陆相断陷盆地层序类型与隐蔽油气藏勘探——以南堡凹陷古近系为例

以南堡凹陷高分辨率三维地震、测井和丰富的地质资料为基础, 运用高精度层序地层分析方法, 结合盆地构造和沉积充填特征的研究, 在南堡凹陷古近系识别出了1个超层序组、4个超层序、11个三级层序, 在柳北扇三角洲体系可划分出6个四级层序.根据古构造坡折带控制层序类型和层序构成模式的思路, 通过南堡凹陷古近系同沉积构造发育特征的分析, 认为南堡凹陷古近系存在同沉积断裂坡折带和同沉积背斜挠曲坡折带2种类型, 由此决定了南堡凹陷古近系主要发育了同生断裂坡折型层序和同沉积背斜挠曲坡折型层序, 建立了这2种类型层序体系域构成模式.其中同生断裂坡折型层序和同沉积背斜挠曲坡折型层序的低位域砂体及高位域砂体成藏条件优越、地震剖面易于识别, 是隐蔽油气藏勘探的主要目标.      

导电、导磁聚苯胺纳米复合物的合成与表征

在纳米Fe₃O₄晶体粒子存在的情况下, 用十二烷基苯磺酸钠(SDBS)作乳化剂及分散剂, 通过HCl调节体系的酸度, 合成了导电、导磁的Fe₃O₄-聚苯胺(Fe₃O₄-PANI)纳米复合物, 用X-衍射(XRD)、透射电子显微镜(TEM)、傅立叶红外(FT-IR)等对该复合物进行了表征, 结果显示: SDBS与HCl发生竞争掺杂行为, 复合物的组成为Fe₃O₄-PANI-DBSA, Fe₃O₄平均粒径约13 nm, 且均匀分布在聚苯胺基体中, 该复合物具有较好的导电性及导磁性, 随着纳米Fe₃O₄含量由7.79%增加到35.34%, 复合物的电导率由1.71 S/m下降至0.41 S/m, 复合物的比饱和磁化强度σ_s则由6.14 A·m2/kg增加到18.11 A· m2/kg, 其矫顽力在0.52~0.73 A/m之间.      

累托石制备润滑脂的初步研究

累托石是一种具有独特的结构组成和性质的粘土矿物,其既具有象蒙脱石一样的阳离子交换性,吸水膨胀性,制浆性等,又具有象云母一样的耐高温性和光滑性等性能。经提纯和有机改性后的累托石吸油速度快,膨胀率高,是一种较好的稠化剂,用它制备的润滑脂滴点〉６３３．１５Ｋ,远高于膨润土润滑脂的指标要求,研究表明,累托石是制备润肖脂稠化剂的好原料,累托石润滑脂是一种新型高温润滑脂。     

Application of Dempster-Shafer theory in mineral resource potential mapping

The Dempster-Shafer theory has been successfully applied to mineral resource potential mapping in G1S environmental. In this applied form, basic probability assignment and combined basic probability assignment are applied to measuring map pattern and map pattern combination, respectively; and the environment composed of the only two singleton sets (deposit set and non-deposit set), is used for expressing the entire map area. For a subarea in which the certain map pattern combination exists, the combined basic probability assignment corresponding to the map pattern combination existing in this subarea, expresses the belief of inferring the subarea belonging to the deposit set from the evidence that the corresponding map pattern combination existing in the subarea. Thus, it may be served as a statistical index measuring the relative mineral resource potentials of the subarea. And it may be determined like 1) dividing the map area into a series of small equal-sized grid cells and then select the training sample set composed of the well-known grid cells or the entire grid cells; 2) estimating the basic probability assignments corresponding to each map pattern from the training sample set; 3) determining the map pattern combination existing in each cell, and then appling the Dempster's Rule of Combination to integrating the all basic probability assignments corresponding to the map patterns existing in the cell into the combined basic probability assignment. Mineral resource potential mapping with the Dempster-Shafer theory is demonstrated on a case study to select mineral resource targets. The experimental results manifest that the model can be compared with the weights of evidence model in the effectiveness of mineral resource target selection.     

The Occurrence of Oleananes in the Beibuwan Basin and Its Application to the Study of Maturity and Oil-Source Rock Correlation

The oleanane parameter, i.e., OP （oleananes/（oleananes＋C30hopanes）） in the two sedimentary columns of the Beibuwan Basin, South China Sea, can be used to delimit the top of oil generation window, with Ro （/%） of 0.53 in Well M1 and 0.55 in Wells H1/Hd1/Hd2, respectively. Comparing with vitrinite reflectance （Ro/%）, the OP features a dynamic range and can indicate the oil generation window more precisely. By using OP and other geochemical indices, the oil-source correlation is also conducted. It suggests that the oils in wells M1 and M2 are derived from the source rocks in situ. The mudstone in Huachang uplift is not the main source rocks for oils in this area, The OP is also a useful oil-source correlation parameter in some Tertiary lacustrine basins.     

Research on formation density MWD instrument in engineering geological exploration

A high efficiency method is very important in geological survey for a new city in China. Geophysical parameters are Measured While Drilling （MWD）, and these parameters are processed and explained on the ground, so the method can replace conventional engineering geological exploration for drilling rock sample. According petroleum engineering MWD, using the different characters of different rock absorbs γ radial, with the method of storing data in hole and explaining data on the ground, engineering geological exploration formation density MWD is researched. The MWD works stabilized, and the performance is good with precise data.     

扬子陆核与陆缘新元古代岩浆事件对比及其构造意义——来自黄陵和汉南侵入杂岩ELA-ICPMS锆石U-Pb同位素年代学的约束

本文报道分别位于扬子克拉通核部和北缘的黄陵及汉南新元古代侵入杂岩体的惰性气体激光剥蚀-等离子体质谱(ELA-ICPMS)锆石U-Pb年代学研究及其构造意义分析.定年数据显示,黄陵地区的三斗坪、大老岭岩套分别形成于794±7和795±8Ma;晓峰浅成岩岩套形成于744±22Ma,不仅与震旦系莲沱组底部火山岩年龄相同,且同期热事件普遍记录于杂岩体内其它岩套.汉南杂岩体中五堵门岩体形成于789±10Ma,在分析误差范围内与三斗坪、大老岭岩套相同;天平河岩形成于863±10Ma,这是在扬子北缘首次识别出这期岩浆作用.在扬子陆核和北缘侵入杂岩中还分别发现了≈860Ma和945～931Ma的捕获锆石.此外,740Ma的后期热事件同样记录于汉南杂岩体,表明扬子陆块内部和北缘共同经历了790Ma的峰期中酸性岩浆作用和≈740Ma的后期强烈热改造事件,即事件具有克拉通范围的性质.与天平河岩体岩性相似、年龄相同的侵入岩体已在攀西多处地区发现,说明空间上860Ma岩浆作用在扬子北缘和西缘可能具延续性.作者认为,"晋宁期"具造山性质的构造运动开始的时间应以830Ma为限,于≈790Ma达到了以壳内物质重熔为主的大规模岩浆侵入事件的峰期,并在≈740Ma以短期内地壳运动由剧烈抬升向快速沉降的构造转换为造山作用结束的标志.本次研究成果为探讨扬子克拉通新元古代大规模岩浆作用与同期全球构造事件的相互关系提供了重要的同位素年代学约束.     

Detrital Zircon Geochronology and Provenance of Core Sediments in Zhoulao Town,Jianghan Plain,China

In our study,the U-Pb age spectrum of detrital zircons from terrigenous sediments is used to determine the sources.The Middle and Upper Reaches of the Yangtze River drain the western Yangtze craton and eastern Tibetan plateau,and take lots of sediments to the Jianghan (江汉) plain.Detrital zircons collected from Zhoulao (周老) core provide an ideal sample for the provenance studies.Here we report LA-ICP-MS U-Pb ages of 125 detrital zircons from one sand sample in the core sediments,which is recovered from a dep...