Ore-control structural features of Xiadian Ⅶ-branch orebody     

CUI Yun-Long  DONG xin  SUN Li  WANG Kun  ZHOU Chun-sheng  FAN Si-qi  DU Pei-jie 《吉林地质》2008,27(3)

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沸石基储能基元的研究     

杨玉山  董发勤  段涛 《矿物岩石》2008,28(1):13-16

以酸活化沸石为载体,十二醇为储能工质.制备沸石基储能基元,并采用X射线衍射、红外光谱和差示扫描量热等对沸石基储能基元进行表征.结果表明:储能基元在2θ=22.50时的衍射峰变强,相变储能材料十二醇和沸石栽体之间仅仅是简单的嵌合关系.储能基元的相变温度有一定的降低,并且熔融峰变宽.  相似文献   

MOP of feeding reservoir group optimal operation based on SPEA          下载免费PDF全文

DING Sheng-xiang  DONG Zeng-chuan  WANG De-zhi  LI Qing-hang 《水科学进展》2008,19(5)

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南堡凹陷油田古近系碎屑重矿物的物源和构造意义   总被引：2，自引：1，他引：1  

董月霞  张宁  周海民  夏文臣 《地质科技情报》2008,27(5)

利用石油钻井岩心,在南堡凹陷古近纪地层中采集了52件砂砾岩样品并进行了重矿物定量分析.重矿物组合的垂向变化指示出了3个碎屑重矿物组合段,它充分展现了物源区多阶段隆升-剥蚀的历史:始新世的沙三至沙二组合段为凹陷基底岩石层圈(以花岗片麻岩为主)的隆升-剥蚀过程;始新世沙-至渐新世的东二组合段为更深层变质岩层圈的隆升-剥蚀过程;渐新世末的东-段为稳定和老化的变质层圈的隆升-剥蚀及物源区调整过程.在石油勘探井较密且分布较广的东-段,系统进行了各类碎屑扩散体系的重矿物分析,区分出了4个碎屑重矿物扩散体系,分别来自两种构造类型的物源区:①扇三角洲和辫状河三角洲前浊积扇体系物源区为燕辽古造山带,重矿物分布模式表现为主蜂左偏、重矿物组分较少、稳定重矿物显示度偏低的特点;②两个河控三角洲体系物源区为华北古克拉通,重矿物分布模式表现为对称的主峰、重矿物组分较多、稳定组分显示度偏高的特点.  相似文献   

渤海湾盆地南堡凹陷原油成因类型及其分布规律   总被引：8，自引：3，他引：5  

李素梅  姜振学  董月霞  王旭东 《现代地质》2008,22(5)

南堡凹陷近年油气勘探取得了重大突破,为揭示该区滩海与陆地油气成因及分布规律,对67个原油和油砂样品进行了详细的地球化学研究。南堡凹陷原油具有低硫、中高蜡含量特征,陆相成因特点显著。共分为4种类型原油:(1)陆地沙三段深部层系原油,具有高4-甲基甾烷丰度、低奥利烷丰度与低甲基菲指数值和轻微偏高成熟度特征;(2)陆地Es1—Ed原油与Ng和Nm原油,其特征与第一类原油相反;上第三系原油普遍遭遇生物降解;(3)滩海东营组原油,以较高伽马蜡烷/C30藿烷和高甾烷/藿烷值区别于陆地原油;(4)滩海奥陶系潜山原油,具有低丰度甾萜类生物标志物、相对高丰度孕甾烷、三环萜烷与重排甾烷系列等特征,显示较高成熟度。上述4种成因类型原油指示南堡凹陷陆地、滩海均存在多层导有利烃源岩;同层位中滩海Es1-Ed存在较陆地更为优越的有利烃源岩,南堡滩海地区具有广泛的油气勘探前景。  相似文献   

矿集区预测中的探索式空间分析方法及应用——以中亚铜矿集区预测为例   总被引：1，自引：0，他引：1  

陈川  周可法  董玉森  张清 《新疆地质》2008,26(1):32-38

随着地理信息科学和计算机技术的发展,计算环境下矿集区预测方法的研究热潮也初现端倪.依据矿集区所包含的理论内涵(矿床密集区、潜力密集区的聚集内涵),提出了应用探索式空间分析法进行矿集区预测的设想,并以北至科克舍套,南至帕米尔高原,西至乌拉尔山,东至新疆边境的中亚区域为研究区,利用探索式空间分析方法从含矿潜力的确定及其空间分布模式的探索入手,对研究区铜矿集区进行了预测,初步圈定了乌拉尔、矿区阿尔泰、北滨巴尔喀什、斋桑、塔尔巴合台等17处铜矿集区.研究成果除包含了研究区已知矿集区外,还有7处新区,反映了探索式空间分析法在矿集区预测中的应用潜力.  相似文献   

灌注桩钢筋笼内部的磁异常特征   总被引：1，自引：1，他引：0  

董平  樊敬亮  王良书  潘卫育  杨毅文 《物探与化探》2008,32(1):101-104,108

通过分析有限长直立圆柱体内部的磁异常特征,结合模型桩试验,研究了灌注桩钢筋笼内部的磁异常特征,结果表明在钢筋笼内部钻孔中的磁异常Za 垂直分量总体上呈现"两峰夹一谷"的特征,钢筋笼中部呈宽缓的马鞍形负异常,钢筋笼底端位置对应磁异常从极小值转变为极大值的拐点,相应梯度曲线出现极大值.  相似文献   

利用钻芯孔检测灌注桩钢筋笼长度的方法     

樊敬亮  董平  叶景艳  李明  朱国伟 《物探与化探》2008,32(3):335-337

根据充电法原理,结合模型桩试验,分析了钢筋笼周围的充电电场特征,结果表明钢筋笼的底端对应于电位梯度曲线的极小值点及电位曲线的拐点。以此研究结果为基础,提出了利用钻芯孔来检测成桩后钢筋笼长度的方法。某桥的应用表明,该方法简便、实用、可靠。  相似文献   

Effect of Bacillus mucilaginosus on weathering of phosphorite and a preliminary analysis of bacterial proteins   总被引：3，自引：0，他引：3  

Shu Chen  Bin Lian  Congqiang Liu 《中国地球化学学报》2008,27(2):209-216

The authors investigated the effect of Bacillus mucilaginosus on weathering of phosphorite. Analysis of different proteins was of significance in exploring the molecular biological mechanism in the bacterial weathering process. The concrete methods are described as follows： Mineral powder was put into liquid culture medium and B. mucilaginosus was incubated in the medium. The control （group） had no mineral powder in the medium. The treatments and controls were cultured simultaneously under the same condition. In a few days, the supernatant was filtrated, the main cations （Ca^2＋, Mg^2＋, Na^＋, Mn^2＋, Al^3＋, Fe^3＋, K^＋） were measured by ICP-OES, and the contents of water soluble phosphorus （Pws） and silicon （Siws） were determined by colorimetry. The residual solid was weighed on the filter paper, followed by digestion with concentrated HNO3. The concentrations of the main cations and Pws, Siws in the digest liquid were measured by using the method mentioned above. After the supernatant was centrifuged, the precipitation was used to analyze the protein differences between the treatment groups and the control groups by 2-dimentional gel electrophoresis （2-DE）. The experimental results showed that apatite and quartz were partially weathered, but kaolinite was dissolved completely. The population of bacteria increased when mineral powder was added in the liquid medium. Software analysis and comparison of the 2-DE pictures of bacterial proteins revealed 1134 visible protein spots in the treatment group, and 729 visible protein spots in the control group. To compare the bacterial protein expression contents of the treatment group with those of the control group, there were 496 different protein spots, including 214 protein spots which indicated that the protein contents increased, 75 protein spots were indicative of a decrease, and 207 proteins were newly synthesized. It is proposed that the increased bacterial contents may be related to some protein expression and activation after the  相似文献   

Jurassic Tectonics of North China: A Synthetic View   总被引：21，自引：1，他引：20  

ZHANG Yueqiao  DONG Shuwen  ZHAO Yue  ZHANG Tian 《《地质学报》英文版》2008,82(2):310-326

This paper gives a synthetic view on the Jurassic tectonics of North China, with an attempt to propose a framework for the stepwise tectonic evolution history. Jurassic sedimentation, deformation and magmatism in North China have been divided into three stages. The earliest Jurassic is marked by a period of magmatism quiescence （in 205-190 Ma） and regional uplift, which are considered to be the continuation of the “Indosinian movement” characterized by continent-continent collision between the North and South China blocks. The Early to Middle Jurassic （in 190-170 Ma） was predominated by weak lithospheric extension expressed by mantle-derived plutonism and volcanism along the Yanshan belt and alongside the Tan-Lu fault zone, normal faulting and graben formation along the Yinshan- Yanshan tectonic belt, depression and resuming of coal-bearing sedimentation in vast regions of the North China block （NCB）. The Middle to Late Jurassic stage started at 165y.5 Ma and ended up before 136 Ma; it was dominated by intensive intraplate deformation resulting from multi-directional compressions. Two major deformation events have been identified. One is marked by stratigraphic unconformity beneath the thick Upper Jurassic molasic series in the foreland zones of the western Ordos thrust-fold belt and along the Yinshan-Yanshan belt; it was predated 160 Ma. The other one is indicated by stratigraphic unconformity at the base of the Lower Cretaceous and predated 135 Ma. During this last stage, two latitudinal tectonic belts, the Yinshan-Yanshan belt in the north and the Qinling-Dabie belt in the south, and the western margin of the Ordos basin were all activated by thrusting; the NCB itself was deformed by the NE to NNE-trending structural system involving thrusting, associated folding and sinistral strike-slip faulting, which were spatially partitioned. Foliated S-type granitic plutons aged 160-150 Ma were massively emplaced in the Jiao-Liao massif east of the Tan-Lu fault zone and indicate important crustal thicken  相似文献