西安石油大学地球科学与工程学院;西安石油大学陕西省油气成藏地质学重点实验室;延长油田股份有限公司勘探开发技术研究中心;
鄂尔多斯盆地中侏罗统延安组是印支运动后滞效应后,受周缘造山带多物源系统影响的一套含煤碎屑岩地层,煤炭及油气等资源勘探潜力巨大。通过轻矿物、重矿物、古流向、主微量及稀土元素等进行物源分析,结合前人研究成果,开展了盆地延安组源-汇系统特征研究。结果表明,盆地延安组受来自北部阴山古陆、西北部阿拉善古陆、西南部祁连古陆及南部北秦岭造山带4个源-汇系统的影响。在源-汇系统分区的基础上深化了古地理格局认识,延安组在前侏罗纪沟壑纵横的地貌基础上,受4个不同古陆风化剥蚀搬运沉积过程差异的影响,形成了以盆地中部延安—东南部济源地区为沉积中心的陆相含煤碎屑岩沉积,自盆地边缘至汇水区,冲积扇-辫状河-曲流河-三角洲-湖泊沉积有序变化,其中以西北、北部源-汇系统沉积规模最大,是盆地勘探重点。研究结果对于深入理解不同物源体系影响下的各类储层特征及储层预测等具有理论和现实意义。
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基本信息:
DOI:10.16152/j.cnki.xdxbzr.2024-06-014
中图分类号:P618.13;P531
引用信息:
[1]袁珍,司豪杰,马瑶等.鄂尔多斯盆地侏罗系延安组源-汇系统特征及古地理格局[J].西北大学学报(自然科学版),2024,54(06):1104-1120.DOI:10.16152/j.cnki.xdxbzr.2024-06-014.
基金信息:
陕西省重点研发计划一般项目(2023-YBGY-079)