|
雄安新区蓟县系雾迷山组岩溶热储特征、主控因素及有利区预测*
|
鲁锴1,2, 鲍志东1,2, 季汉成1,2, 刘金侠3, 王贵玲4, 马峰4, 郭瑞婧1,2, 曹瑛倬1,2, 杨飞5, 符勇1,2, 李潇博1,2, 华盈鑫1,2, 阙宜娟1,2, 李宗峰1,2, 许西挺1,2, 胡先才4 |
Characteristics,main controlling factors and favorable area prediction of karstic geothermal reservoirs of the Jixianian Wumishan Formation in Xiong’an New Area
|
Lu Kai 1,2, Bao Zhi-Dong 1,2, Ji Han-Cheng 1,2, Liu Jin-Xia 3, Wang Gui-Ling 4, Ma Feng 4, Guo Rui-Jing 1,2, Cao Ying-Zhuo 1,2, Yang Fei 5, Fu Yong 1,2, Li Xiao-Bo 1,2, Hua Ying-Xin 1,2, Que Yi-Juan 1,2, Li Zong-Feng 1,2, Xu Xi-Ting 1,2, Hu Xian-Cai 4
|
|
雄安新区蓟县系雾迷山组埋藏溶蚀特征 a—灰色泥晶白云岩,热液硅质沿裂缝充填,任48井,2706.26 m,岩心;b—浅灰色泥晶白云岩,热液硅质充填后破碎角砾化(见箭头),D11井,1639.9 m,岩心;c—泥晶白云岩,白云石重结晶并发育溶孔(见箭头),雁33井,2888.8 m,铸体,(-);d—硅质白云 岩,沿裂缝热液硅质被溶蚀产生溶孔(见箭头),鄚14井,4976.2 m,(+) |
|
|
|
|
|