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 Kai1,2, Bao Zhi-Dong1,2, Ji Han-Cheng1,2, Liu Jin-Xia3, Wang Gui-Ling4, Ma Feng4, Guo Rui-Jing1,2, Cao Ying-Zhuo1,2, Yang Fei5, Fu Yong1,2, Li Xiao-Bo1,2, Hua Ying-Xin1,2, Que Yi-Juan1,2, Li Zong-Feng1,2, Xu Xi-Ting1,2, Hu Xian-Cai4
雄安新区蓟县系雾迷山组储集空间类型 a—藻粘结白云岩,藻架孔(见箭头),后期被硅质充填,任266井,3130.5 m,(-);b—鲕粒白云岩中粒间孔和铸模孔(见箭头),后期被硅质充填,雁33井,2850.4 m,(-);c—粉-细晶白云岩,晶间孔,任48井,2699.4 m,铸体,(-);d—灰色泥晶白云岩,至少发育2期裂缝(见箭头),相互切割关系,网状缝,鄚9井,4174.8 m,岩心;e—灰色泥晶白云岩,发育8条高角度缝,其中1条将岩心切割为两半,鄚9井,4208.6 m,岩心;f—角砾白云岩中发育2期构造缝,未充填,构造缝切割白云岩角砾,高深1井,3760.8 m,铸体,(-);g—硅质白云岩,溶蚀缝发育,溶蚀扩缝现象,白云石和泥质充填、半充填,高深1井,3501.6 m,铸体,(-);h—泥晶白云岩中缝合线发育,泥质充填,淀5井,2028.2 m,(-);i—岩心上溶洞垮塌,洞壁可见白云石晶体半充填(见箭头),溶洞直径大于3 cm,任266井,3205.1 m