兰州城市学院培黎石油工程学院;西安科技大学地质与环境学院;西北大学地质学系;
鄂尔多斯盆地西部下古生界奥陶系因油气勘探潜力大一直备受关注。其中,中奥陶统克里摩里组发育的碳酸盐岩有望成为下一个勘探目标层,因此,对其沉积特征进行深入剖析可以为西缘奥陶系天然气勘探提供地质依据。通过野外剖面考察、岩心观察和薄片鉴定等手段,研究了克里摩里组的岩石学特征、沉积相类型及其空间展布规律。结果表明,克里摩里组岩性主要为薄层泥晶灰岩、砾屑、砂屑、粉屑灰岩、(含)生物碎屑灰岩及黑色页岩。泥晶结构、粒屑结构发育可见薄层状、纹层状、瘤状、角砾状构造和滑塌及鲍马层序。沉积相类型以台地前缘斜坡和深水斜坡海槽发育为主要特征,表现为沿南北向呈狭窄的条带状展布,在自东向西方向上,紧邻鄂尔多斯本部的开阔海台地发育台地前缘斜坡相带,向西迅速相变为深水斜坡海槽相,海水具有逐渐加深的趋势。
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基本信息:
DOI:10.16152/j.cnki.xdxbzr.2024-06-006
中图分类号:P618.13
引用信息:
[1]欧阳征健,冯娟萍,姚韦卓等.鄂尔多斯盆地西部中奥陶统克里摩里组沉积特征研究[J].西北大学学报(自然科学版),2024,54(06):1004-1012.DOI:10.16152/j.cnki.xdxbzr.2024-06-006.
基金信息:
甘肃省高校教师创新基金(2025B-8); 兰州城市学院艾黎学科建设计划项目