鄂尔多斯盆地中央古隆起与天然气聚集 |
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引用本文: | 汤显明,惠斌耀.鄂尔多斯盆地中央古隆起与天然气聚集[J].石油与天然气地质,1993,14(1):64-71. |
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作者姓名: | 汤显明 惠斌耀 |
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作者单位: | 长庆石油勘探局勘探开发研究院,长庆石油勘探局勘探开发研究院 甘肃 庆阳745101,甘肃 庆阳745101 |
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摘 要: | 鄂尔多斯盆地中央古隆起可以划分为中部凸起剥蚀区、西翼陡坡区、东翼缓坡区、北翼平缓北倾区、南翼陡缓变化区.经历了前加里东期、加里东期、海西期、燕山期几个发育阶段.古隆起的构造发育与烃源岩热演化配置良好.其东翼靖边-志丹-富县区为 Ⅰ 类远景区;北翼定边-天池区次之;西翼陡坡区较差.主要储集层是奥陶系顶部风化淋滤带.
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关 键 词: | 鄂尔多斯盆地 中央古隆起 构造发展史 天然气远景评价 奥陶系 |
THE CENTRAL UPLIFT OF ORDOS BASIN AND ITS GAS ACCUMULATION |
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Abstract: | The central uplift of Ordos Basin is located in Wuqi-Qingyang-Fuxian region and could be divided into steep slope area in the west flank,eroded area in central uplift,gen-tle slope area in the east flank,gentle slope in the north flank and steep-gentle changing area in the south flank.The uplift underwent Pre-Caledonian,Caledonian,Hercynian,Yenshan and etc.evolution periods.The uplift is close to two gas generation centers of Or-dovician,Permo-Carboniferous Systems,which provide rich gas-sources for the east flank slope area,thus the uplift is favourable in seeking for weathered-crust and other subtle traps.The bauxite of Middle Carboniferous Benxi Formation can be direct seal,and Per-mian argillaceous rocks may act as regional seals.Hence Jingbian-Zhidan-Fuxian area in the east flank of the uplift is most favorable for gas exploration,then Dingbian-Tianchi,the west steep slope is the reserve area. |
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