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鄂尔多斯盆地中部奥陶系风化壳天然气的运移特征
Migration characteristics of Ordovician weathered crust natural gas in central Eerduosi Basin
【摘要】 鄂尔多斯盆地中部奥陶系风化壳天然气运移是迄今研究比较薄弱的重要问题 .在前人工作的基础上 ,依据实际的地质和地球化学资料 ,分析了鄂尔多斯盆地中部奥陶系风化壳天然气的运移特征 .研究认为 ,以靖边为中心的中部气区是天然气运移的有利区 .奥陶系风化壳天然气的运移较为复杂 ,既有奥陶系来源天然气的侧向运移 ,又有上覆石炭—二叠系来源天然气的穿层运移 .这与研究区的构造演化、古流体等研究结果相吻合
【Abstract】 On the basis of previous works and a lot of actual geological and geochemical data, the migration characteristics of natural gas from Ordovician weathered crust in central Eerduosi Basin are analyzed. The analysis result shows that the middle part (around Jingbian) of Eerduosi Basin is the favorable area for natural gas migration and accumulation. It’s held that the Ordovician weathered crust natural gas can migrate laterally from Ordovician carbonates and vertically from Upper Paleozoic source rocks. These conclusions are consistent with the regional tectonic evolution and the studies of paleo-fluid in Eerduosi Basin.
【Key words】 central Eerduosi Basin; Ordovician weathered crust; natural gas migration, gas reservoir; geological geochemistry;
- 【文献出处】 西安石油大学学报(自然科学版) , 编辑部邮箱 ,2004年01期
- 【分类号】P618.13
- 【被引频次】6
- 【下载频次】365