川东北地区不同构造带地层水化学特征与油气保存的关系

判断油气藏保存条件的优劣,除了盖层和断层封闭性之外,还有油气水的化学特征,如地层水的交替或油气散失。通过对川东北地区地层水的水型、矿化度、水性系数等参数的综合分析认为,川东北宣汉—达县地区与通江—南江—巴中地区的地层水具有矿化度高和氯镁系数越大,变质系数、脱硫系数和碳酸盐平衡系数就越小的特点。矿化度、水性系数及水型的变化具有很好的一致性,表明该区存在有利于油气保存的水文地质条件。     

济阳坳陷博兴洼陷西部沙三段层序地层

选取以基准面为参照面的高分辨率层序地层学的理论与分析技术,对博兴洼陷西部沙三段开展层序地层分析工作。在博兴洼陷沙三段识别出5个层序界面和4个较大规模的洪泛面,由此将研究层段划分为4个长期基准面旋回(相当于3级层序),并通过长期旋回内部次级转换面的识别,细分出8个中期旋回(大致相当于4级层序)。通过对比建立了研究区的高分辨率层序地层格架,并分析了各层序的地层发育特征。以层序格架为基础,探讨了研究区各层序的沉积演化特征,建立了辫状三角洲—浊积扇层序发育模式,认为研究区辫状三角洲和浊积扇均具有加积作用特点;斜坡区为辫状三角洲发育区,而洼陷区为浊积扇发育区;中期基准面旋回下降期辫状三角洲发育,上升期浊积扇发育;浊积扇体的发育规模与湖泛规模相关。综合分析认为,浊积扇是形成岩性圈闭的主要储集砂体类型,其发育的有利层位是MSC8、MSC7、MSC6、MSC5旋回的上升半旋回,岩性圈闭发育的有利区是博兴南部斜坡坡折带之下的洼陷区。     

试论浙东不同盆地塘上组的层位及时代

详细的地质调查和剖面研究,证实了浙东不同盆地原划分的塘上组并非都为同一层位。天台、丽水及缙云壶镇、舒洪盆地原划分的塘上组均整覆于馆头组沉积岩之上,其上为两头塘组整覆,层位大致与馆头组上部相当,为下白垩统。小雄盆地上部原称塘上组的一套火山岩,其岩石组合、地层层序、生物化石组合和同位素年龄等与浙东其他盆地原划分的塘上组均不相同,成岩时代在81.5—92.9Ma,产晚白垩世翼龙和鸟类化石,覆于永康群朝川组之上,其层位大致与永康群方岩组和天台群赤城山组相当,时代为晚白垩世。     

Lithofacies and stratigraphy of the Ordovician Guniutan Formation in its type area,China

The Lower to Middle Ordovician Guniutan (Kuniutan) Formation in the eastern Yangtze Gorges, China has been demonstrated to be similar to the ‘Orthoceratite Limestone’ in Baltoscandia with respect to facies, stratigraphic development and conodont biostratigraphy. Thus the ‘Orthoceratite Limestone’ appears to be a much more widely distributed and characteristically Ordovician facies than has hitherto been assumed. Five lithostratigraphic subdivisions of the Guniutan Formation are here defined in ascending order as the Nanya, Puxi, Wuguixi, Daping and Niangjiafang members. It is shown that these members, which represent considerable spans of time as indicated by their conodont stratigraphy, may be fairly thin but nevertheless regionally extensive. A new conodont zone, with Eoplacognathus crassus as the zonal fossil, is established to accommodate the precise dating of the Wuguixi and Puxi members. Microfacies data from the Guniutan Formation, available for the first time, show that its dominant component particles are sand-sized echinoderm and arthropod debris, as in the Baltoscandian ‘Orthoceratite Limestone’.     

华北陆块东南缘凤台组时代的讨论

华北陆块东南缘凤台组归属于震旦系或寒武系尚无定论,影响了对华北陆块震旦纪与寒武纪转折时期的古构造、古地理和古生物的重大质变事件的探讨。本文根据下震旦统顶部与凤台组之间裂离不整合的发现及其意义的讨论,以及凤台组夹层粉砂质泥岩620Ma的Pb-Pb等时线年龄,基本厘定出凤台组时代为晚震旦世。     

贵州台江凯里组的遗迹化石Treptichnus

贵州台江下中寒武统凯里组中产有丰富的、保存良好的Treptichnus Miller,计5个遗迹种（其中包括2个新遗迹种）：T．bifurcus Miller,T．pedum（Seilacher）,T．pollardi Buatois and Mdngano,T．arcus n．ichnosp．和T．taijiangensis n．ichnosp．,并与节肢动物的觅食迹、爬行迹和游泳迹等共生,属Cruziana遗迹相。产于凯里组的Treptichnus可能为节肢动物的居住迹。随着造迹生物身体的增长和沉积物的增厚,造迹生物在原潜穴的基础上不断地开拓新的潜穴,而构成三维空间复杂的潜穴系统。     

On the Systematic Position of Eosipterus yangi Ji et Ji, 1997 among Pterodactyloids

1 Introduction Eosipterus yangi is the first pterosaur found from western Liaoning Province (Ji and Ji, 1997). Since then, more and more pterosaurs have been reported (Ji and Ji, 1998; Wang and Lü, 2001; Wang et al., 2002, 2005; Wang and Zhou, 2003, 2004; Lü, 2003; Ji et al., 2004; Lü and Ji, 2005a, b; Dong and Lü, 2005; Lü and Yuan, 2005; Lü and Zhang, 2005; Lü et al., 2006). Because Eosipterus yangi lacks skull, it is difficult to resolve its relationships to other pterodact…     

六盘山盆地白垩系马东山组泥页岩稀土元素地球化学特征及地质意义

以六盘山盆地白垩系马东山组泥页岩为研究对象,通过稀土地球化学元素测试分析,结果表明六盘山盆地马东山组泥页岩REE为125.2×10-6～175.1×10-6,均值为153.4×10-6,略低于北美页岩;∑LREE为114.4×10-6～160.6×10-6,均值140.2×10-6,∑HREE值为10.78×10-6～...     

东营凹陷牛38井沙三段高分辨率旋回地层研究

自然伽玛测井资料取自山东省东营市胜利油田的牛38井。该井的沙河街组划分为四个段,其中沙三段依据含艾氏鱼群组合的鲱科化石和沉积物旋回堆积速率(AR)等研究,可与北美始新统绿河组进行对比。根据上世纪90年代沙三段古地磁研究结果,井深3263m处C18n.1n/C18n.1r界线调整为38.975MaBP。通过频谱分析和数字滤波计算,得出了沙三段几个界线的年龄值,其中,在沙三下、中亚段界线算出的36.9MaBP,岁差旋回幅度有明显变化,这一变化与Palike(Palikeetal.,2001)在ODP71线1052孔中发现的类似图像(36.7Ma)可比较。     

The Distribution of Chadian and earliest Arundian strata in North Wales: Implications for Dinantian (Carboniferous) lithostratigraphy and palaeogeography

The late Chadian Foel Formation, previously thought to be confined to the Dyserth area of North Wales, forms a poorly exposed but persistent basal unit to much of the Dinantian crop east of the Clwydian Range, necessitating a revision of the local lithostratigraphy. The formation comprises a peritidal heterolith which, together with the lowest few metres of the overlying Llanarmon Limestone, yields microfossil assemblages diagnostic of the Eoparastaffella Cf4α Subzone. Succeeding strata, containing the lowest archaediscid foraminifera, provide the first record of Cf4β assemblages from North Wales and establish an early Arundian age for these beds. The Foel Formation was deposited as an aggradational sequence on the northern flank of St. George's Land during a pulsed transgression which began in late Chadian times. The widely recognized basal Arundian transgression is represented by the contact between the Foel Formation and overlying platform carbonates. The latter overlap the Foel Formation in the southernmost part of the Clwydian crop demonstrating, for the first time, southwards onlap on the northern side of the Bala–Bryneglwys Fault System.