吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (5): 1247-1260.doi: 10.13278/j.cnki.jjuese.20180210

• 地质与资源 • 上一篇    下一篇

吴起—志丹地区延长组下组合浊沸石的纵向分布特征与成因

王朝1, 王冠民1, 杨清宇2, 胡津1, 何为2, 石晓明1, 张婕1   

  1. 1. 中国石油大学(华东)地球科学与技术学院, 山东 青岛 266580;
    2. 中国石油天然气股份有限公司长庆油田分公司勘探事业部, 西安 710018
  • 收稿日期:2018-08-08 发布日期:2019-10-10
  • 通讯作者: 王冠民(1969-),男,教授,博士生导师,主要从事沉积学与储层地质学研究,E-mail:wguanmin@sina.com E-mail:wguanmin@sina.com
  • 作者简介:王朝(1994-),男,硕士研究生,主要从事沉积学与储层地质学研究,E-mail:502156931@qq.com
  • 基金资助:
    国家自然科学基金项目(41572123)

Vertical Characteristics and Genesis of Laumontite in Lower Combination of Yanchang Group in Wuqi-Zhidan Area

Wang Zhao1, Wang Guanmin1, Yang Qingyu2, Hu Jin1, He Wei2, Shi Xiaoming1, Zhang Jie1   

  1. 1. School of Geoscience, China University of Petroleum(East China), Qingdao 266580, Shandong, China;
    2. Exploration Division of Petrochina Changqing Oilfield Company, Xi'an 710018, China
  • Received:2018-08-08 Published:2019-10-10
  • Supported by:
    Supported by National Natural Science Foundation of China (41572123)

摘要: 吴起-志丹地区延长组下组合包括长8、长9和长10三个油层组。在研究区中、西部,下组合油气主要来源于长73烃源岩;在研究区东部,下组合油气主要来源于长91烃源岩。624个储层样品的X衍射和薄片镜下观察表明,研究区下组合储层中普遍发育浊沸石胶结物,其体积分数在纵向上具有明显的规律性:研究区中、西部浊沸石体积分数在长8段最低,向下逐渐增高,在长10段普遍发育浊沸石胶结物;研究区东部浊沸石体积分数则在长91段最低,向上部长8段逐渐增高,向下部也有所增高,在长10段达到最大值。浊沸石的这种变化规律与烃源岩成熟和流体释放密切相关。浊沸石属于早成岩阶段形成的碱性低温铝硅酸盐矿物,在有机质成熟释放出的有机酸和CO2作用下,由近及远会发生不同程度的溶蚀作用,造成纵向上距离烃源岩越近,浊沸石残留得越少,距离烃源岩越远,浊沸石保留得越多。该分布规律可以指示烃源岩成熟后释放流体运移的距离和范围。

关键词: 鄂尔多斯盆地, 延长组, 浊沸石, 烃源岩

Abstract: Three reservoir groups are existed in the lower combination of the Yanchang Group in Wuqi-Zhidan area:Chang 8, Chang 9 and Chang 10. In the mid-western part of the study area, the oil and gas mainly originate from the source rocks of Chang 73;while in the eastern part of the study area, the oil is from the Chang 91 source rocks. The X-ray diffraction and microscope observations of 624 reservoir samples show that laumontite cement is commonly developed in the reservoir in the lower combination. The content of laumontite has obvious vertical regularity:it is the lowest in Chang 8 in the mid-western part of the study area, gradually increases downward,and commonly develops in Chang 10; in the eastern part of the study area, the content of laumontite is the lowest in Chang 91, gradually increases in the upper reservoir of Chang 8 and lower Chang 10, and reaches the maximum in Chang 10. This change of laumontite is closely related to the maturity of the organic matter and fluid released from the source rocks. Laumontite belongs to the aluminosilicate mineral formed in the early diagenetic stage under alkaline and low temperature. Under the action of the organic acids and CO2 released from the mature source rocks, different degrees of laumontite dissolutions occur from near to far. The closer to the source rocks in the vertical direction the formation is, the less the laumontite remains. This distribution regularity indicates the distance and range of hydrocarbon generation and expulsion from source rocks.

Key words: Ordos basin, Yanchang Formation, laumontite, source rocks

中图分类号: 

  • P587
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