Timing of the Cenozoic magmatic intrusions in the offshore Tanga Basin, Tanzania: correlation to age equivalent deposits in the Eyasi-Wembere Basin and their implications for petroleum potential

IF 1.2 4区 地球科学 Q2 GEOLOGY South African Journal of Geology Pub Date : 2023-06-01 DOI:10.25131/sajg.126.0013
B. N. Mvile, E. B. Kiswaka, O. O. Osinowo, E. Mshiu, V. E. Mboya
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Abstract

The offshore Tanga Basin of north-eastern Tanzania contains Cenozoic sedimentary successions that have been poorly studied. The basin development was due to an interplay of multiple factors including periods of active fault movement linked to the East African Rift system (EARs) which influenced the Cenozoic development of the offshore Tanga Basin. The EARs recorded several discrete tectonic episodes that were associated with magmatic activities and massive volcanism. However, there is no report on the possible presence of magmatic intrusions indicative of magmatic activities and volcanism in the history of the Tanga Basin. Timing of occurrence and distribution of magmatic intrusions are among the key components needed to evaluate the petroleum potential of the basin. A detailed 2D qualitative seismic interpretation, coupled with core logging data and analysis of elemental proxies, has been employed to evaluate the petroleum potential of the Cenozoic successions of the offshore Tanga Basin considering the presence and timing of occurrence of the magmatic intrusions. These used data and the associated interpretation techniques have not been used before to meet similar objectives. Both core logging and elemental proxies are newly collected information used in this study. Results suggest that the Tanga Basin has been variedly intruded by magmatic sills and dikes. Seismic well tie and correlation to age-equivalent deposits across the onshore successions in the EWB revealed that the volcanic events occurred during tectonic episodes that influenced the development of the East African Rift basins. Seismic interpretation also suggests that these tectonic episodes occurred possibly during the Miocene, Pleistocene and Holocene periods when magmatic intrusions are believed to have promoted source rock maturation and facilitated the formation of structural elements for petroleum preservation.
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坦桑尼亚坦加盆地近海新生代岩浆侵入的时间:与Eyasi Wembere盆地年龄当量矿床的相关性及其对石油潜力的影响
坦桑尼亚东北部的近海坦加盆地包含新生代沉积序列,但研究较少。盆地的发展是由多种因素相互作用造成的,包括与东非裂谷系(EARs)有关的活动断层运动期,这影响了近海坦加盆地的新生代发展。EAR记录了几个与岩浆活动和大规模火山活动有关的离散构造事件。然而,没有关于坦噶盆地历史上可能存在岩浆活动和火山活动的岩浆侵入体的报告。岩浆侵入体的发生时间和分布是评估盆地石油潜力所需的关键组成部分。考虑到岩浆侵入体的存在和发生时间,采用了详细的2D定性地震解释,结合岩心测井数据和元素代理分析,来评估近海坦加盆地新生代序列的石油潜力。这些使用过的数据和相关的解释技术以前从未用于实现类似的目标。岩心测井和元素代理都是本研究中新收集的信息。结果表明,坦噶盆地受到岩浆岩床和岩墙的不同侵入。EWB陆上序列的地震井联系和与年龄等效矿床的相关性表明,火山事件发生在影响东非裂谷盆地发展的构造期。地震解释还表明,这些构造事件可能发生在中新世、更新世和全新世时期,当时岩浆侵入被认为促进了烃源岩的成熟,并促进了石油保存结构元素的形成。
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来源期刊
CiteScore
3.60
自引率
5.60%
发文量
18
审稿时长
>12 weeks
期刊介绍: The South African Journal of Geology publishes scientific papers, notes, stratigraphic descriptions and discussions in the broadly defined fields of geoscience that are related directly or indirectly to the geology of Africa. Contributions relevant to former supercontinental entities such as Gondwana and Rodinia are also welcome as are topical studies on any geoscience-related discipline. Review papers are welcome as long as they represent original, new syntheses. Special issues are also encouraged but terms for these must be negotiated with the Editors.
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