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机构地区:[1]中国石油勘探开发研究院,北京100083 [2]中国石油勘探开发研究院廊坊分院,河北廊坊065007
出 处:《天然气地球科学》2011年第4期635-641,共7页Natural Gas Geoscience
基 金:国家"大型油气田及煤层气开发"科技重大专项(编号:2008ZX05)资助
摘 要:柴达木盆地三湖地区第四系的形成是在第三纪末期新构造运动作用下,盆地沉积中心由西向东整体迁移的产物,在第四系中发现了世界上最大的生物气田。近年来三湖地区发现岩性气藏,将现已发现的岩性气(层)藏分为砂岩上倾尖灭型、砂岩透镜体型和物性侧向变化型3种。并提出岩性气藏分布规律是:分布于北斜坡,依附于构造背景,位于k9标志层以下,赋存于薄层砂体中,限于一定的深度范围内。根据分布规律,提出三湖地区岩性气藏的有利勘探区块,为研究区下一步进行岩性气藏勘探提供了理路依据和现实依据。The occurrence of the Quaternary in Sanhu area of Qaidam basin, which has trapped the largest biologic gas field,is the product of migration of basin depositional center from west to east under the tectonic movements at the end of Tertiary. In recent years,lithologic gas reservoirs have been found in this area and been divided into three types including sand updip pinch-out, sand lens and sand property change in the lateral direction. The distribution regularities of lithologic gas reservoirs in the Sanhu area are summarized as distribution in the northern slope, development on the tectonic background, location below the marker bed kg,accumulation in thin sandstone and limitation to a certain depth. At last, according to the distribution regularity of lithologic gas reservoir, the authors point out favorable exploration areas of lithologic gas reservoir. This study has important theoretical and practical significances for lithologic gas reservoirs exploration in the Sanhu area of Qaidam basin.
分 类 号:TE122.24[石油与天然气工程—油气勘探]
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