Common Pb of UHP metamorphic rocks from the CCSD project (100–5000 m) suggesting decoupling between the slices within subducting continental crust and multiple thin slab exhumation     

Shuguang Li  Chenxiang Wang  Feng Dong  Zhenhui Hou  Qiuli Li  Yican Liu  Fang Huang  Fukun Chen 《Tectonophysics》2009,475(2):308-317

In order to understand the vertical structure of the Dabie–Sulu ultrahigh-pressure metamorphic (UHPM) belt, common Pb isotopic compositions of omphacites in eclogites and feldspars in gneisses from the Chinese Continental Scientific Drilling (CCSD) project (100–5000 m) have been investigated in this study. Samples from 0 to 800 m (unit 1) in the drilling core have moderately high radiogenic Pb isotopes with small variations of ²⁰⁶Pb/²⁰⁴Pb (16.82–17.38), ²⁰⁷Pb/²⁰⁴Pb (15.37–15.49), and ²⁰⁸Pb/²⁰⁴Pb (37.21–37.72), indicating either high µ (²³⁸U/²⁰⁴Pb) or high initial Pb isotope ratios of their protoliths. In contrast, the samples from 1600 to 2040 m (unit 3) and most of samples from 3200 to 5000 m (unit 5) have moderately or very unradiogenic Pb (unit 3: ²⁰⁶Pb/²⁰⁴Pb from 16.05 to 16.46, ²⁰⁷Pb/²⁰⁴Pb from 15.22 to 15.29, and ²⁰⁸Pb/²⁰⁴Pb from 36.68 to 37.48; unit 5: ²⁰⁶Pb/²⁰⁴Pb from 15.52 to 15.69, ²⁰⁷Pb/²⁰⁴Pb from 15.15 to 15.27, and ²⁰⁸Pb/²⁰⁴Pb from 36.48 to 37.20), indicating either low µ or low initial Pb isotope ratios of their protoliths. Pb isotopes of samples from 800 to 1600 m (unit 2) and from 2040 to 3200 m (unit 4) in the drilling core with abundant ductile shear zones are intermediate between those of units 1 and 3 or 5 and display larger variations. Pb isotopes combined with the published oxygen isotope data of the CCSD samples reveal the original positions of the five units before the Triassic continental subduction. Units 1, 3, and 5 as three UHPM rock slabs could be derived from the subducted upper continental crust, upper–middle continental crust and lower–middle continental crust, respectively. The ductile shearing zones in units 2 and 4 could be the interfaces where the detachment and decoupling took place between the upper, upper–middle and lower–middle continental crusts. The detachment between the upper slab and subducting continental lithosphere probably occurred during continental subduction, and the upper slab (unit 1) was uplifted to a shallow depth along the detachment surface by thrusting. Units 3 and 5 may be detached later from the subducted middle and lower crust and uplifted to a shallow level underneath unit 1. The low δ¹⁸O values (? 4.0 to ? 7.4‰) [Xiao, Y.-L., Zhang, Z.-M., Hoefs, J., Kerkhof, A., 2006. Ultrahigh-pressure Metamorphic Rocks from the Chinese Continental Drilling Project-II Oxygen Isotope and Fluid Inclusion Distributions through Vertical Sections. Contribution Mineral Petrology 152, 443–458.; Zhang, Z.-M., Xiao, Y.-L., Zhao, X.-D., Shi, C., 2006. Fluid-rock interaction during the continental deep subduction: oxygen isotopic profile of the main hole of the CCSD project. Acta Petrologica Sinica 22 (7), 1941–1951.] in units 2 and 4 suggest that the detachment interfaces could be developed along an ancient fault zones which were the channels of meteoric water activity during the Neoproterozoic.  相似文献   

高效液相色谱-紫外光谱分析氢醌-双(β-羟乙基)醚     

盛东  王美飞  练鸿振 《岩矿测试》2009,28(5):407-410

建立了高效液相色谱-紫外光谱法测定聚氨酯扩链剂氢醌-双(β-羟乙基)醚(HQEE)工业品中HQEE主含量和对苯二酚残留的方法。在氰基柱上,以甲醇-水-1%乙酸溶液(体积比10∶50∶40)为流动相,流速1.0 mL/min时,HQEE、对苯二酚及其他相关杂质得到良好分离,紫外光谱285 nm检测。方法简便、快捷,结果准确可靠,在工业生产中可有效地指导HQEE合成过程的质量控制。  相似文献   

钛磁铁矿的制备及其异相Fenton反应催化性能   总被引：2，自引：0，他引：2  

杨士建  何宏平  吴大清  袁鹏  朱建喜  陈冬  梁晓亮  马月红 《地球化学》2009,38(2):159-164

在水相中合成了钛磁铁矿（Fe3-xTixO4）,并用XRD、MSssbauer、TG-DSC和SEM等手段对合成的Fe3-xTixO4进行了表征。结果表明,合成的Fe3-xTixO4为立方晶系尖晶石结构,样品中的钛离子都已经进入其晶格中;钛掺杂有抑制钛磁铁矿进一步向钛磁赤铁矿转化和稳定尖晶石结构的作用。此外,以亚甲基蓝降解为探针反应,考察了钛磁铁矿异相Fenton反应的催化性能。实验表明,钛含量较高的钛磁铁矿是一种性能优越的异相Fenton反应催化剂。  相似文献   

A Numerical Study on the Screening of Blast-Induced Waves for Reducing Ground Vibration   总被引：1，自引：1，他引：0  

Dohyun Park  Byungkyu Jeon  Seokwon Jeon 《Rock Mechanics and Rock Engineering》2009,42(3):449-473

Blasting is often a necessary part of mining and construction operations, and is the most cost-effective way to break rock, but blasting generates both noise and ground vibration. In urban areas, noise and vibration have an environmental impact, and cause structural damage to nearby structures. Various wave-screening methods have been used for many years to reduce blast-induced ground vibration. However, these methods have not been quantitatively studied for their reduction effect of ground vibration. The present study focused on the quantitative assessment of the effectiveness in vibration reduction of line-drilling as a screening method using a numerical method. Two numerical methods were used to analyze the reduction effect toward ground vibration, namely, the “distinct element method” and the “non-linear hydrocode.” The distinct element method, by particle flow code in two dimensions (PFC 2D), was used for two-dimensional parametric analyses, and some cases of two-dimensional analyses were analyzed three-dimensionally using AUTODYN 3D, the program of the non-linear hydrocode. To analyze the screening effectiveness of line-drilling, parametric analyses were carried out under various conditions, with the spacing, diameter of drill holes, distance between the blasthole and line-drilling, and the number of rows of drill holes, including their arrangement, used as parameters. The screening effectiveness was assessed via a comparison of the vibration amplitude between cases both with and without screening. Also, the frequency distribution of ground motion of the two cases was investigated through fast Fourier transform (FFT), with the differences also examined. From our study, it was concluded that line-drilling as a screening method of blast-induced waves was considerably effective under certain design conditions. The design details for field application have also been proposed.  相似文献   

Investigation of geothermal structure of the Sulawesi,using gravity and magnetic method     

Jian ZHANG  Tianyao HAO  Miao DONG  Ya XU  Beiyu WANG  Yifei AI  Gui FANG 《中国科学:地球科学(英文版)》2021,64(2):278-293

The Sulawesi Sea and Sulawesi Island are located in the western Pacific area where volcanic activity,plate subduction,and seismic activity are very active.The Sulawesi basin formed during the Middle Eocene-Late Eocene and nearly half of the Eocene oceanic crust has subducted below the North Sulawesi Trench.The Sulawesi Island was spliced and finalized in the Early Pliocene-Pleistocene during volcanic activity and is recently very active.This area is an optimal location to study volcanic geothermal conditions and subduction initiation mechanisms in the southern part of the western Pacific plate margin,which are important in geothermal and geodynamic research.In this study,we combined 133 heat flow data with gravity and magnetic data to calculate the Moho structure and Curie point depth of the Sulawesi Sea and periphery of the Sulawesi Island,and analyze the distribution characteristics of the geothermal gradient and thermal conductivity.The results show that the average depths of the Moho and Curie surfaces in this area are 18.4 and 14.3 km,respectively,which is consistent with the crustal velocity layer structure in the Sulawesi Basin previously determined by seismic refraction.The average geothermal gradient is 4.96°C(100 m)-1.The oceanic area shows a high geothermal gradient and low thermal conductivity,whereas the land area shows a low geothermal gradient and high thermal conductivity,both of which are consistent with statistical results of the geothermal gradient at the measured heat flow points.The highest geothermal gradient zone occurs in the transition zone from the Sulawesi Sea to Sulawesi Island,corresponding to the spreading ridge of the southward-moving Sulawesi Basin.Comprehensive gravity,magnetic,and geothermal studies have shown a high crustal geothermal gradient in the study area,which is conducive to the subduction initiation.The northern part of the Palu-koro fault on the western side of Sulawesi is likely the location where subduction initiation is occurring.During the process of moving northwest,the northern and eastern branches of Sulawesi Island have different speeds;the former is slow and the latter is fast.These branches also show different deep tectonic dynamic directions;the northern branch tilts north-up and the eastern branch tilts north-down.  相似文献   

遥感数据空间尺度分级模型与基本比例尺关系     

黄祥志  王栋  赵亚萌  臧文乾 《遥感学报》2018,22(4):591-598

多源遥感数据综合应用是遥感发展的必然趋势,统一的遥感数据空间尺度分级模型是多源数据集成与综合应用的基础。虽然已有多种空间尺度分级模型,但很多主流模型并非出于分尺度综合应用目的,缺乏客观的比较和评价。国家基本比例尺系统作为经过论证、中国应用面最广泛、接受度最高的一种尺度分级系统,是以应用为导向的遥感数据空间尺度分级模型的最优参照系。从不同视觉精度下国家基本比例尺对图像空间分辨率的需求出发,比较各空间尺度分级模型的层级分辨率与需求分辨率的匹配情况,包括OGC Well Known Scale Set的Global CRS84Pixel和Google Maps Compatible,以及NASA World Wind、Google Map、百度地图、天地图等软件平台采用的层级格网系统,以及"五层十五级"遥感数据组织模型,通过对数据信息冗余度的分析,对各个模型进行了评价。结果表明,在高视觉精度应用需求下,"五层十五级"模型与基本比例尺精度要求具有较明显的匹配优势,其次为OGC Google Maps Compatible模型和天地图模型,其余模型平均数据冗余倍数在2倍左右;在低视觉精度应用需求下,"五层十五级"模型平均数据冗余度仍为最低,其次为Google Map模型,其余模型平均数据冗余倍数都在2倍以上。  相似文献   

独立坐标系模型对长度变形影响的研究     

李东  毛之琳  廖文兵  陈敏 《测绘与空间地理信息》2014,(9):79-81

针对海拔较高的城市建立或改造独立坐标系,存在着如何选择模型及各模型对长度变形的影响等问题,通过算例对常见椭球变换和比例缩放模型进行较为全面系统的分析,归纳出常见模型在不同投影带区域、不同投影面高度对长度变形的影响差异,并得出有益的结论。  相似文献   

基于Jurkevich法Cyg X-1光变周期特性研究     

董爱军 《天文研究与技术》2012,(3):277-282

针对天文观测数据不等间隔的特点,利用Jurkevich方法对黑洞候选体X射线双星Cyg X-1近16年的Rossi X-ray Timing Explorer(RXTE)All-Sky Monitor(ASM)数据进行了频谱分析,并结合Kidger周期存在可信度的判据,发现Cyg X-1存在363±11.5 d的光变周期,但没有发现420 d的光变周期,而且150 d的光变周期可能仅仅是51±1.4 d光变周期的观测表象。  相似文献   

UV1600 bright points and magnetic bipoles in solar quiet regions     

Dong Li  ZongJun Ning 《Astrophysics and Space Science》2012,341(2):215-224

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Role of reservoir regulation and groundwater feedback in a simulated ground-soil-vegetation continuum: A long-term regional scale analysis     

Jianhui Wei  Ningpeng Dong  Benjamin Fersch  Joël Arnault  Sven Wagner  Patrick Laux  Zhenyu Zhang  Qianya Yang  Chuanguo Yang  Shasha Shang  Lu Gao  Zhongbo Yu  Harald Kunstmann 《水文研究》2021,35(8):e14341

The regional terrestrial water cycle is strongly altered by human activities. Among them, reservoir regulation is a way to spatially and temporally allocate water resources in a basin for multi-purposes. However, it is still not sufficiently understood how reservoir regulation modifies the regional terrestrial- and subsequently, the atmospheric water cycle. To address this question, the representation of reservoir regulation into the terrestrial component of fully coupled regional Earth system models is required. In this study, an existing process-based reservoir network module is implemented into NOAH-HMS, that is, the terrestrial component of an atmospheric–hydrologic modelling system, namely, the WRF-HMS. It allows to quantitatively differentiate role of reservoir regulation and of groundwater feedback in a simulated ground-soil-vegetation continuum. Our study focuses on the Poyang Lake basin, where the largest freshwater lake of China and reservoirs of different sizes are located. As compared to streamflow observations, the newly extended NOAH-HMS slightly improves the streamflow and streamflow duration curves simulation for the Poyang Lake basin for the period 1979–1986. The inclusion of reservoir regulation leads to major changes in the simulated groundwater recharges and evaporation from reservoirs at local scale, but has minor effects on the simulated soil moisture and surface runoff at basin scale. The performed groundwater feedback sensitivity analysis shows that the strength of the groundwater feedback is not altered by the consideration of reservoir regulation. Furthermore, both reservoir regulation and groundwater feedback modify the partitioning of the simulated evapotranspiration, thus affecting the atmospheric water cycle in the Poyang Lake region. This finding motivates future research with our extended fully coupled atmospheric–hydrologic modelling system by the community.  相似文献