贝加尔裂谷带通京盆地呼兰霍博克火山的玄武岩岩石学和地球化学特征

位于贝加尔裂谷带西南端通京盆地的呼兰霍博克火山为玄武岩质碎屑锥,玄武岩由高拉长石、贵橄榄石、普通辉石和火山玻璃组成,其矿物组成及SiO2-（Na2O＋K2O）图和Hf-Th-Ta图指示为碱性玄武岩.CIPW标准矿物特征、岩石化学成分和单斜辉石化学成分特征表明岩石属碱性系列,钠质型.稀土元素和微量元素的地球化学特征表明岩石为裂谷初期玄武岩.初步推断原始岩浆来源于上地幔,斑晶可能于16.5 km深处的次生壳层岩浆房结晶.     

The effect of temperature on the seepage transport of suspended particles in a porous medium

The main purpose of this study is to experimentally investigate the effect of temperature on the seepage transport of suspended particles (SP) with a median diameter of 10–47 μm in a porous medium for various seepage velocities. The results show that the rise of temperature accelerates the irregular movements of SPs in the porous medium and reduces their migration velocity. As a result, the pore volume corresponding to the peak value of the breakthrough curves is apparently delayed, and the peak value in the effluent is decreased. The migration velocity of SPs decreases with increasing particle size, regardless of the Darcy velocity and temperature. The longitudinal dispersivity of SPs decreases slightly with increasing temperature and then remains almost unchanged. Larger particles experience more irregular movements induced by the limit of pore size, which leads to a larger dispersivity. The deposition coefficient increases with increasing temperature, especially in the case of a high seepage velocity, and then tends to be stable. The deposition coefficient for large‐sized particles is higher than that for small‐sized particles, which can be attributed to the restriction of large‐sized particles by the narrow pores in the porous medium. The recovery rate decreases slightly with the increase of temperature until a critical value is reached, beyond which it remains almost unchanged. In summary, temperature is a significant factor affecting the transport and deposition of SPs in the porous medium, and the transport parameters such as particle velocity, dispersivity, and deposition coefficient.     

蓟县盘山花岗岩岩体成矿地质特征研究

文章通过对蓟县盘山地区已有的1∶5万区域地质调查、物化探资料和大比例尺的矿山勘查资料进行综合研究,发现盘山岩体的矿化类型在空间上呈现规律性分布,矿化几乎全部集中于岩体与围岩的内外接触带上。矿化具有水平分带性,岩体内带发育有中高温含钨石英脉型小型矿床,岩体边部外接触带内侧发育夕卡岩型的磁铁矿、含铜磁铁矿等,岩体外接触带外侧发育有夕卡岩型钼、铜矿,岩体外接触带最外侧发育有热液型铅锌、银矿等。盘山岩体的成矿作用主要受温压条件控制,并受制于含矿溶液性质、构造条件和围岩条件,成矿具有多阶段性和多期性。     

Determination of Unknown Compound in Aromatics by FT-ICR MS with Various Ionization Techniques

<正>Electrospray ionization(ESI)coupled with Fourier transform ion cyclotron resonance mass spectrometry(FT-ICR MS)is a powerful technique capable of detecting heteroatom compounds,present in trace quantities in crude oil and its products without prior sample pretreatment.It enables the assignment of a unique elemental composition to each peak in the mass spectrum     

内蒙古山洞台站背景噪声特征分析

计算内蒙古测震台网2019-12~2020-11山洞观测数据的加速度功率谱密度（PSD）和相应的概率密度函数(PDF),研究相应台站的背景噪声特征。结果表明,高频段背景噪声的昼夜差异显著,疫情防控期间噪声水平明显低于其他时段;次级微震频段背景噪声季节性变化显著,噪声水平冬季强、夏季弱,随着台站离海岸线距离增大,PSD峰值有逐渐减小的趋势;主微震频段背景噪声在10~20 s均有峰值,峰值冬季最强,春、夏、秋季基本没有差异,不同台站同一季节峰值差异小;长周期段噪声水平四季差异不大,春、夏季略高于秋、冬季。     

河北省长城沿线县域旅游产业集聚对经济增长的空间溢出效应研究

通过2015—2019年河北省长城沿线县域旅游产业集聚水平测算,归纳河北省长城沿线县域旅游集聚现状特征,并在地理权重矩阵的基础上采用探索性空间数据分析,探究各县域人均GDP的区域分异规律,运用空间计量经济学模型探讨县域旅游产业集聚对经济增长的空间溢出效应。结果表明：(1)河北省长城沿线县域的旅游集聚差异整体上呈现收敛态势;(2)人均GDP的空间正相关性显著,空间集聚度大体呈现稳中有降,且逐渐向均衡态势发展;(3)县域间人均GDP正向空间溢出效应明显;旅游集聚正向效应显著,是影响人均GDP的重要因素。基于以上分析提出相应建议,有利于县域间旅游经济活动的合作与竞争,对于长城的保护与传承也具有重要意义。     

Intensification of decadal and multi-decadal sea level variability in the western tropical Pacific during recent decades

Previous studies have linked the rapid sea level rise (SLR) in the western tropical Pacific (WTP) since the early 1990s to the Pacific decadal climate modes, notably the Pacific Decadal Oscillation in the north Pacific or Interdecadal Pacific Oscillation (IPO) considering its basin wide signature. Here, the authors investigate the changing patterns of decadal (10–20 years) and multidecadal (>20 years) sea level variability (global mean SLR removed) in the Pacific associated with the IPO, by analyzing satellite and in situ observations, together with reconstructed and reanalysis products, and performing ocean and atmosphere model experiments. Robust intensification is detected for both decadal and multidecadal sea level variability in the WTP since the early 1990s. The IPO intensity, however, did not increase and thus cannot explain the faster SLR. The observed, accelerated WTP SLR results from the combined effects of Indian Ocean and WTP warming and central-eastern tropical Pacific cooling associated with the IPO cold transition. The warm Indian Ocean acts in concert with the warm WTP and cold central-eastern tropical Pacific to drive intensified easterlies and negative Ekman pumping velocity in western-central tropical Pacific, thereby enhancing the western tropical Pacific SLR. On decadal timescales, the intensified sea level variability since the late 1980s or early 1990s results from the “out of phase” relationship of sea surface temperature anomalies between the Indian and central-eastern tropical Pacific since 1985, which produces “in phase” effects on the WTP sea level variability.