PETROLEUM GEOLOGICAL FEATURES AND EXPLORATION POTENTIAL OF THE SERGIPE-ALAGOAS BASIN OF BRAZIL
-
摘要:
塞尔西培-阿拉戈斯盆地是巴西东部重要的含油气盆地,经历了3期构造-沉积演化阶段。根据已掌握的资料,全面总结了盆地的油气地质特征及油气成藏模式,预测了勘探方向:①盆地发育3套烃源岩,其中过渡期烃源岩最为重要,裂谷期次之,漂移期烃源岩生烃潜力最小。②盆地发育3套储层,分别为裂谷早期的三角洲-风成砂岩、裂谷晚期的河流-三角洲相砾质砂岩或砾岩和漂移期的浊积砂岩。目前3套储层均已证实。③最终优选出2套潜力层系的有利区带:盐下裂谷层系有利区带在北部和中央隆起带; 盐上漂移层系有利区带在塞尔西培次盆地南部深水以及Sao Francisco河口外深水区域。
-
关键词:
- 塞尔西培-阿拉戈斯盆地 /
- 油气地质 /
- 勘探方向 /
- 巴西 /
- 含油气盆地
Abstract:The Sergipe-Alagoas Basin is an important petroliferous basin in eastern Brazil, and has undergone three tectonic and sedimentary evolution stages. According to the data available, petroleum geological features and the hydrocarbon accumulation model of the basin are comprehensively summarized, and the exploration potential predicted in this paper. ①There are three sets of source rocks developed in the basin, of which the source rocks formed in the transitional period are the most important, followed by that formed in the rift period. The source rock deposited in the drift period is the one with lowest hydrocarbon generation potential. ②There are three sets of reservoirs confirmed in the basin, i.e. the deltaic-aeolian sandstone deposited in the early rift period, the fluvial-deltaic pebbly sandstone or conglomerate in the late rift period, and the sandstone in the drift period. ③Finally, two favorable exploration zones are predicted, which includes the favorable zone of the subsalt rift system in the north of the basin and on the central uplift, and the favorable zone of the drift system in the deep water of the southern part of the Sergipe sub-basin and deep water area outside the Sao Francisco river mouth.
-
-
[1] 朱伟林, 白国平, 胡根成, 等.南美洲含油气盆地[M].北京:科学出版社, 2012:300-305.
[2] 高兴, 朱毅秀, 杨程宇.巴西塞尔西培-阿拉戈斯盆地油气地质特征[J].内蒙古石油化工, 2011, 37(15):113-115. doi: 10.3969/j.issn.1006-7981.2011.15.058
[3] Kifumbi C, Santos S, Claiton M, et al. High resolution stratigraphy of initial stages of rifting, Sergipe-Alagoas Basin, Brazil[J]. Brazilian Journal of Geology, 2017, 47:657-671. doi: 10.1590/2317-4889201720170003
[4] Hugo R, Felipe T, Luisa S, et al. Facies distribution as a response to early rift tectonic activity in the Sergipe-Alagoas Basin, northeastern Brazil[J]. Sedimentary Geology, 2019, 383:216-237. doi: 10.1016/j.sedgeo.2019.01.008
[5] Valle B, Dal' Bó P, Mendes M, et al. Stratigraphic evolution of a Brazilian carbonate platform during the Cretaceous: the late Albian-early Turonian of the Sergipe-Alagoas Basin[J]. Facies, 2019, 65:1-6. doi: 10.1007/s10347-018-0543-2
[6] Antonietto L, do Carmo D, Viviers M, et al. Ostracoda (Arthropoda, Crustacea) from the Riachuelo Formation, Sergipe-Alagoas Basin, Brazil, Upper Aptian-Albian[J]. European journal of taxonomy, 2016, 244:1-57.
[7] Melton B. A geological and geophysical study of the Sergipe-Alagoas Basin[D]. College Station: Texas A & M University, 2008.
[8] Jandyson M, Flávia M, Rennan G, et al. Chemical aspects of onshore crude oils from the Carmópolis Field, Sergipe-Alagoas Basin, Brazil:a case study on the industrial process for water-oil separation[J]. Energy and Fuels, 2015, 3:1315-1322.
[9] Kinoshita E. Seismic-geometric facies model of lacustrine carbonates of Morro do Chaves Formation, Sergipe-Alagoas Basin[J]. Boletim de Geociencias, 2010, 25:98-105.
[10] Antunes A, Francelino A. Applying filter and seismic attributes for enhancing faults in the 3D seismic survey of alto de Siririzinho (Sergipe-Alagoas basin, Northeast Brazil) [J]. Revista Brasileira De Geofísica, 2013, 31:109-123. doi: 10.22564/rbgf.v31i1.250
[11] IHS. Sergipe-Alagoas basin monitor [EB/OL].2019: 1-16.
[12] Angelica V, Meunier A. Burial and thermal conditions of diagenesis in the lower cretaceous barra de itiuba formation, Sergipe-Alagoas Basin, Brazil[J].Bulletin Society Geology France, 1996, 5:597-607.
[13] Mohriak W, Bassetto M, Vieira I. Crustal architecture and tectonic evolution of the Sergipe-Alagoas and Jacuipe basins, offshore northeastern Brazil[J].Tectonophysics, 1998, 288:199-220. doi: 10.1016/S0040-1951(97)00294-1
[14] Garry D, Stuart S, Jeffrey K. Modelling the tectonic development of the Tucano and Sergipe-Alagoas rift basins, Brazil [J].Tectonophysics, 1992, 215:133-160. doi: 10.1016/0040-1951(92)90078-K
[15] Destro N. Release fault: a variety of cross fault in linked extensional fault systems, in the Sergipe-Alagoas Basin, NE Brazil [J].Structural Geology, 1995, 5:615-629.
[16] Pinheiro J, Schnurle P, Evain M, et al. Lithospheric structuration onshore-offshore of the Sergipe-Alagoas passive margin, NE Brazil, based on wide-angle seismic data[J].Journal of South American Earth Sciences, 2018, 88:649-672. doi: 10.1016/j.jsames.2018.09.015
-