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安徽省庐枞盆地龙桥铁矿床深部辉长闪长岩的发现及其意义 总被引:1,自引:0,他引:1
龙桥铁矿床是安徽省庐枞矿集区中大型铁矿床。矿床主矿体呈似层状赋存于三叠系东马鞍山组泥灰岩、角砾状灰岩、白云岩、泥质粉砂岩和石英砂岩中,前人研究认为矿区内正长岩侵入体与成矿关系密切。随着龙桥矿床的生产勘探,在矿区0线井下巷道开拓发现了辉长闪长岩侵入体。辉长闪长岩岩体呈岩株状产出,被正长岩体穿切破坏,靠近矿体部位发育透辉石矽卡岩化蚀变。辉长闪长岩主要造岩矿物为辉石和斜长石,角闪石较少,根据矿物组合将其定名为辉长闪长岩。本文通过综合分析初步认为,辉长闪长岩与可能与铁成矿作用关系密切,而正长岩为成矿期后破矿岩体,研究结果为龙桥铁矿床的成因提供了新的证据, 相似文献
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选择位于南沙台地的NS93-5钻孔进行地磁场相对强度的研究.根据氧同位素地层学(MIS1~MIS5),建立130 ka以来的沉积序列.岩石磁场研究表明,沉积物中的磁性矿物主要为1~15μm的细粒磁铁矿,磁性矿物浓度的变化在同一数量级之内,而且沉积物磁性比较稳定.选择NRM/x作为相对磁场强度的估计指标,发现在10~100ka时间尺度上,可以很好地进行全球对比,千年时间尺度上尽管有一定的误差,但也可以进行有效对比.130ka以来,有4次强度变化的低谷,分别发生在32.5~40 ka、44~52.5 ka、6 相似文献
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黔北桐梓红花园地区的五峰组是华南地区奥陶系的重要剖面之一,在其以泥质灰岩为特征的五峰组观音桥段下部黑色含炭质钙质页岩和褐色粉砂岩中分别产有较为丰富的双壳类Modiolopsis和腹足类Holopea。产双壳和腹足类的地层中岩性和生物具有差异性,表明观音桥段沉积早期的沉积环境具有多变的特征。横长卵形、较膨凸的Modiolopsis和其两瓣壳相连保存的标本表明为近原地埋藏,为弱水动力、有氧的、较浅水环境的软质基底。丰度较大的低圆锥形Holopea的不规则的壳顶指向指示了具一定水动力的、沙性基底的浅水环境。 相似文献
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KONG Xu LIN Lin LI Jin-rong ZHOU Xu ZOU Hu LI Hong-yu CHEN Fu-zhen DU Wei FAN Zhou MAO Ye-wei WANG Jing ZHU Yi-nan ZHOU Zhi-min 《Chinese Astronomy and Astrophysics》2014
In recent years the number of worldwide 8∼10 m-class ground-based telescopes is continually increased, the 4 m-diameter or smaller telescopes have become the small and medium-sized telescopes. In order to obtain some noticeable scientific results by using these existing small and medium-sized telescopes, we have to consider very carefully what we can do, and what we can not. For this reason, the Time Allocation Committee of the 2.16 m telescope of the National Astronomical observatories of China (NAOC) has decided to support some key projects since 2013. The long-term project “Spectroscopic Observations of the Star Formation Regions in Nearby Galaxies” proposed by us is one of three key projects, it is supported by the committee with 30 dark/grey nights in each of three years. 相似文献
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利用卫星遥感高光谱AIRS数据, 获取了发生在青藏高原周缘三个不同构造单元的2017年8月九寨沟MS7.0地震、 2019年4月西藏墨脱MS6.3地震和2020年6月新疆于田MS6.4地震伴生的CH4气体地球化学异常。 用Matlab编程处理AIRS数据的结果表明, CH4柱含量在三次地震前一周到半个月出现高值异常, 异常沿着断裂带分布, 其中断裂带的交会部位异常幅度较大。 由于地震所处的构造环境、 发震类型、 震级大小差异, 三个构造单元地震引起的CH4气体浓度异常出现时间、 持续时间、 异常强度等方面存在一定差异。 三次地震前后遥感信息异常与地震活动对应较好, 这归因于在孕震应力场作用下地下气体沿着裂隙及裂缝的逸散作用。 研究结果对利用卫星高光谱分辨率遥感技术监测地震及其在大地震短临预测中的应用具有重要意义。 相似文献
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The characteristics of swells within the East China Sea have been reported by Tao et al.(2017), while the question of where the swells come from remains unanswered. By using the wave model WAVEWATCH III and the swell tracking method proposed by Hanson(2001), the spatial sources of the swells are investigated during four typical typhoon scenarios, which usually affect the wave environment in the East China Sea, including the Recurving type,the Northward type, the Westward type(striking the East China Sea) and the Westward type(over the South China Sea). The numerical results show that parts of the swells are from the North West Pacific with a long-distance travelling. The moving paths of the swells are affected by the typhoon tracks, which result in various fetches. The Westward type(over the South China Sea) makes one peak in the evolution process. The landing process of the Westward type(striking the East China Sea) could result in swells with low energy. The swell energy depends on swell propagation distance, existence time and wind intensity of generation fetch. The consistent fetch and forceful wind intensity make swell carry more energy. 相似文献
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