共 50 条
The post-depositional evolution of Mesoproterozoic to early Neoproterozoic tight sandstone reservoirs, Sao Francisco basin, Brazil
被引:0
|作者:
de Paiva, Jessica Melanya Sisti
[1
]
Varajao, Angelica Fortes Drummond Chicarino
[1
]
Reis, Humberto Luis Siqueira
[2
,3
,4
]
Gomes, Newton Souza
[5
]
Suss, Joao. F.
[6
]
机构:
[1] Univ Fed Ouro Preto, Sch Mines, Campus Morro Cruzeiro, BR-35400000 Ouro Preto, MG, Brazil
[2] HR Consulting Energy & Geosci Ltda, Rua Nunes Vieira 35, BR-30350120 Belo Horizonte, MG, Brazil
[3] Univ Fed Minas Gerais, Comp Sci Dept, Campus Pampulha, BR-31270901 Belo Horizonte, Brazil
[4] Univ Fed Minas Gerais, Inst Geosci, Campus Pampulha, BR-31270901 Belo Horizonte, Brazil
[5] Fundacao Gorceix, Rua Carlos Walter Marinho Campos 57, BR-35400000 Ouro Preto, MG, Brazil
[6] Araunah Tech Solucoes Tecnol, Rua Presidente John Kennedy 237,Parque Amer, BR-38045210 Uberaba, MG, Brazil
关键词:
Siliciclastic rocks;
Diagenesis;
Proterozoic;
Unconventional reservoir;
Hydrothermal alteration;
U-PB;
BRASILIA BELT;
SEDIMENTARY PROVENANCE;
DEPOSITIONAL FACIES;
TECTONIC EVOLUTION;
ALKALI FELDSPARS;
PORE STRUCTURE;
CRATON REGION;
MINAS-GERAIS;
TARIM BASIN;
D O I:
10.1016/j.jsames.2024.105278
中图分类号:
P [天文学、地球科学];
学科分类号:
07 ;
摘要:
This study presents the first comprehensive assessment of unconventional gas reservoirs in the Proterozoic sequences of the intracratonic Sao 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 mthick interval of the Paranoa<acute accent>-Upper Espinha & ccedil;o 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.
引用
收藏
页数:21
相关论文