西藏日喀则地区恰布林组物源分析

长期以来，沿西藏雅鲁藏布江南岸呈东西向展布的恰布林组砾岩，被认为是造山期后磨拉石的产物，而被置于第三纪。由于在屯穷紫色泥岩底部灰绿色粉砂质灰岩中发现腹足类化石Ｋａｔｏｓｉｒａｓｐ．，并结合其他地质证据，可以确定该组时代属于早中侏罗世。结合岩石学特征、典型砾岩中砾石的岩石地球化学和物源区分析表明，恰布林组砾岩的砾石有相当一部分来自蛇绿岩，其特征明显不同于现今的雅鲁藏布江蛇绿岩。因此认为雅鲁藏布江存在早中侏罗世之前的古蛇绿岩。     

中侏罗世枫杨属果序化石的发现及意义

华北燕辽地区中侏罗世植物群中的一段枫杨属Ｐｔｅｒｏｃａｒｙａ果序化石，其形态、结构及习性，与现代枫杨属枫杨组Ｓｅｃｔ．Ｐｔｅｒｏｃａｒｙａ各种的果序酷似．这一事实表明：中侏罗世的枫杨属已具有现代水平，而自中侏罗世至现代，该属变异甚微；该属在中侏罗世之前已经过长期演化．这与研究同一侏罗纪化石植物群中的鼠李科植物时所见情况相同．显然，柔荑花序植物及木兰型植物在中侏罗世或更早的时代，已共生于中国北部，不能排除枫杨属，或连同胡桃科的其他属，曾于中生代之前起源于华北     

Lithostratigraphy and faunal aspects of marine Jurassic rocks in Thailand

Thai marine Jurassic rocks are well exposed in the Mae Sot, Umphang, and Phop Phra areas, less extensively near Mae Hong Son, Kanchanaburi, Chumphon, Nakhon Si Thammarat and Krabi. Generally they rest unconformably on Permian and Triassic, and are overlain by Quaternary strata. Fourteen lithostratigraphic units are defined (in ascending order): Pa Lan, Mai Hung, Kong Mu formations of the Huai Pong Group-Mae Hong Son area; Khun Huai, Doi Yot, Pha De formations of the Hua Fai Group-Mae Sot area; Klo Tho, Ta Sue Kho, Pu Khloe Khi, Lu Kloc Tu formations of the Umphang Group-Umphang area; and Khlong Min Formation-Chumphon, Nakhon Si Thammarat, and Krabi areas. Dominant widespread mudstones, siltstones and sandstones; limestones are confined to the Mae Sot, Phob Phra, Umphang, Kanchanaburi and Mae Hong Son areas; marls are found only in Mae Sot. Sequences are approximately 900 m thick (Mae Sot), 450 m thick (Umphang) and thinner elsewhere, especially the south. Based on ammonites, brackish to marine bivalves, and foraminifera, the beds are dated mainly as ToarcianEarly Bajocian.     

羌塘盆地中晚侏罗世旋回地层初步分析

羌塘盆地是中国海相侏罗系最为发育的地区之一,对该套地层开展了旋回地层学研究,初步的研究结果表明羌塘盆地中上侏罗统至少存在四种旋回类型,即沉积旋回、古生物旋回、地球化学旋回和磁化率旋回,并按级别将低频旋回划分为3个旋回级次.其中一级旋回是由顶底不整合面限制的一个总体向上变粗变浅的充填序列,持续时间为48 Ma;二级旋回显示为大型的海进-海退旋回,旋回的时间跨度为27～29 Ma;三级旋回显示为向上变粗或向上变细的不完整旋回,旋回的时间跨度为7～14 Ma.古生物旋回、地球化学旋回(碳氧稳定同位素、微量元素)和磁化率旋回与沉积旋回具有良好的响应,并与特提斯同期低频旋回具有很好的对比性.     

藏北改则—色哇地区的蛇绿岩特征

藏北改则-色哇缝合带的蛇绿岩,与特罗多斯、岛湾的蛇绿岩剖面对比,区别是厚度小和缺乏席状岩墙。该区的变质超镁铁岩属阿尔卑斯橄榄岩-蛇纹岩组合,其化学成分与玄武岩互补,说明玄武岩浆系地幔岩分熔的产物。     

Geochemistry and petrogenesis of Jurassic high Sr/low Y granitoids in eastern China: Constrains on crustal thickness

The Jurassic high Sr/low Y granitoids in eastern China are characterized by high Sr/Y (27—166) and La/Yb (14—66) ratios, low abundance in Y (6—21 μg/g) and Yb (0.5—2.0 μg/g), comparable with those of adakites defined by Defant et al. Thus, they were recently considered as adakitic rocks by some researchers. Compared with the typical adakites in circum-Pacific margins, however, these high Sr/low Y granitoids have higher K₂O (-3.5%) but lower Al₂O₃ (-16.0%) as well as lower Mg^# (-38) and δ Sr_N (-1.23) values. Furthermore, they show relatively flat HREE patterns with Y/Yb values of -10 close to the chondritic value. These geochemical characteristics indicate a residue mineral assemblage of hornblende, garnet and plagioclase for these high Sr/low Y granitoids melt. Thus, they were generated by partial melting at 9—13 kbar (30—45 km in depth), similar to the Archaean high-Al TTG rather than the modern adakites. Generation of these high Sr/low Y granitoids cannot be considered as evidence for a thickened crust (>50 km) and/or the presence of the “Eastern China Plateau” in Jurassic.     

柴达木东部侏罗系源岩生油组分荧光特征

通过显微荧光分析与光度学研究 ,探讨了柴达木盆地东部侏罗系源岩的生烃意义 ,指出了其主要生油组分的类型、特征、生烃贡献、热演化特征及源岩中存在的排烃现象。研究表明 ,柴达木盆地东部侏罗系源岩有暗色泥岩、油页岩、煤及碳质泥岩等 4种类型 ,其中生油组分含量与生油组分种类存在着显著差别。主要生油组分为腐泥组、壳质组和矿物 -沥青基质 ,生油组分荧光特征差异是其生烃潜力大小、热演化程度及降解情况的综合反映。生油组分荧光特征反映出该区源岩整体处于低熟阶段 ,对于寻找油气资源勘探靶区具有指导意义     

准噶尔盆地昌吉凹陷西斜坡侏罗系层序地层特征

在对地震、岩心、钻井、测井及分析化验资料综合分析的基础上 ,研究了准噶尔盆地昌吉凹陷西斜坡侏罗系的层序地层特征。结果表明 ,工区内侏罗系本身构成了一个由低水位、湖侵和高水位体系域组成的二级层序 (超层序 ) ,超层序的顶、底界面分别是侏罗系与三叠系、侏罗系与白垩系的区域性不整合面。根据层序内局部不整合面的分布范围、地层叠置样式 ,识别出 4个三级层序。由于侏罗系沉积时期受振荡性构造运动的影响 ,三级层序的发展不完整。除了层序 1发育低水位和湖侵体系域外 ,其他 3个层序均由湖侵和高水位体系域组成。超层序的低水位体系域 (相当于八道湾组下段 )发育湿地扇扇前河流平原沉积体系。湿地扇辫状沟道中的粗粒碎屑岩是该区的有利储层 ,与上覆煤层或炭质泥岩配置可形成优质储盖组合。湖侵体系域发育三角洲或滨浅湖沉积 ,高水位体系域发育辫状河沉积。     

影响侏罗纪双壳动物群分异度的主要因素

古大西洋地区侏罗纪双壳动物群分异度的变化主要受沉积相的多样性和相类型、温度梯度、盐度以及海平面变化的影响．在这些环境因素的控制下，双壳类分异度的分布特点主要表现在：①位于中纬度地区的法国北部和英国南部地区分异度值最高，由此向南向北逐渐降低；②低纬度地区的分异度高于高纬度地区；③尽管经历了２次下降期，在Ｋｉｍｍｅｒｉｄｇｉａｎ期前双壳类分异度总的变化趋势是逐渐增高的，并在Ｋｉｍｍｅｒｉｄｇｉａｎ期达到最大．此后，开始第３次下降期     

Aspects of Romanian Early-Middle Jurassic palaeobotany and palynology. Part VII. Successions and floras

The Jurassic floras of Romania occur in the Carpathian Mountains and in Dobrogea (Eastern Romania). In the South Carpathians, diverse and well preserved floras have been recorded since the middle of the 19th Century in the Resita, Sirinia, Presacina, CernaJiu, Holbav and Cristian Basins. The ages of these floras range between Hettangian and Sinemurian, with representatives belonging to Bryophytes, Pteridophytes and Gymnosperms. Excellent preservation and diversity were recorded in Anina, in the central area of the Resita Basin, a possible fossile-Lagerst?tte locality. The 3D collecting opportunities due to underground coal mining permitted detailed phytostratigraphical studies. These studies showed a floral change at the Hettangian-Sinemurian boundary, related to climate change. The Jurassic coal basins of the South Carpathians show both intramontainous and paralic features. The Resita Basin is a typical intramountainous depression basin, while the other basins are influenced by the marine realm. From a paleogeographical point of view, the Romanian Early and Middle Jurassic floras occurred on the northern frame of the Tethys realm, floristic features indicating the Eurosinian Province. One of the closest floras in terms of floristic similarities is the Iranian Early Jurassic flora. In the Apuseni Mountains, the HettangianSinemurian flora is less well-preserved and diverse than those of the South Carpathians. The Middle Jurassic flora of Romania is confined to Dobrogea (Eastern Romania), where a bennettite-dominated assemblage with low diversity and preservation was recorded.