1) Lianghe basin
梁河盆地
1.
This paper deals with favorable and unfavorable factors of uranium mineralization in the Lianghe basin based on hydrogeological,palaeohydrogeological and hydrogeochemical characteristics.
通过分析梁河盆地水文地质特征、古水文地质特征和水文地球化学特征,列举了对铀成矿有利和不利因素,认为盆地盖层南部诸多因素决定其不利成矿,盆地盖层北部地层剥蚀严重,构造发育,具有形成砂岩型铀矿床的潜力,但不利因素决定其成矿规模非常有限。
2) Mohe Basin
漠河盆地
1.
Study on the Features of Magnetic Field and the Sedimentary Structure in Mohe Basin;
漠河盆地重力场特征与沉积构造研究
2.
Provenance Analysis of Middle Jurassic Sediments and Its Geological Significance in Mohe Basin;
漠河盆地中侏罗世沉积源区分析及地质意义
3.
Tectonic Characteristics and Basin Evolution of the Mohe Basin, Heilongjiang Province;
黑龙江漠河盆地构造特征与成盆演化
3) Hetao Basin
河套盆地
1.
Characteristics of Sporopollen Assemblage and Its Palaeoclimate during Quaternary Pleistocene in the Huhe Sag,Hetao Basin;
河套盆地古气候演化与生物气勘探
2.
Charater of seismicity before the Ms≥5.5 earthquakes in Hetao basin;
河套盆地Ms≥5.5级地震前地震活动性特征
3.
Research about Geological Conditions of Shallow Gas (Biogenic Gas) Accumulation in HETAO Basin;
河套盆地浅层气（生物气）成藏地质条件研究
4) Liaohe Basin
辽河盆地
1.
Characters of coal classification and coal rank distribution in third member of Shahejie Formation in eastern depression of Liaohe basin;
辽河盆地东部凹陷沙三段煤种和煤级分布特征
2.
Lithologic identification and reservoir division of Xing-Ma Archean group buried hill in Liaohe basin;
辽河盆地兴马太古界潜山的岩性识别与储层划分
3.
Research on hydrocarbon abundance conditions in nearshore sublacustrine fan in Western sag of Liaohe Basin——take Rehetai Formation in Xing-Bei area as an example;
辽河盆地西部凹陷近岸湖底扇油气富集条件研究—以兴北地区热河台油层为例
5) the Liaohe Basin
辽河盆地
1.
Oil-oil meticulous correlation research shows that there exist both immature and mature oils in Oulituozi area of the Liaohe Basin,and the maturity level of these oils is generally lower than those in the other areas of the East Sag.
油—油精细对比揭示辽河盆地欧利坨子地区低熟油和成熟油共存,与东部凹陷其它地区原油相比总体上成熟度较低。
2.
According to analysis of formation water and crude oil at the west Jinganpu of Damintun Sag in the Liaohe Basin,type NaHCO_3 formation water on the top of the burial hills in the studied area is dominative,type CaCl_2 appear in local area.
对辽河盆地大民屯凹陷静安堡西侧低潜山带地层水化学性质特征分析表明,潜山顶部地层水是以NaHCO3水型为主,局部出现CaCl2水型,反映了潜山顶部总体上具有一定的自由交替水动力条件的开放性环境,而局部出现封闭性环境;这种局部性的封闭环境主要是由于封堵性断层及上覆欠压实泥岩的封堵造成的。
6) Powder River basin
粉河盆地
1.
In order to understand the control of hydrogeological conditions on accumulation of coalbed methane in low rank coal,a comparison study is carried out between the Powder River basin in America and the Juggar basin in China.
为了研究水文地质条件对低煤阶煤层气成藏的控制作用,对美国粉河盆地和我国准噶尔盆地进行了对比研究。
补充资料：漠河县
| 漠河县 中国纬度位置最北县份。位于黑龙江省黑龙江上游南岸，大兴安岭北麓。1990年人口8.5万。汉族为主，有蒙古、回、苗、壮、朝鲜、满、土家、达斡尔等13个少数民族。面积1.85万平方千米。明隶木河卫，清宣统元年（1909）置漠河卡衙门，1914年7月改漠河设治局，1917年改漠河县，1947年1月并入呼玛县。1981年5月复设漠河县。矿产资源有黄金、银、煤炭、铁、铜、锡、钼、铅、石墨、珍珠岩、石灰石、大理石等。野生动物资源有鹿、灰鼠、狍、狼、雪兔、貂、野猪、熊、獾、狐、水獭、猞猁等。野生植物资源有越桔、都柿、牙格达、杜鹃、草参、黄芪、五味子、木灵芝、金针菜、猴头菌、榛蘑、贝母等。土特产品主要有毛皮、山珍、鱼类等。名胜古迹主要有北极村、松苑公园、胭脂沟、黑龙江源头等。 |
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