1) 3rd member of Quantou Formation
泉头组三段
2) Member 3 and 4 of Quantou formation
泉头组三四段
3) 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。
4) the second and the third members of Quantou Formation
泉头组2、3段
1.
It is considered that Daluozhen-Xiangyangshan has favorable metallogenetic potentiality for interlayered oxidation type uranium deposits,the target horizon is the second and the third members of Quantou Formation.
在资料分析研究的基础上,从区内目的层地质特征出发,全面分析了本区的构造位置、铀源条件、目的层砂体特征、氧化及含铀性,详细探讨了本区可地浸砂岩型铀成矿条件,初步认定大罗镇一向阳山林场地区有较好的层间氧化带型铀成矿前景,目的层为泉头组2、3段。
5) the fourth segment of Quantou-Yaojia Formation
泉头组四段-姚家组
6) Quantou Formation
泉三、四段
1.
Diagenesis and pore evolution of the third and the fourth members of Quantou Formation in Xinli Oilfield;
新立油田泉三、四段储层成岩作用及储集空间演化
2.
Based on the high-quality 3-D post-stack seismic data,we use wavelet frequency-division process,sonic log reconstruction and non-linear constrained inversion techniques to do a reservoir prediction on the thin-bed channel sands of the Quantou formation in the Xinli oilfield,southern Songliao basin.
根据松辽盆地南部新立油田泉头组的地质特征,在三维地震资料叠后处理提高剖面品质的基础上,有针对性地运用小波分频处理、测井曲线重构技术、非线性高精度薄砂体预测技术,对泉三、四段薄互层河道砂岩储层展开了地震反演预测工作。
补充资料：北山三咏其三——道光泉
【诗文】：
箨龙将雨绕山行，注远投深静有声。
云涌浴槽朝自暖，虹垂斋镬午还晴。
铜瓶各满幽人意，玉甃因高正士名。
神力可嗟妨智巧，桔槔零落便苔生。
【注释】：
【出处】：
箨龙将雨绕山行，注远投深静有声。
云涌浴槽朝自暖，虹垂斋镬午还晴。
铜瓶各满幽人意，玉甃因高正士名。
神力可嗟妨智巧，桔槔零落便苔生。
【注释】：
【出处】：
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