Jéssica Melanya Sisti de Paiva , Angélica Fortes Drummond Chicarino Varajão , Humberto Luis Siqueira Reis , Newton Souza Gomes , João F. Suss
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引用次数: 0
Abstract
This study presents the first comprehensive assessment of unconventional gas reservoirs in the Proterozoic sequences of the intracratonic São Francisco basin, providing depositional and post-depositional characterization and insights into reservoir quality. Detailed stratigraphic, petrological, and seismic analyses, integrated with 2D seismic data, were performed to evaluate the influence of diagenesis and hydrothermal fluids. The drill core was drilled in the central sector of the basin and within the southern border of the Pirapora aulacogen, in a 303 m-thick interval of the Paranoá-Upper Espinhaço sequence. The petrological analysis shows arkoses and sublitharenites as well as conglomerates, siltstones and mudstones successions deposited in deltaic, fluvial braided and marine depositional systems. Six sedimentary environments were identified, from the base to the top: (i) deltaic plain, (ii) delta front, (iii) braided fluvial, (iv) delta front, (v) prodelta and (vi) basin plain. The integration of seismic data review three depositional domains, characterized by lower frequency arranged to transgressive-regressive cycles identified by gamma ray, resistivity and density logs. The studied strata review eo - and mesodiagenetic alterations, being also influenced by intrusion-related hydrothermal and contact metamorphism. The main diagenetic events resulted in cementation of calcite (0.84%), chlorite (1.23%) and silica (6.19%), which largely obliterated porosity at the shallow burial depths. The main secondary porosity is intergranular, with minor contributions to intragranular, fracture, moldic and vugular. Diagenetic processes as well as the influence of hydrothermal processes highlight the complexity of post-depositional processes in these units. The presence of natural helium and hydrogen within the basin also suggests that these reservoirs should be considered in future exploration campaigns targeting unconventional energy resources.
本研究首次对 o Francisco盆地克拉通内元古代层序非常规气藏进行了综合评价,提供了沉积和沉积后特征,并对储层质量进行了深入了解。结合二维地震数据,进行了详细的地层、岩石学和地震分析,以评估成岩作用和热液流体的影响。钻探岩心位于盆地中部和皮拉波拉裂陷槽南部边界,位于Paranoá-Upper espinhaarso层序303 m厚的区间内。岩石学分析表明,在三角洲沉积体系、河流辫状沉积体系和海相沉积体系中,沉积有粗砂岩、次岩屑岩、砾岩、粉砂岩和泥岩等。从底部到顶部,确定了6种沉积环境:(i)三角洲平原,(ii)三角洲前缘,(iii)辫状河,(iv)三角洲前缘,(v)前三角洲和(vi)盆地平原。综合地震资料考察了三个沉积域,其特征是由伽马射线、电阻率和密度测井识别出的较低频率的海侵-海退旋回。所研究的地层受侵入体相关热液和接触变质作用的影响,具有古、中成岩作用。主要成岩事件是方解石(0.84%)、绿泥石(1.23%)和二氧化硅(6.19%)的胶结作用,这些胶结作用在很大程度上掩盖了浅埋深度的孔隙。次生孔隙主要为晶间孔隙,其次为晶内孔隙、断裂孔隙、模型孔隙和空洞孔隙。成岩作用和热液作用的影响突出了这些单元沉积后作用的复杂性。盆地内天然氦和氢的存在也表明,在未来的非常规能源勘探活动中应该考虑这些储层。
期刊介绍:
Papers must have a regional appeal and should present work of more than local significance. Research papers dealing with the regional geology of South American cratons and mobile belts, within the following research fields:
-Economic geology, metallogenesis and hydrocarbon genesis and reservoirs.
-Geophysics, geochemistry, volcanology, igneous and metamorphic petrology.
-Tectonics, neo- and seismotectonics and geodynamic modeling.
-Geomorphology, geological hazards, environmental geology, climate change in America and Antarctica, and soil research.
-Stratigraphy, sedimentology, structure and basin evolution.
-Paleontology, paleoecology, paleoclimatology and Quaternary geology.
New developments in already established regional projects and new initiatives dealing with the geology of the continent will be summarized and presented on a regular basis. Short notes, discussions, book reviews and conference and workshop reports will also be included when relevant.