西准噶尔巴音达拉地区卡拉岗组火山岩锆石U-Pb年代学、地球化学及其地质意义

西准噶尔巴音达拉地区发育一套酸性火山岩,被称为卡拉岗组,岩石组合以流纹岩、英安岩、流纹质熔结凝灰岩等酸性火山岩为主。本文对卡拉岗组火山岩进行高精度锆石LA-ICP-MS U-Pb测年,获得英安岩和流纹岩的加权平均²⁰⁶Pb/²³⁸U年龄分别为（294.4±1.3）Ma（n=9,MSWD=0.8）和（298.4±2.5）Ma（n=9,MSWD=3.4）,其形成于早二叠世。岩石地球化学特征表明,卡拉岗组火山岩岩具有高硅（66.69%~75.21%）,富碱（Na₂O+K₂O：6.98%~8.35%）,低MgO（0.18%~1.32%）,贫钙（0.24%~2.49%）的特征,均属过铝质（A/CNK：1.14~1.33）及高钾钙碱性系列。微量元素数据显示,稀土总量为∑REE为83.82×10^-6~197.61×10^-6,（La/Yb）_N=3.15~12.50,轻、重稀土元素分馏比较明显,轻稀土元素（LREE）较为富集,重稀土元素分布相对平坦,球粒陨石标准化配分模式为右倾型。微量元素富集大离子亲石元素（LILE）Rb、Th、U、K,并亏损高场强元素（HFSE）_Nb、Ta、P、Ti。综合最新区域资料及本文研究成果,文章认为研究区早二叠世卡拉岗组火山岩岩浆来源于壳源物质不同程度的部分熔融,残留相中有少量斜长石和角闪石,为后碰撞伸展阶段的产物。     

多核处理器的机载激光雷达点云并行三角网渐进加密滤波方法

滤波是机载LiDAR点云数据处理的关键步骤之一,点云数据的海量化特性使得一般的串行化滤波处理方法无法满足快速成图的应用需求。提出一种基于多核计算技术的并行三角网渐进加密滤波方法,将串行方法中最耗时的三角网构建与脚点判别过程进行了并行化改造。三角网构建算法的并行化基于分治法实现,脚点判别算法的并行化采用一种随机分配策略将三角网划分为多个离散分布的三角形子集合来实现负载均衡。并行滤波方法在8核环境下多次渐进加密的实际加速比达到3.1左右。试验证明,该方法可以充分发挥多核计算优势,并且对不同分布形态点云数据具有良好的适应性。     

泉州湾桐花树和老鼠簕根际土壤细菌和真菌群落特征比较

红树植物根际土壤微生物对近海生物地球化学循环及其生物多样性等起着重要作用,受地上部和土壤性质影响,两种不同药用红树植物桐花树（Aegiceras corniculatum）和老鼠簕（Acanthus ilicifolius）根际土壤微生物群落组成可能存在独特性。本研究分别以细菌 16S rRNA基因和真菌ITS 基因为分子标记,采用高通量测序技术分析比较了桐花树和老鼠簕根际土壤微生物多样性特征及其与土壤理化性质之间的关系。结果表明：①老鼠簕根际土壤细菌和真菌多样性与丰富度均显著高于桐花树,且两者之间的细菌和真菌组成皆存在明显差异（P<0.05）;②两者根际土壤细菌和真菌门和属的优势（大于1%）物种组成皆相似;在门水平,桐花树根际土壤主要优势物种变形菌门（Proteobacteria）和未分类门（unclassified_k_Fungi）的相对丰度显著高于老鼠簕,而拟杆菌门（Bacteroidota）、脱硫杆菌门（Desulfobacterota）、子囊菌门（Ascomycota）和担子菌门（Basidiomycota）则相反;在属水平,桐花树的主要优势物种硝化螺菌属（Nitrospira）和Denitromonas属的相对丰度显著高于老鼠簕,而枝孢菌属（Cladosporium）和囊状担子菌属（Cystofilobasidium）则相反;③桐花树根际土壤pH、总碳和总酚含量皆显著高于老鼠簕,pH和总酚显著影响细菌群落组成,而总碳和总硫则显著影响真菌群落组成;此外,pH、总碳和总氮是影响细菌物种的主要因素,而总酚、pH和总碳是影响真菌物种的主要因素。本研究揭示了桐花树和老鼠簕根际土壤细菌和真菌多样性存在明显差异并与土壤理化性质密切相关,可为今后从不同红树物种所具备的独特功能根际微生物菌群来开发相关资源及保护近海的生态环境提供新的视角。     

基于地质异常的内蒙古新达来草原覆盖区钼铜多金属矿产定量预测

内蒙古新达来草原覆盖区位于古亚洲成矿域的二连—东乌旗钼铜多金属成矿带西段,分布有乌兰德勒、准苏吉花等与中酸性侵入体有关的内生金属矿床,成矿地质条件优越.然而,因受牧草和第四系大面积覆盖的影响,该区各种成矿/示矿信息具有间接、叠加、隐蔽、微弱、不完整等特点,给找矿勘查带来更大的不确定性和风险.因此,必须加强矿产定量预测研...     

不同升温阈值下中国地区极端气候事件变化预估

本文基于耦合模式比较计划第五阶段(CMIP5)的18个全球气候模式的模拟结果,预估了全球平均气温在不同典型浓度路径(RCPs)下达到2℃、3℃和4℃阈值时,中国地区气温和降水的变化,并采用了具有稳定统计意义的27个极端气候指标定量评估了全球平均气温达到不同阈值时,中国地区极端气候事件的可能变化。结果表明,未来我国平均气温增幅将高于全球平均增暖,极端暖事件(如暖夜、暖昼、热带夜)明显增多,达到4℃阈值时,暖夜指数相比参考时段增加约49.9%。极端冷事件(如冷夜、冷昼、霜冻)减少。随全球气温升高,中国北方平均降水增多。在不同升温阈值下,中国地区降水的极端性都体现出增强的趋势,强降水事件发生频率(如中雨日数、大雨日数)和强度(如五日最大降水量、极端强降水量)都明显增加。随升温阈值的升高,这些变化幅度更大,在 RCP8.5 情景下全球升温 3℃和4℃时,中国平均五日最大降水分别增加 12.5mm和17.0mm。我国西南地区极端降水强度的增幅高于其他地区。     

三维高密度电法在土石坝渗漏探测中的应用

正高密度电法是以地下空间内地质体之间的电阻率差异为研究对象,按照协定的观测系统进行供电与测量,把收录到的地电数据体进行去噪、计算、分析以及表达,从而揭示出地下介质的空间分布及变化特征(严加永等,2012)。目前,高密度二维电阻率成像在水库大坝渗漏隐患探测中得到广泛的应用,为土石坝病害的治理及安全评价提供了有的放矢的靶区,但大坝渗漏病因复杂、     

Simulation of the Power Take-off System for a Heaving Buoy Wave Energy Converter

The heaving buoy wave energy device is popular for wave conditions with small wave heights and short periods. This paper presents the design of a wave ener     

Petrography and geochemistry of the Paleogene sandstones from the Ningnan Basin,NW China: implications for provenance,weathering and tectonic setting

Petrographical and geochemical characteristics of the Paleogene sandstones in the Ningnan Basin, NW China, were studied by analyzing thin sections and major, trace, and rare earth element (REE) compositions. The sandstones of the Sikouzi and Qingshuiying formations are sublitharenite to feldspathic litharenite and characterized by low-medium compositional and textural maturity. Petrographic provenance study indicates a quartzose-recycled provenance with higher concentration of Zr in the Qingshuiying Formation. Depositional environment of the Sikouzi and Qingshuiying sandstones was mainly oxic as evidenced by lower values of δEu, δCe, V/Cr, Ni/Co, U/Th, and δU. The Chemical Index of Weathering (CIW’) and the Th/U ratios (av. 3.3 and 3.54) reveal weak and moderate weathering history in the source area. The Zr, Nb, Y, Th, and U concentrations in the Qingshuiying Formation are comparable to upper continental crust (UCC) values and the negative Eu anomalies support contribution from a felsic source. However, a significantly larger range of Ce anomalies in the Sikouzi Formation also reveals mixing of felsic and mafic/ultramafic source terrains. The petrology and geochemistry analyses of the Sikouzi sandstones imply that the provenance was mainly derived from diabase in Xiang Shan and lower Cretaceous strata in the study area whereas the Qingshuiying sandstones were derived from the granites in the southern part of Liupan Shan, which means that the northeastward expansion of the Tibetan Plateau did not make the Liupan Shan a high relief during Paleogene. The present study has let to document the origin of the Ningnan Basin that was formed during the late phase of Ordos Basin reformation, along with the other synchronous peripheral fault-bounded basins of the Ordos Basin, and was not related to the northeastern extrusion of Tibetan Plateau.     

Mechanism of Underground Fluid Injection Induced Seismicity and Its Implications for CCS Projects

CO₂ capture and storage projects must consider the potential possibility ofinjection induced seismicity. Moderate earthquakes and strong earthquakes may endanger human life and property, and even felt earthquakes and microquakes also pose a threat to seal integrity of CO₂ reservoir and increase the risk of leakage. Underground fluid injection induced seismicity usually happens in some geoengineering projects such as waste fluid disposal, EOR and EGS, and it occurs when fluid is injected along the fault. Therefore, it can be studied through stress analysis. The density of supercritical CO₂ is smaller than water, which may develop density flow in the deep strata or water-rock interactions in pre-existing structures, and cause the variation in permeability and pressure to induce a seismic activity. In this paper, we reviewed the mechanism of underground fluid injection induced seismicity with the focus of CCS, combined with fluid injection projects and seismic monitoring analysis in both commercial scale and experimental scale, to investigate its impact on the integrity of the cap rock of the reservoir. Finally, we summarized the appropriate site selection, injection methods and monitoring programs to prevent the occurrence of induced seismicity.