New Zircon SHRIMP U-Pb Ages of the Langjiu Formation Volcanic Rocks in the Shiquanhe Area, Western Lhasa Terrane and their Implications

<正>Objective The potassic and ultrapotassic rocks relating to the India-Eurasia collision and continual plate convergence are widely distributed in the Lhasa terrane.These rocks are very important to understand the deep processes of the India-Eurasia collision and the uplift and evolution of the Tibetan Plateau.Although high-potassic volcanic rocks are also exposed in the western Lhasa terrane,their formation     

A marginal revenue equilibrium model for spatial water allocation

The outside water is transported into the water-shorted area. It is allocated among many sub-areas that composed the water-shorted area, in order to maximize the total benefit from the input water for the areas. This paper presents a model for spatial water allocation based on the marginal revenue of water utilization, taking the six southern districts of Hebei Province as an example.     

TJ-2体应变传感器传递函数测试

为对TJ-2体积式应变传感器传递函数做测试,设计传递函数测试装置,介绍传递函数估计方法,给出传感器输出接10 Hz低通滤波器和无滤波时传递函数拟合结果,并对测试结果和测试装置问题进行分析。测试结果表明,该传感器输出频带大于10 Hz,可应用于动态信号观测。     

山东莱芜胡家庄地区稀土矿流体包裹体特征及成矿条件

胡家庄稀土矿床位于莱芜弧形断裂弧顶的北侧,该文重点研究稀土矿床石英矿物中的流体包裹体特征。研究表明,流体包裹体以气液两相H2O包裹体为主,均一温度主要集中119.1～233.2℃。盐度变化范围大致分布在8.1～22.4 wt%,平均16.2%,成矿流体盐度为中低盐度流体;密度变化于0.9～1.1 g/cm3,平均1.02 g/cm3;成矿压力范围在30～95 MPa,平均62.5 MPa,推断矿床成矿压力环境为中低压环境,矿床成矿深度范围为2.5～3.5 km。     

TJ-2体积式应变仪器网络化实现

为适应中国地震局"十五"前兆仪器总体设计的要求,对TJ-2体积式应变仪实现网络化功能进行了开发.本文介绍了网络化仪器的硬件设计、采用的操作系统和功能软件,并介绍了在TJ-2体积式应变仪仪器上的具体应用.     

体积式钻孔应变仪的标定研究

介绍了体积式钻孔应变仪的结构原理,分析计算了仪器的热标定.通过别尔采夫滤波去掉仪器产出数据中的低频趋势变化,求得M2波潮汐因子,并利用潮汐因子对仪器数据进行校正.     

Cytogenetic analysis in two scallops (Bivalvia: Pectinidae) by PRINS and PI banding

Cytogenetic analysis was performed for the bay scallop(Argopecten irradians Lamarck 1819) and the Japanese scallop(Patinopecten yessoensis Jay 1857) by primed in situ labeling(PRINS) and propidium iodide(PI) banding techniques.The PRINS analysis revealed that major rRNA genes were clustered in two loci on the telomeric regions of the short arms on two acrocentric chromosome pairs in A.irradians and on two submetacentric pairs in P.yessoensis.The histone H3 gene sites differed in number and location between these two species.The C-band-like patterns revealed by PI staining varied considerably between these two species.A.irradians displayed terminal bands at long arms on all chromosomes,centromeric bands on some pairs and interstitial bands on five pairs.P.yessoensis exhibited only centromeric bands on all chromosomes.These results would contribute to the better understanding of karyotype evolution in A.irradians and P.yessoensis.     

气候变化和人类活动对白洋淀上游水源区径流的影响

白洋淀是华北平原最大的湖泊湿地,对维持华北平原生态平衡具有极其重要的作用。近年来,白洋淀流域水源减少已经引起了严重的生态环境问题,本文以唐河上游流域为例,根据流域内1960-2008 年水文气象数据,采用气候弹性系数和水文模拟方法,研究了气候变化和人类活动对白洋淀上游水源区径流量的影响。结果表明：年径流下降趋势显著,下降速率为1.7 mm/a,且径流在1980 年前后发生了突变;气候变化对唐河上游流域径流减少的贡献率为38%~40%,人类活动对径流的减少起主导作用,为60%~62%。为维持白洋淀的生态功能,必须保证一定的最小生态需水量,开展湿地生态用水调度与监管。     

新疆夏季对流性降水时空分布特征及成因分析

利用1979—2016年ERA-Interim再分析数据对新疆地区夏季对流性降水的时空分布特征及环流成因开展了研究。结果表明:(1)新疆夏季降水主要集中在山区,对流性降水占总降水的比例在50%上下,在大部分盆地地区,对流性降水占比达70%以上;(2)对流性降水EOF第一模态表现为塔里木盆地西侧山区和伊犁及天山北麓的反相位变化,这种分布在21世纪00年代以前存在5年和10年左右的周期,而从1995年开始出现突变。而大范围降水塔里木盆地南侧山区和天山区域是同相位的空间型分布;(3)水汽条件和层结不稳定条件的差异共同作用导致了塔里木盆地西侧和伊犁两个地区夏季对流性降水反相位的变化。