松辽盆地北部大庆长垣南端上白垩统四方台组物源体系分析

肖鹏; 金若时; 汤超; 刘华健; 邓永辉; 魏佳林; 徐增连

doi:10.11781/sysydz201804493

松辽盆地北部大庆长垣南端上白垩统四方台组物源体系分析

doi: 10.11781/sysydz201804493

肖鹏^1,2,
金若时^1,2,
汤超^1,2,
刘华健^1,2,
邓永辉³,
魏佳林^1,2,
徐增连^1,2

1. 中国地质调查局天津地质调查中心, 天津 300170;
2. 中国地质调查局天津地质调查中心非化石能源矿产实验室, 天津 300170;
3. 中海石油(中国)有限公司深圳分公司, 广东深圳 518000

基金项目:

国家重点基础研究发展计划（973计划）（2015CB453000）和中国地质调查局地质调查项目（DD20160128）联合资助。

详细信息

作者简介:
肖鹏(1988-),男,硕士,工程师,从事砂岩型铀矿地质调查研究。E-mail:394653105@qq.com。

中图分类号: TE121.3
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- 被引次数: 0
出版历程
- 收稿日期: 2017-10-24
- 修回日期: 2018-05-28
- 刊出日期: 2018-07-28

Provenance system of the Late Cretaceous Sifangtai Formation in the south of Daqing placanticline of the northern Songliao Basin

1. Tianjin Center, China Geological Survey, Tianjin 300170, China;
2. Laboratory of Non-fossil Energy Minerals, Tianjin Center of China Geological Survey, Tianjing 300170, China;
3. CNOOC Shenzhen Branch, Shenzhen, Guangdong 518000, China

摘要

摘要: 物源体系制约着层间水的流动方向及砂体储层的展布。前人对松辽盆地北部上白垩统物源体系分析多集中在四方台组以下，缺乏对四方台组物源的报道。因此，在结合区域地质认识的基础上，通过沉积构造分析、砂体展布形态及重矿物分析等手段，系统研究了松辽盆地北部大庆长垣南端四方台组物源体系特征，明确了物源方向与母岩类型。结果表明，四方台组地层的母岩类型主要为中酸性岩浆岩与中高级变质岩；通过与源区对比分析，认为大庆长垣南端四方台组物源主要来自张广才岭、吉黑东部及盆地东南部地区。
- 物源体系 /
- 四方台组 /
- 上白垩统 /
- 大庆长垣南端 /
- 松辽盆地北部
Abstract: The provenance system restricted the flow direction of interlayer water and the distribution characteristics of sandstone reservoirs. The previous analysis of the upper Cretaceous provenance system in the northern Songliao Basin was focused below the Sifangtai Formation, and there was a lack of reports on the origin of the Sifangtai Formation. We systematically studied the characteristics of source systems of the Sifangtai Formation at the southern end of Daqing placanticline in the northern Songliao Basin using regional geological understanding, through sedimentary structural analysis, sand body distribution pattern and heavy mineral analysis, and identified the source direction and parent rock type. The results showed that the main parent rocks of the Sifangtai Formation are intermediate acid magmatic rocks and intermediate and high-grade metamorphic rocks. Through contrast analysis with the source regions, it was concluded that the provenance of the Sifangtai Formation in the south of Daqing placanticline was mainly from the Zhangguangcai Ranges, the eastern Jilin-Heilongjiang provinces and the southeastern region of the basin.
- provenance system /
- Sifangtai Formation /
- Upper Cretaceous /
- southern Daqing placanticline /
- northern Songliao Basin

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