A new species of Gobiconodon （Triconodonta, Mammalia） and its implication for the age of Jehol Biota

A new species of Gobiconodon is found from the Yixian Formation of western Liaonlng, China. The new taxa,G zofiae sp. nov., has a confluent opening for branches Ⅱand Ⅲ of the trigeminal nerve on the anterior lamina of the petrosal. G zofiae sp. nov. is similar to Repenomamus in having an ossified Meckel‘s cartilage connecting the lower jaws and ear region. The new species, with enlarged I^1/I1, posteriorly located infraorbital foramen and four mental foramina,distinctly differs from the other species of Gobiconodon. The new material indicates that Gobiconodon has four, not five,upper molariforms. The presence of Gobiconodon in Jchol Biota makes it possible to correlate Jehol Biota with faunas in eastern Asia and North America, and suggests the age of the Yixian Formation to be Early Cretaceous.     

Magnetostratigraphic study of Cretaceous depositional succession in the northern Kuqa Depression, Northwest China

Stratigraphic studies on the depositional succession in the Kuqa Depression can be traced back to as early as 1950s[1], however, there are still some disputes about chronostratigraphic division of the Bashenjiqike For- mation because of the paucity of fos…     

Shenzhousia qilianshanensis gen. et sp. nov. (Protodonata, Meganeuridae), a giant dragonfly from the Upper Carboniferous of China

A new dragonfly of family Meganeuridae Shenzhousia qilianshanensis gen. et sp. nov., discovered from Ningxia Hui Autonomous Region in North China, is described in the present paper. It has an estimated wingspan of about 450?500 mm and may be the largest fossil insect in Late Carboniferous Namurian Stage discovered by far. The new species is referred to Meganeuridae because of the presence of the characteristic oblique vein between anterior branch of radius (RA) and posterior branch of radius (RP) near the base of RP2. It differs from other genera within the family in the following characteristics: Precostal area short and not extending to the midwing; posterior branch of subcostal vein short, merging into costal vein near the level of originating point of IR₂; RP forking earlier than anterior branch of media basally; RP_1＋2 and RP_3＋4 parallel and close to each other for a long distance, and then diverge gradually surpass midwing.     

西藏措勤地区的下白垩统岩石地层单位评述

西藏区域地质调查大队在1:100万日喀则幅区调中将措勘地区划分为两个地层小区,各自建立了下白垩统的岩石地层系统.作者根据在该区测制的下白垩统连续地层剖面及相关地质调查,认为这两个地层小区并不存在;建议在措勤地区建立统一的下白垩统岩石地层系统,从下至上划分为则弄组、多尼组和郎山组.     

C-isotope composition and correlation of the Upper Neoproterozoic in Keping area, Xinjiang

C-isotope analysis of the carbonates in the Upper Neoproterozoic in Keping, Xinjiang indicates that the Qigebrak Formation and the Upper Sugaitbrak Formation mainly record positive C-isotope values, and a distinct positive excursion occurs in the lower part of the Qigebrak Formation. There are three negative excursions in the boundary between the Qigebrak Formation and the Cambrian, the uppermost and lowermost Upper Sugaitbrak Formation. These characters resemble those of the Upper Neoproterozoic in the Three-Gorge area, which suggests that the Upper Sugaitbrak Formation and Qigebrak Formation can be correlated with the middle and upper parts of the Doushantuo Formation and Dengying Formation, respectively. The negative excursion at the top of the Upper Sugaitbrak Formation corresponds to that at the top of the Doushantuo Formation, while the negative excursion at the bottom of the Sugaitbrak Formation can be correlated with that at the middle part of the Doushantuo Formation in the Three-Gorge area and that at the top of the Hangelchaok diamictites in the Quruqtagh area.     

鄂尔多斯盆地东南部上古生界储集砂岩的成岩作用

研究鄂尔多斯盆地东南部上古生界砂岩储层特征,以及不同的成岩作用类型与储集性能的关系。通过分析取芯井的岩石薄片、铸体薄片、扫描电镜、能谱分析数据,发现储集砂岩中发育有粒内溶孔、粒间孔、粒间溶孔、晶间孔、溶缝等多种孔缝类型,其中最主要的是粒内溶孔和粒间溶孔;主要成岩作用类型有压实作用、溶蚀作用、碳酸盐矿物、硅质矿物和黏土矿物的形成作用。结合不同砂岩组分与孔隙面孔率的相关性,得到如下结论:(1)压实作用是导致砂岩孔隙度较差的重要原因;(2)增加砂岩整体孔隙度最重要的是溶蚀作用;(3)碳酸盐矿物的形成会导致砂岩孔隙度减小;(4)硅质矿物会一定程度减少砂岩粒间孔;(5)高岭石的形成对增加岩石整体孔隙作用有限,水云母和绿泥石对溶孔和晶间孔的形成不利。     

拟单调广义向量变分不等式

在集值映射T：K→2^L（X,Y）是拟单调和弱上半连续的条件下,考虑了广义向量变分不等式强解存在的强制条件,证明了与广义向量变分不等式非奇异解非空等价的强制条件,同时提出使广义集值向量变分不等式解集非空的极小强制条件．     

采用工艺巷防止高瓦斯易自燃综放面上隅角瓦斯积聚的探讨

上隅角瓦斯积聚是采用综呆放顶煤技术开采高瓦斯易自燃煤层必须面对的难题。文章提出了利用工艺巷防止综放面上隅角瓦斯积聚的方法。并且,根据计算流体力学理论建立数学物理模型,模拟计算了综放工作面及采空区内空气、瓦斯流动的规律,有力地论证了该方法的可行性和有效性,为我国高瓦斯易自燃煤层综放工作面的瓦斯防治工作提供了新的思路。     

中扬子北部上震旦统陡山沱组沉积特征及演化

中扬子区上震旦统陡山沱组中下部为一大套灰黑色、黑灰色泥页岩,且大部分地区深埋地腹,具有较好的页 岩气勘探潜力。基于钻井岩芯及野外剖面测量观察,开展了系统的基础地质研究,建立了陡山沱组区域地层格架,进 行了层序和沉积相分析。上震旦统陡山沱组岩性具有四分特征,钻井岩芯和实测剖面各分段的岩性特征和沉积厚度 有所不同,地层厚度在90∼250 m,总体上呈东西走向展布,即自北西向东、南逐渐增厚的趋势。将陡山沱组划分为一 个二级层序（SS1）,其中包含4 个三级层序（SQ1、SQ2、SQ3、SQ4）。沉积相包括滨岸潮坪相和台地相,台地相划分为 开阔台地、局限台地和台内盆地3 类亚相。陡山沱期,研究区整体上为台地相沉积,区内东南部为开阔台地沉积,西北 部为局限台地,西南部花鸡坡-X1 井-九里垭一带为相对深水的台内盆地相沉积。     

特大规模组合电路测试数据产生方法研究

针对特大规模组合电路和全扫描设计电路提出了一种高速测试生成方法。该方法采用有限回溯测试模式产生方法生成测试码,采用ｎ（机器字长）个测试码并行的单故障传播方法模拟验证测试覆盖。测试生成与故障模拟为ｎ对１紧耦合集成方式。该方法运行１０个Ｂｅｎｃｈｍａｒｋ电路,取得了低测试长度、高故障覆盖、高效率的良好效果。