Source Rock Potential of Chichali and Samana Suk Formations Deposits in Panjpir Oilfield Subsurface, Punjab Platform, Pakistan

Syed Bilawal Ali Shah, Syed Bilawal Ali Shah, Adeeb Ahmed, Muhammad Nofal Munir
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引用次数: 1

Abstract

By using total organic carbon (TOC) and Rock-Eval pyrolysis analysis measurements, the  hydrocarbon source rock potential of Chichali and Samana Suk formations found in the subsurface of Panjpir oilfield in Punjab platform located in the eastern part of the middle Indus Basin was investigated. Twenty two core samples were collected from producing well. The analysed samples of Chichali formation contains TOC ranging between 0.99-4.61 wt.% having average TOC of 1.51 wt.% and the S2 values of Rock-Eval show the poor to fair generative potential with values ranging from 0.99-3.08 mg HC/g rock. The samples have low hydrogen index values ranging from 21-302 mg HC/g TOC and also most of the samples have low T_(max ) values ranging from 422-432 °C and have OI values ranging from 15-82 mg CO2/g TOC. Samana Suk formation samples have TOC ranging between 0.28-1.38 wt.% having average TOC of 0.84 wt.%. S2 values of Rock-Eval shows poor generative potential with values ranging from 0.05-2.99 mg HC/g rock. The samples have low hydrogen index values ranging from 13-322 mg HC/g TOC and T_(max) values ranging from 423-435 °C, and have OI values ranging from 41-182 mg CO2/g TOC. On the basis of analysis performed only one sample from Chichali and five samples of Samana Suk formations have entered early maturity zone, while all remaining samples lie in immature zone as indicated by HI vs T_(max) plot. HI vs OI plot and HI vs T_ (max) indicates the presence of kerogen Type III. All of the samples from Samana Suk formation shows poor generative potential as compared to Chichali formation having fair generative potential as indicated by S2 vs TOC plot. Hence, from the results some minor gas could be expected to have been generated from Chichali formation in Panjpir oilfield subsurface.
巴基斯坦旁遮普省Panjpir油田地下Chichali和Samana Suk组烃源岩潜力
通过总有机碳(TOC)和rock - eval热解分析测量,对位于印度河中东部Panjpir油田地下的Chichali和Samana Suk组烃源岩潜力进行了研究。从生产井采集岩心样品22个。Chichali组的TOC含量在0.99 ~ 4.61 wt.%之间,平均TOC为1.51 wt.%,岩石- eval的S2值在0.99 ~ 3.08 mg HC/g岩石之间,显示出较差到一般的生成潜力。样品的氢指数较低,范围为21 ~ 302 mg HC/g TOC,大部分样品的T_(max)值较低,范围为422 ~ 432℃,OI值为15 ~ 82 mg CO2/g TOC。Samana Suk地层样品的TOC含量范围为0.28-1.38 wt.%,平均TOC含量为0.84 wt.%。岩石- eval的S2值为0.05 ~ 2.99 mg HC/g岩石,显示出较差的生成潜力。样品的低氢指数为13 ~ 322 mg HC/g TOC, T_(max)值为423 ~ 435℃,OI值为41 ~ 182 mg CO2/g TOC。根据HI - T_(max)图,仅有Chichali组1个样品和Samana Suk组5个样品进入早熟区,其余样品均处于未成熟区。HI / OI图和HI / T_ (max)表明存在ⅲ型干酪根。S2 / TOC图显示,与具有良好生成潜力的Chichali组相比,Samana Suk组的所有样品都显示出较差的生成潜力。因此,从结果来看,可以预计Panjpir油田Chichali组地下产生了少量天然气。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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