB)的煤层气资源在年龄和等级上与巴基斯坦大部分煤炭相似。上述盆地的成功促使巴基斯坦的地球科学家重新审视信德省的煤层气资源。该煤被认为是巴基斯坦储量最大的低等级煤。开展了初步地质调查;结果表明,信德省存在褐煤B ~高挥发分烟煤B级低阶煤层。上述等级为粉河矿区质量较好,值得进一步评价,以确定进一步勘探和后续开采。几口井之间的相互电缆相关性已经明确地进行了。结果表明,拉基组Bara段(古新世)和Sonari段(始新世)在地下数公里处存在孤立煤层。该区煤层厚度最大,瓦斯吸附能力较好。煤层气专项研究还表明,在Badin、Sonda、Thatta和Jherruck地区存在烟煤。利用板块重建技术,建立了该矿床的沉积模型。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
An Overview of CBM Resources in Lower Indus Basin, Sindh, Pakistan
Pakistan is energy deficient and underdeveloped country but it contains wide resources of low quality coal. The contemporaneous models for Coal Bed Methane (CBM) in low-rank coals have changed dramatically in recent years due to the growth of commercial CBM activity in the Powder River Basin (PRB). The CBM models are still evolving because the CBM evaluation concepts are on steep learning curve based on proven and tested commercial activities. Coal is an unusual lithology in that it is both an excellent source and reservoir rock. CBM resource has also been found in commercial quantities in the Cambay Basin of India. The CBM resource of Cambay Basin and Powder River Basin (PRB) are similar in age and rank to most of Pakistan’s coal. The success in the above mentioned basins provoked geoscientists in Pakistan to re-look into Sindh`s CBM resource. Thar coal is considered as the largest reserves of low ranking coal in Pakistan. Preliminary geological investigation was carried out; results show that low ranked coal seams of class Lignite B to High Volatile B bituminous coal exists in Sindh. The rank specified above is better in quality from Powder River Coal Deposits, so it warrants further evaluation to firm up further exploration and subsequent exploitation. Interactive wireline correlations between several wells have been carried out explicitly. Results show that isolated coal seams of Bara Member (Paleocene) and Sonari Member of Laki Formation (Eocene) exists a few kilometers in sub-surface. The thickness of coal seams is thickest in Thar area with better prospect for gas adsorption capacity. The dedicated CBM studies also reveal that the bituminous coal exists in Badin, Sonda, Thatta and Jherruck areas. Depositional Model of Thar coal deposit has been prepared using plate reconstruction.
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