2) Xiaoquan gas pool
孝泉气藏
3) Quantou Formation
泉头组
1.
Sedimentary facies of the Member 4 of Quantou Formation of Lower Cretaceous in southern Central Depression of Songliao Basin;
松辽盆地中央坳陷南部下白垩统泉头组四段沉积相
2.
A New Oospecies,Dictyoolithus Gongzhulingensis,from the Early Cretaceous Quantou Formation in the Central Jilin Province;
吉林省公主岭早白垩世泉头组网形蛋(Dictyoolithus)一新种
3.
Study of the sedimentary system of the Early Cretaceous Quantou Formation in northern Liaoning;
辽北早白垩世泉头组沉积体系
4) the bottom of Quantou Formation
泉头组底部
5) 3rd member of Quantou Formation
泉头组三段
6) the first member of Quantou Formation
泉头组1段
1.
Based on the lithological-lithofacies, sand bodies, epigenetic alteration, uranium mineralization of the first, second and third members of Quantou Formation in Hailitu area, south of Songliao Basin, it is considered that the first member of Quantou Formation has better metallogenic prospect for the in-situ leachable sandstone-type uranium deposit.
对松辽盆地南部海里吐地段泉头组1、2、3段岩性-岩相及砂体、后生蚀变、铀矿化特征等进行了分析,认为泉头组1段具有较好的地浸砂岩型铀成矿前景,提出铀成矿有类似钱家店铀矿床,即"成矿前富含炭质、有机质砂体预富集-断裂构造煤成气或油气有机流体还原褪色蚀变与铀叠加富集-层间氧化作用"三位一体的成矿模式,预测海里吐地段黑五家子—协尔苏远景区为进一步工作的有利地段。
补充资料：孝感泉
孝感泉 在原西门内孝感坊北,今趵突泉北路22号院内。金《名泉碑》、明《七十二泉诗》、清《七十二泉记》均著录。泉池以石砌岸,长3.4米,宽2米。据北宋乐史《太平寰宇记·卷十九》载:“孝感水在县北门……耆老传云,昔有孝子事母,取水远。感此,泉涌出,故名‘孝水’。天宝六年敕改为‘孝感水’。”又据《山东通志》载：元代一名叫刘琮的孝子，其父久病卧床,他精心服侍，用尽家产。家距水源甚远，必须每天到远处取水,因而感动神灵。一日,刘琮刨地,得金一窖,取尽后,忽涌一泉。刘琮用掘得的金子买药并汲此泉之水煎熬,父亲病愈,活到百岁,所以人们给这泉取名为“孝感泉”。后来,刘父寿终,刘琮削发为僧,并把宅舍捐给寺院,这寺改称孝感寺,后又改为太平寺。
古时孝感泉处,翠竹蔽日,清流潺潺。其后,太平寺废,孝感泉依然存留,而且水势尚好。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条