新疆博格达—哈尔里克山晚新生代压扭性变形与隆起成山

压扭性走滑变形是陆内变形的最主要构造样式之一,并且是陆内造山系统得以形成的最基本构造样式。位于天山东部的博格达—哈尔里克山链,横亘在吐哈盆地和准噶尔盆地之间,是研究新生代山脉形成理想的野外实验室。本文结合压扭造山带的研究,通过野外地质填图、遥感解译和DEM分析,裂变径迹测试等研究,确认博格达—哈尔里克山与山脉隆起相关的断裂构造主要为北东东向和北西西向压扭性走滑断裂,认为它是晚新生代压扭造山带(transpressional orogen)。主要证据是:首先博格达—哈尔里克山与山脉隆起相关的构造变形为北东东70°走向和北西西290°走向,山脉两侧呈现向盆地方向的逆冲冲断构造,体现了近南北向为构造主压应力场特点;其次天池河床砂岩屑AFT分析出的年龄峰值集中在42.8 Ma(62.8%)、18.8 Ma(29.0%)、3.2 Ma(8.2%),表明样品所代表的流域地质体在42.8 Ma、18.8Ma、3.2 Ma经历了3次冷却事件。依据裂变径迹等年龄投影圈闭图显示博格达山裂变径迹年龄存在中间新,两边老的特点。基于相同的大地构造背景,压扭造山模式也可以解释整个天山晚新生代山脉强烈隆升。     

腾格里沙漠地区砂质管状物的发现及其地质意义

砂质管状物,浅褐色,管状,致密,硬脆,中空,内孔贯通。长度3.4～18.1cm,外径1.55～3.5cm,内径0.6～1.9 cm,壁厚1～11mm。随着长度由长到短,外径、内径及壁厚均逐渐变小。管内孔壁上时有白色微晶方解石薄膜,或有管孔被白色微晶方解石半堵塞。有的管子上有与主孔相通的小孔,小孔与管壁垂直、呈30°交角或近于相切。按砂粒粒度,管子分为粗砂型和细砂型两种,其中粗砂型管子暗色砂粒含量略多。砂粒成分主要为硅质,胶结物主要为微晶方解石,孔隙式胶结。说明在地表砂层之下存在弱承压碳酸盐型咸水,这种水的上涌、渗透作用及沙漠特有干旱、风力等条件,是其主要成因。显示古腾格里湖在干涸过程中,湖水经历了"碳酸盐型→硫酸盐型→氯化物型"的浓缩过程。如果在古代砂岩中发现相同或类似的管状物,可进一步推断,该砂岩形成环境为古沙漠、有在同一套地层中存在蒸发盐矿产的可能。     

湘西北宁乡式铁矿的成因与质量

宁乡式铁矿在湘西北主要分布在三个层位,存在两类矿石结构,这两类矿石结构的铁矿是由不同的成矿方式形成,因而矿石质量也是不同的,具体表现在两类矿石中P、SiO2的含量存在明显差异。通过分析对比,Fe0、Fe22层砾状、豆状类赤铁矿的质量优于鲕状赤铁矿,其中位于二户溪至西界地区的FeO层砾状、豆状赤铁矿矿石质量全区最佳,应为该区的赤铁矿下一步工作的主要方向。     

Geochemistry of the Jinduicheng Mo-bearing porphyry and deposit,and its implications for the geodynamic setting in East Qinling,P.R. China

Simultaneous determinations of U–Pb dating and Hf isotopes on single zircon grains by excimer laser-ablation quadrupole and multiple-collector ICP-MS and petrologic and ore geochemical studies have been applied to the ore-bearing porphyry of the Jinduicheng porphyritic molybdenum deposit in East Qinling. Lithogeochemical data show that the porphyry is characteristic of high K₂O, K-feldspar porphyritic calc-alkaline granitoids with ¹⁷⁶Hf/¹⁷⁷Hf=0.282020–0.282436 and ε_Hf(t)=?23.7 to ?8.9, which indicates its mixed origin involving a crustal and a mantle component. The weighted average U–Pb age from single zircon grains of the porphyry is 141.5±1.5 Ma. This age coincides with the oldest molybdenite Re-Os model age as dated by others, suggesting that the period of mineralization was almost simultaneous with the porphyry emplacement, or slightly later. The porphyry intrusion and the molybdenum mineralization occurred during the transition from compression to extension in the Jurassic – Cretaceous periods. The corresponding tectonic setting was the intracontinental orogenic and extension stage after collision and orogenesis between the Southern China plate and the Northern China plate. The Jinduicheng porphyry and the deposit's geochemical data indicate that the ore-forming material originated from a mixing of lower crust and upper mantle. When the molybdenum-enriched magma intruded into the upper crust along zones of structural weakness, ore-forming fluid generated by magma crystallization of the porphyry interacted with wall rock or mingled with meteoric water to form the deposit.     

Historical contamination and sources of organochlorine pesticides in sediment cores from Quanzhou Bay, Southeast China

Three sediment cores were collected from the top to the mouth of Quanzhou Bay, Southeast China, in order to establish sources and historical trends of organochlorine pesticides (OCPs) in the region. The spatial distribution of OCPs in surface sediments implies that Quanzhou Bay received the contamination inputs not only from rivers near the shore, but also from outside the bay. The variation profiles of concentrations clearly showed that OCPs were widely used between 1960s and 1980s in China. A recent increasing trend was found in all cores despite their ban in China in 1983. Different ratios of (DDD+DDE)/DDTs indicated that DDTs at the top of the bay were mainly derived from long-term weather soils, while DDTs near the mouth of the bay were mainly derived from fresh inputs from outside the bay. Higher percentage of gamma-HCH in HCHs deposited after 1990 implies that lindane may have been used recently around Quanzhou Bay.     

Pyritization of trace metals in estuarine sediments and the controlling factors: a case in Jiaojiang Estuary of Zhejiang Province,China

Three undisturbed sediment samples were collected from the intertidal zone of the Jiaojiang Estuary of Zhejiang Province, China. The sediments were found to contain remarkably low concentrations of organic carbon (<0.6%) and acid volatile sulfide (AVS) (<30 μmol g⁻¹). The availability of these two substrates likely constrained sulfate reduction and pyritization of several trace metals, respectively. This was especially true at one station where AVS concentrations in the upper 20 cm averaged less than 0.05 μmol g⁻¹. Although the depth dependence of the degree of trace metal pyritization was generally consistent with expectations based on redox conditions, depth profiles of reactive-metal and pyrite-metal concentrations in several cases revealed more complex behavior and a positive correlation between reactive-metal concentrations and pore water metal concentrations.     

利用非差资料的精密点定位方案

单站精密定位 (PrecisePointPositioning ,以下简称PPP)是在同时固定GPS精密星历和卫星钟的前提下 ,利用载波相位和伪距资料进行单台站的精密点定位 .采用该方法时不同台站之间不存在共同的待估参数 ,即各台站互不相关 ,这一特点大大降低了计算量 .采用美国喷气推进实验室JPL发展的数据处理软件GIPSY处理APSG联测资料 ,计算表明PPP的重复率相当于目前国内普遍采用的双差解算结果 .采用较好保持地面网构型的无基准算法 ,计算表明通过Helmert参考系转换后 ,PPP的解算结果与双差算法的外符精度大致相当 .解算表明 ,采用PPP处理 1 0 0个台站约需 3 .5小时 ,而处理同样的资料采用双差算法则需 1 8～2 0小时 .对于我国即将建成的大科学工程或地震监测的多达 2 0 0 0个接收机的GPS网而言 ,在保持精度前提下的节省计算资源和计算时间的PPP解算方案值得广泛的应用     

雷达发射机灯丝电源故障维修

灯丝电源是一个交流稳压电源,通过灯丝中间变压器和位于油箱中的脉冲变压器及灯丝变压器,为速调管灯丝供电.2011年7月18日,内蒙古气象局通辽天气雷达站的CINRAD/CB雷达发射机反复出现灯丝电源故障,且无法加高压导致雷达停机,经分析和排查故障原因,最终排除了雷达故障.就此次故障的出现,分析其原因,举一反三,对雷达台站在今后的工作中加强备件的管理和测试数据的管理有一定的启示.