1) Beipiao
北票
1.
The contents of rare earth elements(REE) of 26 coal samples in Beipiao coalfield,Liaoning Province were determined by ICP MS and their occurrence and distribution pattern were discussed in this paper.
采用等离子电感耦合质谱 (ICP-MS)测试了辽宁省北票煤田 2 6个煤样的稀土元素含量 ,对稀土元素的分布模式、稀土元素来源及其赋存状态进行了探讨 ,发现北票煤田煤中稀土元素含量较世界平均值偏高 ,与灰分关系密切 ,稀土元素分布模式图中存在一定的 Eu负异
2.
The trace elements of coal in Beipiao coal district, Liaoning Province are studied in this paper.
对辽宁北票地区煤中微量元素进行了研究 ,将研究区煤中微量元素的平均质量分数与世界范围煤的微量元素的平均质量分数进行比较 ,发现北票煤中的Cr、Co、Ni、As、Sr、Y、Zr、Ba、Ta、Sc具有较高的富集 ,而Sn、U具有较低的富集 ,这种差异可能主要与聚煤区域的地球化学背景有关。
3.
AccordingtocoalfieldprospectionandsomedataanalysisoncoalmineproductionatSanbaoofBeipiaoOrefield,Liaoning,thepaperputsforwardthattherearecoalbedsanddispersedorganismforgrowinggasinthecosl-bearingstrata.
依据煤田勘探及煤矿井下生产资料分析,认为北票煤田三宝含煤地层具有煤层和分散有机质(干络根)两种生气母质。
2) Beipiao Formation
北票组
1.
Jinlingsi-Yangshan Basin Beipiao Formation Hydrocarbon Source Rock Characteristics;
金岭寺—羊山盆地北票组烃源岩特征
2.
Through comprehensive analysis of coal-bearing strata combinative characteristics in the area,figured out the strata belong to Lower Jurassic Beipiao Formation coal-bearing rock series.
通过对该区含煤地层组合特征综合分析,认为其应属下侏罗统北票组含煤岩系。
3.
Through analyzing a mass of geophysical explorations and drill holes materials,open-air geological survey,sampling and the relevant test about Jinlingsi-Yangshan Basin,the author thinks that Jurassic Beipiao Formation deposits in week oxidation to week deoxidation environment which is lake or marshes,shallow lake to half a deep lake.
通过对金岭寺—羊山盆地大量的地球物理勘探资料、钻孔资料、野外地质调查、取样及相关测试的分析,认为盆地内侏罗系北票组是弱氧化—弱还原环境下接受的一套湖沼、滨浅湖—半深湖相沉积,暗色泥岩、页岩为本区烃源岩,其类型属于低成熟—中成熟阶段的差—中等烃源岩。
3) Beipiao of Liaoning
辽宁北票
1.
Discovery of Pseudolarix from Lower Cretaceous Yixian Formation in Beipiao of Liaoning and its significance for origin and evolution;
辽宁北票早白垩世义县组松柏类金钱松属(Pseudolarix)的发现及其起源与演化意义
2.
A new taxon of Anura from Beipiao of Liaoning in China;
辽宁北票发现一新的无尾两栖类
4) Beipiao Basin
北票盆地
1.
According to the features of the Beipiao Basin and effect of volcanism, three types of cycle are put forward and the Jurassic sequence is divided into 2 GradeⅠ,5 GradeⅡ,and several GradeⅢ.
陆相盆地地层充填序列主要受控于构造作用、古气候和沉积物的供给速度 ,而构造的控制作用尤为重要 ,根据北票盆地的演化特点 ,充分考虑火山作用的影响 ,界定了 3个级别火山—沉积旋回的涵义 ,并将北票盆地侏罗系充填序列划分为 2个一级旋回 ,5个二级旋回及若干个三级旋回。
5) Beipiao mining area
北票矿区
1.
Effect of faults structure on surface gas leakage in Beipiao mining area;
断层构造对北票矿区煤层气地表泄漏的影响
2.
Numerical simulation of leaking gas source concentration from abandoned Beipiao mining area;
北票矿区废弃矿井煤层气泄漏气源集聚数值模拟
6) Beipiao Yixian area
北票-义县地区
1.
The Yixian formation in Beipiao Yixian area,composed mainly of volcano sedimentary strata,contains four volcanic subcycles.
北票-义县地区义县组以火山-沉积地层为主体,具有4个火山活动亚旋回,生物化石主要形成于第一、第二、第四亚旋回期间,构成了3个产出层位。
2.
The Yixian formation in Beipiao Yixian area,Liaoning Province includes a series of volcanic sedimentary strata with volcanic rocks more than 80%,involving four volcanic subcycles.
北票-义县地区的义县组地层是一套火山-沉积地层,其中火山岩地层占80%以上,具有四个火山作用亚旋回,第一亚旋回以基性-偏碱的基性-中基性火山作用为特征,第二亚旋回以中基性-酸性的火山作用为特征,第三亚旋回以基性-中性火山作用为特征,第四亚旋回以中酸性火山作用为特征;义县组火山-沉积地层包含至少7个沉积夹层,可以进一步归纳为四套沉积层,即底砾岩层、下部火山岩中的沉积夹层、中部湖相沉积层和上部河湖相沉积层,沉积层中生物化石主要集中在3个主要层位。
补充资料:白鸽票
1.彩票的俗称。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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