Geohistory Reconstruction and Maturity Modelling in the Southern Pletmos Basin, Offshore of South Africa

F. Agbor, S. Mhlambi, N. A. Teumahji, W. Sonibare, J. Donker, T. Chatterjee
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Abstract

Despite the undergoing exploration and research for hydrocarbons during the recent decades, the hydrocarbon potentials of existing source rock(s) in the Pletmos basin still remain enigmatic. The basin has undergone rifting and transforms processes during its evolution in a manner that its present-day architecture and geodynamic evolution can only be better understood through the application of a multidisciplinary and multi-scale geo-modelling procedure. In the study, thermal modelling and reconstruction of burial history of the source rocks in the southern depocenter of the Pletmos Basin has been investigated through an integration of data and methods. Through geohistory Modelling, an integration of the acquired multidisciplinary dataset allowed us to reconstruct the burial history, basement subsidence, vertical fluid flow, and the changes in rock properties (i.e. porosity, permeability, pressure and fluid flow rate) both in time and depth, as well as established a reliable tectonostratigraphic framework of the Mesozoic sedimentary infill. Then based on the reconstructed burial history, thermal history was reconstructed by modifying the paleoheat flux to minimize variances, and comparing between measured borehole and predicted vitrinite reflectance and Tmax (thermal indicator) values. These enable us to achieve an improved understanding of the subsurface controlling processes that might have led to the sedimentary infill and resulted to the heat-flow distribution and present-day thermal maturity of the source rocks in the Basin. The approach gives us the opportunity to considered the geodynamic evolution events from Mesozoic (Upper Jurassic) rifting to Cenozoic (including major uplifts, erosion and subsidence, and the Shona Buvet hot spots). Here we present some selected results, from the burial and thermal history modelling reconstructions of the sedimentary geothermal evolution and thermal maturity levels of the source rocks at selected well locations within the area. Likewise, this study has provided supplementary information that aids towards understanding the Petroleum System(s) of the Basin.
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南非近海南部Pletmos盆地地史重建与成熟度模拟
尽管近几十年来一直在进行油气勘探和研究,但Pletmos盆地现有烃源岩的油气潜力仍然是一个谜。盆地在演化过程中经历了裂谷和变形过程,只有应用多学科、多尺度的地质模拟程序才能更好地理解其现今的构造和地球动力学演化。本文采用数据与方法相结合的方法,对Pletmos盆地南部沉积中心烃源岩的热模拟与埋藏史重建进行了研究。通过地史模拟,整合多学科数据,重建了中生代沉积充填体的埋藏史、基底沉降、垂直流体流动以及岩石性质(孔隙度、渗透率、压力和流体流速)的时间和深度变化,建立了可靠的中生代沉积充填体构造地层格架。然后,在重建的埋藏史基础上,通过修正古热通量以减小方差,并将实测钻孔与预测镜质组反射率和Tmax(热指示值)进行比较,重建热历史。这使我们能够更好地了解可能导致沉积充填并导致盆地热流分布和现今烃源岩热成熟度的地下控制过程。该方法使我们有机会考虑从中生代(上侏罗统)裂谷到新生代(包括主要的隆升、侵蚀和沉降,以及Shona Buvet热点)的地球动力学演化事件。在这里,我们介绍了一些精选的结果,这些结果来自该地区选定井位的沉积地热演化和烃源岩热成熟度水平的埋藏和热历史模拟重建。同样,本研究也为了解盆地含油气系统提供了补充资料。
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