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991.
992.
Traditional magneto-electric vibration sensors and servo accelerometers have severe shortcomings when used to measure vibration where low frequency components predominate. A low frequency characteristic extension for velocity vibration sensors is presented in this paper. The passive circuit technology, active compensation technology and the closedcycle pole compensation technology are used to extend the measurable range and to improve low frequency characteristics of sensors. Thses three types of low frequency velocity vibration sensors have been developed and widely adopted in China. 相似文献
993.
This study reports new zircon U–Pb ages, Lu–Hf isotope data, and oxygen isotope data for Mesozoic Mo-bearing granitoids in the eastern Xing–Meng Orogenic Belt (XMOB) of Northeast China, within the eastern Central Asian Orogenic Belt. Combining these new laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) zircon U–Pb ages with the results of previous research indicates that two stages of Mo-bearing granitoid magmatism occurred in the eastern XMOB, during the Early–Middle Jurassic (200–165 Ma) and the Early Cretaceous (ca. 111 Ma). The eastern XMOB also contains Mo-bearing granitoids with variable δ18O compositions that record variations in source oxygen isotopic compositions. Combining δ18O data with zircon U–Pb and Hf isotopic data provides evidence of the origin of these granitoids. Three types of zircon have been identified within these granitoids. Type 1 zircons formed during the Mesozoic and having high δ18O values (5.71–7.05‰) that are consistent with the compositions of magmatic zircons from the Luming, Jiapigou, and Kanchuangou areas. These zircons suggest that the Mo-bearing granitoids were derived from a source containing supracrustal materials. The type 2 zircons have extremely low and heterogeneous δ18O values (4.64–4.89‰) that are consistent with the compositions of magmatic zircons from the Jidetun and Fuanpu areas. These magmas were generated by the remelting of juvenile crustal material that was previously significantly modified by interaction with fluids. Type 3 zircons generally have mantle-like δ18O values (5.42–5.57‰), with several zircons yielding higher δ18O values, suggesting that these intrusions formed from mantle-derived magmas that assimilated and were metasomatized by crustal material. Combining these geochemical data with the geology of this region indicates that the Mo-bearing granitoids were generated as a result of subduction of the Palaeo-Pacific Plate beneath the Eurasian continent. 相似文献
994.
Taking the Taizihe River Basin located in Liaoning Province as a study area, we applied HBV hydrological model to simulate the hydrological process of this river basin with the support of observed daily precipitation, mean temperature, hydrological data in Xiaolinzi hydrologic station, and global digital elevation model data from SRTM3, land utilization types, etc. According to the simulation results of daily runoff, the possible impact of future climate change on runoff was analyzed through forcing HBV model by RegCM4.4 dynamic downscaled climatic data. The results show that HBV model performed generally well for daily simulation of the Taizihe River Basin with Nash Sutcliffe coefficient and deterministic coefficient being all over 0.60 in the calibration period and validation period, and the response of flooding to precipitation were simulated better. This indicates the HBV model can be successfully applied to the Taizihe River Basin. Mean temperature will increase obviously with persistent rising trend by RegCM4.4 model in 2021-2070 under RCP4.5 scenario. Annual precipitation and runoff depth are expected to reduce a bit. Compared with the baseline period (1986-2005), annual runoff depth will increase by 9.79%. At the same time, the runoff depth will increase significantly in summer and autumn. The variation of runoff quantile indicates that both peak extreme runoff and dry extreme runoff will increase to different degrees than that in the baseline period. In the future, the Taizihe River Basin will be likely to experience extreme flooding. 相似文献
995.
Huichao Zhang Peng Chai Hongrui Zhang Zengqian Hou Shouming Chen Yanbin Sun Qing Peng 《Resource Geology》2019,69(3):270-286
The Laowangzhai gold deposit, located in the Ailaoshan gold belt (SW China), is hosted in various types of rocks, including in quartz porphyry, carbonaceous slate, meta‐sandstone, lamprophyre, and altered ultramafic rocks. In contrast to other wall rocks, the orebodies in altered ultramafic rocks are characterized by the occurrence of a large amount of Ni‐bearing minerals. The ore‐forming process of the orebodies hosted by altered ultramafic rocks can be divided into two stages: pyrite‐vaesite‐native gold and gersdorffite‐violarite stages. The contents of As and Sb increased during the evolution of ore‐forming fluid based on the mineral assemblages. Thermodynamic modeling of the Ni‐Cu‐As‐Fe‐S system using the SUPCRT92 software package with the updated database of slop16.dat indicates the fS2 in ore‐forming fluid decreases significantly from stage I to stage II. The decreases of fS2 due to crystallization of sulfides and fO2 due to fluid–rock reaction were responsible for ore formation in altered ultramafic rocks of the Laowangzhai gold deposit. Geological evidence, the in situ sulfur isotope values of pyrite, and the other published isotopic data suggest that the ore‐forming fluid for ultramafic rock ores was dominantly composed of evolved magmatic fluid with the important input of sediments. 相似文献
996.
Assimilation systems absorb both satellite measurements and Argo observations. This assimilation is essential to diagnose and evaluate the contribution from each type of data to the reconstructed analysis, allowing for better configuration of assimilation parameters. To achieve this, two comparative reconstruction schemes were designed under the optimal interpolation framework. Using a static scheme, an in situ-only field of ocean temperature was derived by correcting climatology with only Argo ... 相似文献
997.
在建立了小行星区星云凝聚模型的基础上,对类地行星区中上物质(硅酸盐、氧化物、金属、硫化物等)的凝聚作用,以及凝聚物的水化作用进行了讨论,进而建立了包括小行星区在内的整个类地行星区的星云凝聚模式。根据地球核慢质量比和关于地球初期演化的研究结果;使用顽火辉石球粒陨石和C1陨石的化学成分分别做为地球形成区中类顽火辉石球粒陨石质星子和类C1陨石质星子的成分数据;假定类顽火辉石无球粒陨石质星子的成分与类顽火辉石球粒陨石质星子的硅酸盐部分成分相同,计算出原始地球可能由1.58%的类铁陨石质星子、13.9%的类顽火辉石无球粒陨石质星子、82.52%类顽火辉石球粒陨石质星子、2%的类C1陨石质星子组成。 相似文献
998.
以内蒙古自治区乌达矿区为例,介绍了地理信息系统在煤岩煤质资料分析中应用的可能性、基本原理、方法、优势及其展望。在分析中使用了该系统的软件和dBASEⅣ,以科学的、系统的方式连接各类地质资料,从而提供了一种利用这些信息的简单方便的方法。 相似文献
999.
四川北川埃洛石矿物学特征及工业利用前景 总被引:6,自引:0,他引:6
本文对四川北川埃洛石的矿物学特征进行研究表明,埃洛石呈管状,其TFe2O3,TiO2,MnO等杂质含量低,其化学成分接近理论值,XRD,IR,DTA等分析均表明其为埃洛石矿物。对埃洛石的主要工艺性能测试研究表明,北川埃洛石型粘土具有优良的工艺性能,应用前景广阔。 相似文献
1000.