1. 西北大学地质学系大陆动力学国家重点实验室
2. 陕西延长石油(集团)有限责任公司天然气研究院分公司
3. 陕西延长石油(集团)有限责任公司气田公司
纸质出版:2025
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樊宇洁, 孟祥振, 蒲仁海, 等. 鄂尔多斯盆地延长探区本溪组物源分析[J]. 地质科技通报, 2025,44(3):197-211.
樊宇洁, 孟祥振, 蒲仁海, et al. 鄂尔多斯盆地延长探区本溪组物源分析[J]. Bulletin of Geological Science and Technology, 2025, 44(3): 197-211.
樊宇洁, 孟祥振, 蒲仁海, 等. 鄂尔多斯盆地延长探区本溪组物源分析[J]. 地质科技通报, 2025,44(3):197-211. DOI: 10.19509/j.cnki.dzkq.tb20240191.
樊宇洁, 孟祥振, 蒲仁海, et al. 鄂尔多斯盆地延长探区本溪组物源分析[J]. Bulletin of Geological Science and Technology, 2025, 44(3): 197-211. DOI: 10.19509/j.cnki.dzkq.tb20240191.
碎屑物质来源是控制鄂尔多斯盆地延长探区内本溪组砂岩储层发育和展布的重要因素之一。对延长探区内37口井砂岩和泥岩样品开展了碎屑锆石U-Pb年龄、重矿物组合、微量元素以及砂砾岩粒径统计等分析,揭示了本溪组碎屑物质的主要来源和搬运方向。研究表明探区内延528井的1 912 Ma和2 425 Ma 2个年龄峰值与华北克拉通北缘相对应,其他5口井的年龄峰值段435~447 Ma和952~976 Ma则与北秦岭的年龄峰值相对应,据此可将探区内物源划分为NE和S部2个方向。通过锆石、电气石和金红石等重矿物,可将S部物源进一步划分为WS和ES 2个方向;与重矿物分析结果相对应,在微量元素锆铌比分析中,存在WS陇东地区和ES豫西地区2个方向的物源;对砂砾岩粒径在平面上分布特征的显示,研究区存在来自ES方向的物源。综合分析可得,延长探区本溪组总体上可划分为NE、WS和ES 3个物源区,分别指示了盆地北缘阴山、盆地南缘祁连山和北秦岭东段剥蚀区,其中ES方向物源距延长探区最近,对探区影响较大。该成果探明了研究区内的3个物源方向以及其影响区域,对延长探区本溪组砂体分布预测和沉积相划分具有重要的参考意义。
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