SHRIMP zircon U–Pb and molybdenite Re–Os isotopic dating of the tungsten deposits in the Tianmenshan–Hongtaoling W–Sn orefield, southern Jiangxi Province, China, and geological implications

The southern Jiangxi Province is a major part of the Nanling W–Sn metallogenic province of southern China, where all W–Sn ore deposits are temporally and spatially related to Mesozoic granitic intrusions. The Tianmenshan–Hongtaoling orefield is a recently explored territory endowed by several styles of W–Sn mineralization. The orefield comprises three composite granitic plutons: Tianmenshan, Hongtaoling and Zhangtiantang associated with several tens of W–Sn-polymetallic ore deposits (Maoping, Baxiannao, Niuling, Zhangdou, Yaolanzhai and others) along their contacts. In this study, four new SHRIMP zircon U–Pb ages were determined for three composite granitic plutons, and 33 molybdenite samples from five W–Sn deposits were analysed by ICP-MS Re–Os isotopic method. SHRIMP zircon U–Pb ages for both medium to coarse-gained biotite granite and porphyritic biotite monzogranite from the Tianmenshan composite pluton are 157.2 ± 2.2 Ma and 151.8 ± 2.9 Ma, respectively. Molybdenite Re–Os isochron ages for the related Baxiannao fracture-controlled tungsten deposits are 157.9 ± 1.5 Ma. Maoping greisens-type tungsten deposits were emplaced at 155.3 ± 2.8 Ma and the Maoping wolframite–quartz veins at 150.2 ± 2.8 Ma, respectively. The SHRIMP U–Pb age of zircons from the Hongtaoling biotite granite is 151.4 ± 3.1 Ma whereas the molybdenite Re–Os isochron ages of the genetically related Niuling endocontact tungsten quartz veins and Zhangdou exocontact tungsten quartz veins are 154.9 ± 4.1 to 154.6 ± 9.7 Ma and 149.1 ± 7.1 Ma, respectively. The SHRIMP zircon U–Pb age of the Zhangtiantang fine-grained muscovite granite is 156.9 ± 1.7 Ma, whereas the molybdenite Re–Os isochron age for the related Yaolanzhai greisens-type tungsten deposit is 155.8 ± 2.8 Ma. These new age data, combined with those available from the literature, indicate that the ages of W–Sn ores and related granites are Late Jurassic with a peak at 150 to 160 Ma, which corresponds to the widespread Mesozoic metallogenic event in southern China. Molybdenites from this group of tungsten deposits have quite low Re contents (29.1 to 2608 ppb), suggesting continental crustal provenance of the ore metals.     

Regional effects by the construction of Suzhou Industry Garden

１　ＡＤＶＡＮＣＩＮＧＯＦＴＨＥＱＵＥＳＴＩＯＮＡＮＤＣＯＮＳＴＲＵＣＴＩＯＮＢＡＣＫＧＲＯＵＮＤＯＦＳＵＺＨＯＵＩＮＤＵＳＴＲＹＧＡＲＤＥＮＰｅｒｒｏｘｇａｖｅｓｐｅｃｉａｌａｔｔｅｎｔｉｏｎｔｏｔｈｅｅｆｆｅｃｔｏｆｉｍｐｏｒｔａｎｔｉｔｅｍｓａｎｄｃｏｎｓｔｒｕｃｔｉｏｎｏｆｉｎｆｒａｓｔｒｕｃｔｕｒｅｗｈｅｎｈｅｄｉｓｃｕｓｓｅｄｔｈｅｐｒｏｄｕｃｔｉｏｎｏｆｇｒｏｗｔｈｐｏｌｅ（Ｌｉ,１９８８）．Ｌｏｔｓｏｆｄｏｍｅｓｔｉｃｓｃｈｏｌａｒｓｈａｖｅａｌｓｏｐｒｏｂｅｄｉｎｔｏｔｈｉ…     

利用车载LiDAR点云数据提取城市道路规则多边形

随着自动驾驶高精地图的发展,准确高效地提取道路规则多边形成为必要。本文以苏州市某城市快速路为研究对象,通过使用徕卡车载激光移动测量系统获得城市道路点云数据,观察了解车载点云数据各类属性信息,根据观察结果组合利用点云数据高差、点云灰度差值、点云强度差值,在此基础上再利用网格密度法实现道路规则多边形的提取,然后通过对目标的矢量化得到三维矢量规则多边形。最后对提取的矢量化结果进行精度评定。试验结果表明:该方法在提取道路规则多边形方面能得到较好的结果且能满足高精地图需求。     

南非奥坦尼瓜盆地构造演化与油气差异分布

奥坦尼瓜盆地位于非洲大陆最南端,为典型被动大陆边缘盆地。晚侏罗世,盆地随着东西冈瓦纳大陆的解体,由非洲、南美和南极洲三大板块的裂开而形成。盆地经历了裂谷期(J3-K1凡兰吟期)、过渡期(凡兰吟期)和漂移期(K1欧特里夫期至今)三大构造演化阶段,发育漂移期下白垩统欧特里夫阶和巴雷姆—阿普特阶2套烃源岩,以Ⅱ2/Ⅲ型干酪根为主,偏生气。主要储集层为下白垩统凡兰吟阶浅海相砂岩,其次为下白垩统阿尔比阶深水浊积砂岩。圈闭发育具有典型的两分特征,裂谷期以构造圈闭为主,漂移期以构造—岩性圈闭为主。截至2014年,盆地已发现41个油气田/藏,石油可采储量2 042万m3, 凝析油可采储量2 016万m3, 天然气可采储量1160亿m3。平面上, 油气呈现西多东少的特点;垂向上,绝大多数油气发现集中在裂谷期顶部凡兰吟阶储层中。通过对盆地南部阿古拉斯走滑带的分析认为,阿古拉斯走滑带的活动是造成盆地东、西部油气富集差异的主要因素。在对盆地油气分布特征基础上,认为勘探前景区应聚焦盆地西部。     

古气候事件对刚果扇浊积水道发育的控制作用

刚果扇是渐新世以来快速堆积的巨型深水扇体,浊积水道广泛发育,油气成藏条件优越。精细标定水道集中发育的年龄、期次及其与同期地质事件之间的关联,对认识水道发育的主控因素和分布规律具有重要意义。基于测井、地震和古生物资料的综合分析,将盆地北部渐新统—中新统划分为2个二级层序、8个三级层序;通过微体古生物带和海平面变化旋回精细确定了各层序界面的年龄;进而在层序格架内明确了刚果扇北部浊积水道的发育期次和演化规律,认为刚果扇在盆地北部可划分为3个演化期次,即渐新世晚期快速填充期、中新世早—中期稳定沉积期和中新世晚期大规模水道发育期。实验研究发现,盆地中新统孢粉化石由早到晚出现水藓孢属-栎粉属、光面球藻属-盘星藻属-单束松粉属、拟桫椤孢属-凸瘤水龙骨单缝孢属、粗肋孢属-水龙骨单缝孢属-拟桦粉属4种组合类型,表明盆地中新世气候变化频繁,且大规模水道发育期与降温事件及海平面快速下降期高度吻合。此外,3次大规模水道发育期与西非海岸3次构造抬升事件关系密切。由此认为,刚果扇浊积水道的发育直接受控于降温事件,而构造隆升是源头性的触发因素。     

硅碳双键稳定性的CNDO/2法研究

本文用CNDO/2法研究了硅碳双键Si=C不稳定的原因。通过分析SiH_2CH_2的烷基和苯基取代物的计算结果,对有大基因连接硅碳双键的化合物之所以能稳定存在做了合理的说明。     

海水表面张力的研究

用最大泡压法测定大洋海水及其被纯水稀释的海水温度在１５－３５℃，盐度５－３５的表面张力，所得数据经计算机统计处理得出海水表面张力同温度和盐度之间的经验公式：σｓｔ＝７５．５９＋０．０２１３５２ｓ－０．１３４７６ｔ－０．０００２９５２９ｓｔ在分别恒定盐度、温度度时，海水表面张力与温度、盐度有很的线性关系；其温度系数和盐度系数均非常数，温度系数随盐度增加绝对值增大，而其盐度系数随温度升高而变小。     

赤鼻棱鳀松果体显微结构研究

本文用组织学方法研究了赤鼻棱鳀（Thrissapurava）松果体的形态结构，结果表明赤鼻棱鳀有松果体窗，并有发达的松果体，感光细胞聚集成团，顶突伸入终囊腔中，终囊类型为折褶型。背囊由单层细胞构成，细胞大而圆，松果体司感光内分泌功能。     

Rendering 2D Lines on 3D Terrain Model with Optimization in Visual Quality and Running Performance

With the gradual shift from 2D maps to a 3D virtual environment, various visual artifacts were generated by overlaying 2D map symbols on 3D terrain models. This work proposes a novel screen‐based method for rendering 2D vector lines with the accuracy of more than one pixel on the screen in real time. First, screen pixels are inversely projected onto a 3D terrain surface, and then onto the 2D vector plane. Next, these pixels are classified into three categories in terms of their intersection situation with the 2D lines. After that, a multiple sampling process is applied to the pixels that intersect with the 2D lines in order to eliminate visual artifacts, such as intermittence and aliasing (in pixel scale). Finally, a suitable point‐in‐polygon judgment is implemented to color each sample point quickly. The algorithm is realized in a heterogeneously parallel model so that the performance is improved and becomes acceptable.     

A new,high-resolution geoid for Canada and part of the U.S. by the 1D-FFT method

A new, high-resolution and high-precision geoid has been computed for the whole of Canada and part of the U.S., ranging from 35°N to about 90°N in latitude and 210°E to 320°E in longitude. The OSU91A geopotential model complete to degree and order 360 was combined with a 5 × 5 mean gravity anomaly grid and 1km × 1km topographical information to generate the geoid file. The remove-restore technique was adopted for the computation of terrain effects by Helmert's condensation reduction. The contribution of the local gravity data to the geoid was computed strictly by the 1D-FFT technique, which allows for the evaluation of the discrete spherical Stokes integral without any approximation, parallel by parallel. The indirect effects of up to second order were considered. The internal precision of the geoid, i.e. the contribution of the gravity data and the model coefficients noise, was also evaluated through error propagation by FFT. In a relative sense, these errors seem to agree quite well with the external errors and show clearly the weak areas of the geoid which are mostly due to insufficient gravity data coverage. Comparison of the gravimetric geoid with the GPS/levelling-derived geoidal heights of eight local GPS networks with a total of about 900 stations shows that the absolute agreement with respect to the GPS/levelling datum is generally better than 10 cm RMS and the relative agreement ranges, in most cases, from 4 to 1 ppm over short distances of about 20 to 100km, 1 to 0.5 ppm over distances of about 100 to 200 km, and 0.5 to 0.1 ppm for baselines of 200 to over 1000 km. Other existing geoids, such as UNB90, GEOID90 and GSD91, were also included in the comparison, showing that the new geoid achieves the best agreement with the GPS/levelling data.Presented at theIAG General Meeting, Beijing, P.R. China, Aug. 6–13, 1993