青海龙尾沟铜、金矿床地质特征、矿床成因及成矿远景分析   总被引：6，自引：2，他引：4  

徐善法  张汉成  陈建平  叶树民 《地质与勘探》2004,40(2):12-17

龙尾沟铜、金矿床是在青海省柴北缘成矿亚区内所取得的重大找矿突破,该矿床产于下元古界达肯大坂群(Pt1dk)地层内,并受F6断裂破碎带控制.通过对矿床地质特征、矿石及花岗斑岩脉地球化学特征研究,首次提出龙尾沟铜、金矿床是与岩浆作用有关的斑岩型矿床.从已查明铜、金矿床(体)的控矿因素和矿化特征分析,深部存在规模较大矿化体的前景,应进一步加强该地区深部勘探及研究力度,以期获得找矿的更大突破.  相似文献   

A Research on the Algorithm of Local Atomic Time     

Li Bian  Qu Li-li  Gao Yu-ping  Hu Yong-hui 《Chinese Astronomy and Astrophysics》2011,35(2):314

The goal of all time laboratories’ pursue is to produce and keep a stable, precise and reliable time scale. The long-term stability of the time scale is mainly taken into account in the traditional ALGOS algorithm, while the local atomic time scale should give consideration to both the long-term and shortterm stabilities. From the analysis and research on the atomic clock noise model and under the condition that the long-term stability of the local atomic time scale does not drop, a complete algorithm is proposed which is suitable for the calculation of the local time scale TA (NTSC) carried out at the time laboratory with the time-keeping clocks of a unitary type and being close in performance at the National Time Service Center, called the NTSC for short, of Chinese Academy of Sciences. The data of all the clocks in the NTSC which participated in the calculation of the International Atomic Time (TAI) all the year round in 2008 are applied to the test and verification of the new algorithm, with the result showing that both the short- and long-term stability indexes of the obtained TA (NTSC) are improved. The research result is suitable for the calculation of the atomic time scale of the time laboratory whose time keeping system is similar to that of the NTSC.  相似文献   

Altimeter Signal-to-Noise for Deep Ocean Processes in Operational Systems     

KIRK R. WHITMER  GREGG A. JACOBS  OLE MARTIN SMEDSTAD 《Marine Geodesy》2013,36(3-4):433-451

The ocean signal for this study is the sea surface height due to the slowly varying (greater than 5-day) ocean processes, which are predominantly the deep ocean mesoscale. These processes are the focus of present assimilation systems for monitoring and predicting ocean circulation due to ocean fronts and eddies and the associated environmental changes that impact real time activities in areas with depths greater than about 200 m. By this definition, signal-to-noise may be estimated directly from altimeter data sets through a crossover point analysis. The RMS variability in crossover differences is due to instrument noise, errors in environmental corrections to the satellite observation, and short time period oceanic variations. The signal-to-noise ratio indicates that shallow areas are typically not well observed due to the high frequency fluctuations. Many deep ocean areas also contain significant high frequency variability such as the subpolar latitudes, which have large atmospheric pressure systems moving through, and these in turn generate large errors in the inverse barometer correction. Understanding the spatial variations of signal to noise is a necessary prerequisite for correct assimilation of the data into operational systems.  相似文献   

Near-Real–Time GPS-Based Orbit Determination and Sea Surface Height Observations from the Jason-1 Mission Special Issue: Jason-1 Calibration/Validation     

《Marine Geodesy》2013,36(3-4):383-397

The Jason-1 Operational Sensor Data Record (OSDR) is intended as a wind and wave product that is aimed towards near-real–time (NRT) meteorological applications. However, the OSDR provides most of the information that is required to determine altimetric sea surface heights in NRT. The exceptions include a sufficiently accurate orbit altitude, and pressure fields to determine the dry troposphere path delay correction. An orbit altitude field is provided on the OSDR but has accuracies that range between 8–25 cm (RMS). However, tracking data from the on-board BlackJack GPS receiver are available with sufficiently short latency for use in the computation of NRT GPS-based orbit solutions. The orbit altitudes from these NRT orbit solutions have typical accuracies of < 3.0 cm (RMS) with a latency of 1–3 h, and < 2.5 cm (RMS) with a latency of 3–5 h. Meanwhile, forecast global pressure fields from the National Center for Environmental Prediction (NCEP) are available for the NRT computation of the dry troposphere correction. In combination, the Jason-1 OSDR, the NRT GPS-based orbit solutions, and the NCEP pressure fields can be used to compute sea surface height observations from the Jason-1 mission with typical latencies of 3–5 h, and have differences with those from the 2–3 day latency Interim Geophysical Data Records of < 5 cm (RMS). The NRT altimetric sea surface height observations are potentially of benefit to forecasting, tactical oceanography, and natural hazard monitoring.  相似文献   

Reproductive biology of horse mackerel Trachurus capensis and Trachurus trecae in Namibia and Angola     

《African Journal of Marine Science》2013,35(2):141-150

Harvest control measures for Namibia and Angola are defined using reference points for spawning biomass, which requires knowledge of spawning potential and dynamics of fishery stocks. The reproductive biology of two species of horse mackerel, Trachurus capensis and Trachurus trecae, in these waters was investigated for spawning distribution in time and space. Samples were collected during two scientific cruises conducted in February and July/August 2007 off the coast of Namibia and Angola. A total of 396 fish ovaries was examined to determine the spawning dynamics of the two species. The ovaries were histologically analysed and their oocyte distributions mapped. The length (TL)–weight relationships of the two species differed significantly. The observed development of oocyte recruitment and absence of a hiatus in the oocyte distribution indicated that these species are indeterminate spawners. Analyses of the data from the NatMIRC database (2001–2004) indicated annual changes in gonadosomatic index (GSI) for T. capensis at different latitudes, but these changes were small. GSI also fluctuated between years and areas, but there were no clear spatial or temporal trends, with averages ≤4.0% at all stations. The GSI of both species was not indicative of the histologically determined development of gonad maturity. Oocyte maturation for T. capensis indicated that smaller and younger fish spawn first. Batch fecundity (F) for T. trecae was best described by F = 4 986 TL (cm) – 99 645 (r ² = 0.83). This study provided the first analyses of oocyte development in time and space for the two species in the region.  相似文献   

Behaviour of hatchery‐reared and wild‐caught 4th and 5th stage American lobsters,Homarus americanus     

Kathleen M. Castro  J. Stanley Cobb 《新西兰海洋与淡水研究杂志》2013,47(4):963-972

Behavioural deficiencies in 4th and 5th stage hatchery‐reared lobsters were examined using time budget analysis and predator trials. Hatchery‐reared 4th stage lobsters were found to behave differently than wild‐caught lobsters and differences existed between hatchery‐reared lobsters from different sources. Local hatchery‐reared 4th stage lobsters spent less time on shelter and suffered higher predator rates in laboratory trials than both wild‐caught 4th stage and lobsters reared in a hatchery in Maine. Fifth stage hatchery‐reared lobsters spent significantly more time in shelter than their wild‐caught counterparts. These differences may be attributable to the lack of development of proper predator‐avoidance behaviour and need to be understood and corrected to maximise the effect of enhancement projects.  相似文献   

岩墙厚度对成矿作用的约束:以石湖金矿为例   总被引：8，自引：0，他引：8       下载免费PDF全文

李德东  罗照华  周久龙  杨宗锋  刘翠 《地学前缘》2011,18(1):166-178

根据透岩浆流体成矿理论,岩浆体是含矿流体的通道而不是来源,因而估算含矿流体注入岩浆体的能力是评价高位侵入体成矿潜力的有效方法。文中利用一维传热模型计算了石湖金矿区三类代表性岩墙(花岗斑岩、石英闪长玢岩和辉绿岩)不同厚度条件下的冷却时间尺度,同时估算了岩浆冷却过程中的粘度变化速率。假定岩浆侵位于约6 km,且完全固结时含矿流体才不能有效注入,石湖金矿区三类代表性岩墙的最小临界成矿厚度分别为3345 m(花岗斑岩)、822 m(石英闪长玢岩)和102 m(辉绿岩)。模拟结果与石湖金矿区矿体的产状一致,暗示模拟结果具有较强的实用价值。结合岩墙长度/宽度比值,进一步估算致矿侵入体的最小临界出露面积分别约为312～1 561 m2(玄武质岩体)、0014～0068 km2(石英闪长玢岩)和0011～0034 km2(花岗斑岩)。估算结果为野外地质找矿提供了一个定性的标准,对快速资源勘查具有参考价值。  相似文献   

NTSC的守时工作进展     

董绍武  屈俐俐  李焕信  刘春侠 《时间频率学报》2010,33(1):1-4

概括介绍了中国科学院国家授时中心（简称NTSC）时间基准系统的组成、功能和相关工作的最新进展情况。NTSC负责我国标准时间的产生、保持和发播。多年来,NTSC的守时系统以完美的表现满足了国家大科学装置—长、短波授时系统的发播控制任务的要求。2008年度,NTSC的守时工作取得突破性进展,实现的指标综合排名于全球实验室的2～3位,我国守时工作已经跻身世界前列,NTSC已成为国际原子时合作单位中最重要的守时实验室之一。  相似文献   

广西巴马县水晶宫洞穴沉积物特征及其沉积环境   总被引：4，自引：3，他引：1  

张美良  朱晓燕  吴夏  阳和平  潘谋成 《中国岩溶》2013,32(3):345-357

巴马县水晶宫洞内次生化学沉积物景观丰富,类型多样,有石钟乳、石幔、石瀑布、石笋、石柱、石盾等特色景观;尤其是近期仍在发育的洞顶鹅管、卷曲石、石花等是国内外较为罕见的洞穴奇景。据沉积物的沉积类型、物质成分、沉积序次及测年等资料研究表明,水晶宫洞穴沉积物形成于晚第三纪以来。晚第三纪和第四纪早更新世早期,洞内沉积主要为外源水携带的硅质岩、砂岩类砾石沉积形成的钙华砾石层。早更新世中期—中更新世气候温暖湿润,是水晶宫洞穴主要景观的形成期,沉积物景观宏大而壮观,230Th-U系测年得出其分别形成于100～35万年前。晚更新世早期12.5～9万年的末次间冰期主要为温暖气候环境,洞内仅有少量的石笋沉积,且极少保存;9万年后气候环境发生突变,更不利沉积物发育和保存;自4万年后气候环境开始表现为温暖湿润,化学沉积活跃,洞穴沉积物主要由高约50～150 cm的纯白色石笋群和钟乳石组成,为洞穴奇景的形成期,230Th-U系测年得出其分别形成于40 ka BP和7 500 a BP以及1 450 a BP。晚更新世晚期以来形成的洞穴沉积物景观,不仅为水晶宫提供了丰富的旅游资源和价值,同时也为广西重建古气候环境提供了重要的信息载体。   相似文献   

断层的大地震复发概率研究   总被引：1，自引：0，他引：1  

朱元清  解朝娣  宋秀青  秦浩文 《地震》2013,33(4):1-10

本文以布朗过程时间物理模型为基础, 以地震孕育过程为研究主线, 计算了中国大陆地区主要活动断层在不同预测时段内的强震复发概率, 进而对断层的地震危险性进行了研究。 结果表明: 鲜水河断裂带、 阿尔金断裂带、 东昆仑断裂带、 小江断裂带这4条断层的强震复发概率值显著高于其他断裂带, 反映了这些断层所处地区的应力积累水平高于其他地区, 应属于未来可能复发强震的危险地带。  相似文献