岩性油气藏 ›› 2015, Vol. 27 ›› Issue (6): 2329.doi: 10.3969/j.issn.1673-8926.2015.06.004
张光伟1,潘树新1,魏浩元2,李伟2,张丽萍1,龙礼文1
Zhang Guangwei1, Pan Shuxin1, Wei Haoyuan2, Li Wei2, Zhang Liping1, Long Liwen1
摘要:
酒西盆地鸭儿峡白垩系砂(砾)岩储层发育良好,但目前针对其物源体系的认识还不清晰。 以酒西盆地鸭儿峡白垩系砂(砾)岩为研究对象,分析其稀土元素的有关参数,探讨柳北和鸭儿峡砂(砾)岩的物源及地球化学特征。 研究区白垩系砂(砾)岩各稀土元素质量分数小且无明显的差异,实验样品的稀土元素配分模式相同,均呈现轻稀土元素相对富集、重稀土元素相对贫乏且变化平缓的右倾模式; Eu 负异常明显,物源相似,均来自上地壳; Ce/Ce* 和 Ce anom 指数均显示酒西盆地白垩系沉积的古水介质为还原环境,这有利于油气的形成。 初步认为,柳北和鸭儿峡砂(砾)岩来自于同一物源体系。
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