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作 者:郑一丁[1] 雷裕红[2] 张立强[1] 王香增[3,4] 张丽霞 姜呈馥[3,4] 程明 俞雨溪[2,5] 田飞 孙兵华[3,4]
机构地区:[1]中国石油大学(华东),山东青岛266580 [2]中国科学院油气资源研究重点实验室,中国科学院地质与地球物理研究所,北京100029 [3]陕西延长石油(集团)有限责任公司,陕西西安710075 [4]陆相页岩气工程研究中心,陕西西安710075 [5]中国科学院大学,北京100049
出 处:《天然气地球科学》2015年第7期1395-1404,共10页Natural Gas Geoscience
基 金:国家重点基础研究发展规划(“973”)项目(编号:2011CB201105);国家重大科技专项课题(编号:2011ZX08005-004);国家自然科学基金项目(编号:41102078)联合资助
摘 要:页岩厚度、总有机碳含量、脆性矿物含量、物性等是页岩储层评价的关键参数,明显受其沉积环境控制。因此,分析页岩形成过程中的沉积环境对页岩储层评价和甜点预测具有重要意义。系统测试了鄂尔多斯盆地中南部Y1井钻遇的张家滩页岩525组样品的40余种元素丰度,分析了其元素地球化学特征和页岩沉积环境的古气候、古水深、古盐度、古生产力、氧化还原特征。结果表明,自下而上张家滩页岩元素的丰度和比值呈周期性变化,指示其形成于温暖湿润、淡水—微咸水、缺氧等沉积环境,其中4单元发育在最潮湿的沉积环境,当时的水体最深、还原性最高,具有较高的古生产力。Shale thickness, total organic carbon content, brittle mineral content and physical property are key parameter of shale reservoir evaluation, which are obviously controlled by the sedimentary environment. Therefore,it's significant to study the sedimentary environment and the evolution of the shale formation a- bout gas reservoir evaluation and desserts prediction. This paper systematically tested more than 40 ele- ment concentrations of 525 groups of samples in Zhangjiatan shale drilled by well Y1 in the South-Central Ordos Basin. Then we analyzed the evolution of the paleoclimate, the paleobathymetry, the paleosalinity, the paleoproductivity and the oxidation-reduction states of sedimentary environment. The results showed that there are significant periodical changes of the element concentrations and ratios of Zhangjiatan shale from bottom to top, indicating that Zhangjiatan shale was deposited in a warm and humid, freshwater- brackish, hypoxia sedimentary environment, between which, the @ unit was deposited in a wet sedimentary environment,when the water was deepest and highest reducing with high paleoproductivity.
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