Organic geochemical characteristics of the Late Cretaceous coal and carbonaceous shale succession from the Taranaki Basin, New Zealand: Implications for sedimentary environmental setting and petroleum generation potential

IF 1.4 4区 地球科学 Q3 GEOSCIENCES, MULTIDISCIPLINARY
Geological Journal Pub Date : 2024-04-23 DOI:10.1002/gj.4962
Mahdi Ali Lathbl, Akm Eahsanul Haque, Mohammed Hail Hakimi, Aref Lashin, S. M. Talha Qadri
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Abstract

This comprehensive study investigates the organic matter characteristics within the Late Cretaceous Rakopi and Taniwha formations, based on data from four exploration wells situated in New Zealand's Taranaki Basin. It employs a multifaceted approach, integrating bulk geochemical analyses, biomarker measurements and carbon isotopes to unveil the geological history of these formations. Analytical results include total organic carbon content, ranging from 7.27 to 75.78 wt%, and generation potentials spanning from 28.24 to 309.16 mg hydrocarbon/g rock. These observations underscore the source rock potential of these Late Cretaceous strata. These rocks show a mixed organic matter of hydrogen-rich Type II and Type II/III kerogens, as evidenced by hydrogen index values (HI) between 237 to 428 mg hydrocarbon/g rock. These formations demonstrate promise potential for both oil and gas generation. Biomarker analysis uncovers distinct signatures, featuring a pristane/phytane (Pr/Ph) ratio ranging from 3.27 to 10.91, a Tm/Ts ratio surpassing 7 and elevated concentrations of C29 regular steranes relative to C27 and C28 regular steranes. These biomarker characteristics suggest a composite organic matter composition, influenced by terrigenous organic matter, likely deposited in oxygenated fluvial deltaic environments. Bulk carbon isotopic data corroborate these findings, highlighting the abundance of terrigenous organic matter. Collectively, these insights reveal that the coal and carbonaceous shale intervals in the examined wells are in the early stages of oil generation. Therefore, the Rakopi and Taniwha formations have not yet yielded commercially viable oil and/or gas quantities. In this case, these formations hold substantial promise for future exploration activities in relatively deep wells, with limited oil expulsion from coals.

Abstract Image

新西兰塔拉纳基盆地晚白垩世煤和碳质页岩演替的有机地球化学特征:对沉积环境背景和石油生成潜力的影响
这项综合研究以新西兰塔拉纳基盆地四口勘探井的数据为基础,调查了晚白垩世拉科比地层和塔尼瓦地层的有机物特征。该研究采用了一种多方面的方法,综合了大量地球化学分析、生物标记测量和碳同位素,以揭示这些地层的地质历史。分析结果包括总有机碳含量(从 7.27% 到 75.78%)和生成潜力(从 28.24 到 309.16 毫克碳氢化合物/克岩石)。这些观察结果凸显了这些晚白垩世地层的源岩潜力。这些岩石显示出富含氢的第二类和第二/三类角砾岩的混合有机质,氢指数值(HI)介于 237 至 428 毫克碳氢化合物/克岩石之间。这些地层显示出有望产生石油和天然气。生物标志物分析揭示了独特的特征,其特点是pristane/phytane(Pr/Ph)比率在 3.27 到 10.91 之间,Tm/Ts 比率超过 7,C29 正甾烷的浓度高于 C27 和 C28 正甾烷。这些生物标志物特征表明,这里的有机物成分是一种复合有机物,受到土著有机物的影响,很可能沉积在含氧的三角洲河流环境中。大量碳同位素数据证实了这些发现,凸显了土著有机物的丰富性。总之,这些发现揭示了所考察油井中的煤层和碳质页岩层处于石油生成的早期阶段。因此,拉科比地层和塔尼瓦地层尚未产出具有商业价值的石油和/或天然气。在这种情况下,这些地层为今后在相对较深的油井中开展勘探活动带来了巨大希望,因为煤炭的石油排出量有限。
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来源期刊
Geological Journal
Geological Journal 地学-地球科学综合
CiteScore
4.20
自引率
11.10%
发文量
269
审稿时长
3 months
期刊介绍: In recent years there has been a growth of specialist journals within geological sciences. Nevertheless, there is an important role for a journal of an interdisciplinary kind. Traditionally, GEOLOGICAL JOURNAL has been such a journal and continues in its aim of promoting interest in all branches of the Geological Sciences, through publication of original research papers and review articles. The journal publishes Special Issues with a common theme or regional coverage e.g. Chinese Dinosaurs; Tectonics of the Eastern Mediterranean, Triassic basins of the Central and North Atlantic Borderlands). These are extensively cited. The Journal has a particular interest in publishing papers on regional case studies from any global locality which have conclusions of general interest. Such papers may emphasize aspects across the full spectrum of geological sciences.
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