Magma sources and petrogenesis of the early–middle Paleozoic backarc granitoids from the central part of the Qilian block,NW China     

《Gondwana Research》2016

The petrology, geochemistry, geochronology, and Sr–Nd–Hf isotopes of the backarc granitoids from the central part of the Qilian block are studied in the present work. Both S- and I-type granitoids are present. In petrographic classification, they are granite, alkali feldspar granite, felsic granite, diorite, quartz diorite, granodiorite, and albite syenite. The SHRIMP ages are 402–447 Ma for the S-type and 419–451 Ma for the I-type granitoids. They are mostly high-K calc-alkaline granitoids. The S-type granitoids are weakly to strongly peraluminous and are characterized by negative Eu anomalies (Eu/Eu* = 0.18–0.79). The I-type granitoids are metaluminous to weakly peraluminous and are characterized mostly by small negative to small positive Eu anomalies (Eu/Eu* = 0.71–1.16). The initial (⁸⁷Sr/⁸⁶Sr) values are 0.708848–0.713651 for the S-type and 0.704230–0.718108 for the I-type granitoids. The ε_Nd(450 Ma) values are − 8.9–−4.1 and − 9.7–+ 1.9 for the S-type and I-type granitoids, respectively. The T_DM values are 1.5–2.4 Ga for the S-type and 1.0–2.3 Ga for the I-type granitoids. For the Qilian block, the backarc granitoid magmatism took place approximately 60 million years after the onset of the southward subduction of the north Qilian oceanic lithosphere and lasted approximately 50 million years. Partial melting of the source rocks consisting of the Neoproterozoic metasedimentary rocks of the Huangyuan Group and the intruding lower Paleozoic basaltic rocks could produce the S-type granitoid magmas. Partial melting of basaltic rocks mixed with lower continental crustal materials could produce the I-type granitoid magmas. Major crustal growth occurred in the late Archean and Meso-Paleoproterozoic time for the Qilian block. The magma generation was primarily remelting of the crustal rocks with only little addition of the mantle materials after 1.0 Ga for the Qilian block.  相似文献   

利用CFCs定年数据计算静升盆地含水层渗透系数   总被引：1，自引：0，他引：1  

乔小娟  李国敏  王宏义  黎明  樊荣  肖永吉  赵春虎  徐海珍 《水文地质工程地质》2009,36(3):21-24

文章利用CFCs(氟氯碳化合物)定年数据,计算山西静升盆地含水层渗透系数。结果表明:补给条件较好的区域与补给条件差的深层承压区相比,地下水年龄偏年轻;从冲洪积扇顶部到扇缘,地下水径流逐渐变缓,含水层渗透系数变小;盆地南部较北部,地下水流动缓慢,渗透系数整体偏小。该方法获得的渗透系数符合实际地质条件。  相似文献   

灰-水混合过程的水文地球化学模拟研究          下载免费PDF全文

孙亚乔  钱会  段磊  覃兰丽 《水文地质工程地质》2009,36(5):72-75

通过粉煤灰与水6种不同比例的混合实验,利用质量平衡模型模拟分析混合静置0,1,3,7,14,21d后的水化学组分,以揭示粉煤灰浸出液中水化学组分的形成机制。研究结果表明:灞桥电厂粉煤灰浸出液为高pH值溶液,浸出液pH值急剧上升是粉煤灰中碱性氧化物CaO水解的结果;粉煤灰-水反应系统中,矿物的溶解沉淀作用和阳离子交换作用是主要的水文地球化学作用。  相似文献   

Hydrogen isotopic ratios of plant wax n-alkanes in a peat bog deposited in northeast China during the last 16 kyr     

Osamu Seki  Philip A. Meyers  Kimitaka Kawamura  Yanhong Zheng  Weijian Zhou 《Organic Geochemistry》2009,40(6):671-677

Based on paleoclimatic reconstructions using various proxies, the Holocene Climate Optimum (10.5–6 ka) has been characterized as a warmer and wetter period in most of East Asia. The summer monsoons associated with the East Asian Monsoon evidently intensified and extended further inland from the Pacific Ocean, a source region of moisture. A notable exception to this general pattern exists in northeast China, where less wet conditions are recorded. We determined molecular compositions of individual plant wax hydrocarbons and their hydrogen isotope compositions (δD values) in a radiocarbon-dated peat core recovered from the Hani marsh in Jilin Province (China) and confirmed that the temperature-dependent effective precipitation in northeast China decreased during the Holocene Climate Optimum. A combination of P_aq, an indicator of the relative contribution of aquatic to terrestrial plants, and the difference in δD between low (C₂₃, C₂₅ and C₂₇) and high molecular weight (C₃₁) n-alkanes in the Hani peat bog indicates a dramatic change in vegetation from the deglaciation to the Holocene. No significant differences were observed between the δD values of low and high molecular weight n-alkanes with relatively high δD values and low P_aq during the early Holocene, indicating that all n-alkanes were produced by evapotranspiration-sensitive terrestrial plants during that time. However, lower δD values of mid-chain n-alkanes (C₂₃, C₂₅ and C₂₇) relative to the long chain n-alkane (C₃₁), together with higher P_aq values during the deglaciation (14–11 ka), suggest an increase in the contribution of aquatic plants and a higher water level during the period. The study demonstrates that northeast China was under a markedly wetter climate condition during the late deglaciation. For the 16 kyr record in the Hani peat sequence, we infer that moisture delivery by the East Asian Monsoon was relatively invariable in northeast China, but increased evaporation during the warmer Holocene Climate Optimum reduced the effective precipitation, defined by the balance between precipitation and evaporation.  相似文献   

一种自动搜索水准环及计算闭合差的方法研究     

蒋宏飞  刘伟东  王文胜 《测绘科学》2012,37(4):202-203,212

本文采用深度优先搜索算法(Depth-First-Search)实现自动搜索水准闭合环,并结合ArcGIS的图形拓扑关系技术来获得最小水准环的信息;将此项技术应用于水准测量闭合环的闭合差计算,最终实现了自动计算水准闭合环的闭合差及精度统计。  相似文献   

数字城市建模方法研究与应用     

张超  魏占营  王锐  陈学霞 《测绘科学》2012,37(5):190-193

建筑物模型是大规模数字城市建设的重要组成部分。本文主要讨论了大规模数字城市建设中建筑物的建模方法,包括批量建模方法和重点区域建筑物精细建模方法。文中介绍了建模的基本思想,使用AutoCAD二次开发的插件和OSG(Open Scene Graph)渲染引擎实现了基于DLG(Digital Line Graphic)的模型批量生成和精细模型生成。实验证明,该方法能够快速有效地进行大规模建筑物批量建模,并支持重点区域精细模型的编辑与生成,在最终的三维场景浏览中,模型美观,空间地理坐标精确,量测精度高,符合数字城市的建模要求。  相似文献   

基于移动窗口分析法的西安市热岛效应研究     

张瑜  韩玲  谢露蓉 《测绘科学》2012,37(5):148-150

本文利用西安市两期Landsat5 TM影像,提取了西安市土地利用变化信息、NDVI指数、MNDWI指数和地表亮温,并基于移动窗口分析法进行了热岛效应边界的定量研究,旨在为陕西省地理国(省)情监测中环境监测部分探索一些可行的研究方法。研究结果表明:11年间,西安市热岛效应的发展趋势与城市扩张情况基本一致;地表亮温与植被指数和水体指数存在负相关关系,因此增加植被和水体面积有助于调节城市热岛效应的强度。  相似文献   

输电线路状态监测的GIS平台设计与实现     

曹建成  余晓松  刘继生 《测绘科学》2012,37(5):170-172

本文分析了电力工业输电线路状态监测工作中对GIS的需求,结合输电线路状态监测的特点,提出了基于SOA架构的二三维一体化输电线路状态监测GIS平台建设思路,开发了原型系统,实现了输电线路及其状态在三维环境下的展示、分析、模拟和实时信息查询,对实现输电线路状态空间监测具有参考意义。  相似文献   

利用单基准站改正信息和电离层参数估计的单频PPP算法     

涂锐  黄观文  张勤  王利 《武汉大学学报(信息科学版)》2012,37(2):170-173,182

利用单个基准站提供的改正信息对流动站的单频观测值数据进行改正,同时引入电离层参数进行实时电离层延迟估计,进行单频精密单点定位（PPP）计算。相比传统的单频PPP方法,本文方法对单频PPP的收敛速度和定位精度都有很大的提高,定位精度优于2cm,且受基准站距离的影响较小。  相似文献   

利用GPS观测资料分析山西地堑系现今地壳构造活动特征     

瞿伟  张勤  王庆良  李振洪 《武汉大学学报(信息科学版)》2012,37(2):195-198,246,259

基于中国地壳运动观测网络1999～2007年的GPS复测资料,建立起整体无净旋转基准,分析了山西地堑系内部地壳运动的细节特征,并利用图形单元法分析了其应变场的分布特征,深入剖析了地壳变形的动力学机制,得出山西地堑系现今构造应变场以NW-SE向拉张应变为主,与区域现代震源机制解及长期构造变形背景相一致;临汾、大同盆地是地堑内剪切应变高值区,现今地壳活动强烈。解释了地堑系内形变异常区的成因,由此揭示出连接临汾与太原盆地的构造隆起带两端的现今地壳活动十分强烈,并同时兼有拉张破裂趋势这一重要的构造事件。  相似文献