Cenozoic basin development and its indication of plateau growth in the Xunhua-Guide district   总被引：1，自引：0，他引：1  

LIU ShaoFeng  ZHANG GuoWei  P.L.HELLER 《中国科学D辑(英文版)》2007,50(Z2):277-291

The Xunhua, Guide and Tongren Basins are linked with the Laji Mountain and the northern West Qinling thrust belts in the Xunhua-Guide district. Basin depositional stratigraphy consists of the Oligocene Xining Group, the uppermost Oligocene-Pliocene Guide Group and the Lower Pleistocene. They are divided into three basin phases by unconformities. Basin phase 1 is composed of the Xining Group, and Basin phase 2 of the Zharang, Xiadongshan, Herjia and Ganjia Conglomerate Formations in the Guide Group, and Basin phase 3 of the Gonghe Formation and the Lower Pleistocene. Three basin phases all develop lacustrine deposits at their lower parts, and alluvial-braided channel plain depositional systems at upper parts, which constitute a coarsening-upward and progradational sequence. Basin deposition, paleocurrent and provenance analyses represent that large lacustrine basin across the Laji Mountain was developed and sourced from the West Qinling thrust belt during the stage of the Xining Group (Basin phase 1), and point-dispersed alluvial fan-braided channel plain deposition systems were developed beside the thrust and uplifted Laji Mountain and sourced from it, as thrusting migrated northwards during the stage of the Guide Group (Basin phase 2). Evolution of basin-mountain system in the study area significantly indicates the growth process of the distal Tibetan Plateau. The result shows that the Tibetan Plateau expanded to the northern West-Qinling at Oligocene (29―21.4 Ma) by means of northward folded-and-thrust thickening and uplifting and frontal foreland basin filling, and across the study area to North Qilian and Liupan Mountain at the Miocene-Pliocene (20.8―2.6 Ma) by means of two-sided basement-involved-thrust thickening and uplifting and broken foreland basin filling, and the distant end of Tibetan Plateau behaved as regional erosion and intermontane basin aggradational filling during the Pliocene and early Pleistocene (2.6―1.7 Ma).  相似文献   

基于Geoda 095i区域经济增长率的空间统计分析研究   总被引：5，自引：0，他引：5  

胡青峰  张子平  何荣  牛遂旺 《测绘与空间地理信息》2007,30(2):53-55

空间统计分析的核心是认识与地理位置相关的数据间的空间依赖、空间关联或空间自相关,通过空间位置建立数据间的统计关系。本文利用空间分析的相关知识,通过对河南省各辖市2006年第一季度GDP增长速度及其相关因素的分析,发现该时期内河南省各辖市GDP增长率水平的空间分布并非表现出完全随机性,而是表现出空间相似值之间的空间聚集。基于对Moran散点图的分析和空间滞后回归模型的回归分析,得出空间统计分析对于分析区域经济发展的空间结构形态以及政策制定具有参考价值。  相似文献   

A simple approach for determining particle size enlargement mechanisms in nickel reduction     

V.C. Taty Costodes  C.F. MausseK. Molala  A.E. Lewis 《International Journal of Mineral Processing》2006

This paper examines the active mechanisms responsible for the size enlargement of nickel metal particles during reduction by hydrogen gas. The population balance, related to particle size distribution, is discretized and solved with the method of moments to model the experimental data. This data was generated in a solution of intermittently constant supersaturation during the batch reduction in an 11,000 l of autoclave. PSD and mass distributions were determined by periodically removing suspension samples. In the proposed model, only the growth mechanism is taken into account and aggregation is ignored. Comparison of simulated and experimental PSD and mass distributions show that growth was not the only active mechanisms. Results from the plant indicate that there is an increase in particle size as the cycle progresses. The model generally underpredicts the growth shift in the PSDs' for the early and the larger densifications although it correctly predicts the growth shift in the middle densifications. Constant growth is therefore not the exclusive controlling mechanism. The findings have been confirmed by the trend of the zeroth moment as a function of time.  相似文献   

Heterogeneous growth of cordierite in low P/T Tsukuba metamorphic rocks from central Japan     

K. Miyazaki 《Journal of Metamorphic Geology》2001,19(2):155-164

This paper examines the spatial statistics of matrix minerals and complex patterned cordierite porphyroblasts in the low‐pressure, high‐temperature (low P/T) Tsukuba metamorphic rocks from central Japan, using a density correlation function. The cordierite‐producing reaction is sillimanite + biotite + quartz = K‐feldspar + cordierite + water. The density correlation function shows that quartz is distributed randomly. However, the density correlation functions of biotite, plagioclase and K‐feldspar show that their spatial distributions are clearly affected by the formation of cordierite porphyroblasts. These observations suggest that cordierite growth occurred through a selective growth mechanism: quartz adjacent to cordierite has a tendency to prevent the growth of cordierite, whereas other matrix minerals adjacent to cordierite have a tendency to enhance the growth of cordierite. The density correlation functions of complex patterned cordierite porphyroblasts show power‐law behaviour. A selective growth mechanism alone cannot explain the origin of the power‐law behaviour. Comparison of the morphology and fractal dimension of cordierite with two‐dimensional sections from a three‐dimensional diffusion‐limited aggregation (DLA) suggests that the formation of cordierite porphyroblasts can be modelled as a DLA process. DLA is the simple statistical model for the universal fractal pattern developed in a macroscopic diffusion field. Diffusion‐controlled growth interacting with a random field is essential to the formation of a DLA‐like pattern. The selective growth mechanism will provide a random noise for the growth of cordierite due to random distribution of quartz. Therefore, a selective growth mechanism coupled with diffusion‐controlled growth is proposed to explain the power‐law behaviour of the density correlation function of complex patterned cordierite. The results in this paper suggest that not only the growth kinetics but also the spatial distribution of matrix minerals affect the progress of the metamorphic reaction and pattern formation of metamorphic rocks.  相似文献   

Bioenergetic responses in green lipped mussels (Perna viridis) as indicators of pollution stress in Xiamen coastal waters, China     

Wang S  Hong H  Wang X 《Marine pollution bulletin》2005,51(8-12):738-743

Samples of green lipped mussels (Perna viridis) were collected from three sites (Huoshao, I’Maluan and Tong’an) around Xiamen coastal waters, where levels of various trace organic pollutants have been studied. Samples were also collected at a “cleaner” reference site near Dongshan Island for comparison. Clearance rate, absorption efficiency and oxygen consumption of the mussels were measured under controlled laboratory condition; organic pollutants in their tissues were also analyzed. Scope for growth (SFG) was employed as a general biomarker to evaluate the stress of pollutants. Specimens from Tong’an site had the lowest SFG values (1.14 J/h/g); while specimens from the I’Maluan site and Huoshao site had SFG values of 5.01 and 6.72 J/h/g, respectively. Specimens from Dongshan (reference site) had a relatively high SFG value of 10.96 J/h/g. There was a significant negative correlation between the SFG of the different populations of green lipped mussels and the concentration of DDT in their tissues.  相似文献   

成矿动力系统在混沌边缘分形生长——一种新的成矿理论与方法论(上)   总被引：21，自引：3，他引：18  

於崇文 《地学前缘》2001,8(3):9-28

“成矿动力系统在混沌边缘分形生长”理论是笔者将复杂性理论及非线性科学与矿床地质学相结合 ,对中国扬子古陆周缘六个矿集区的基本范式进行长期系统研究所取得的总结性成果。研究指出 ,成矿系统总体上是开放、远离平衡、时空延展的动力学系统。它们具有复杂性和自组织临界性的内禀基本属性 ,并且在混沌边缘分形生长。该理论以“地质作用与时 空结构是一切地质现象的本质与核心”的自然哲学理念作为根本立足点 ,建立起一种具有普适性的理论框架。然后进一步将其具体化为三大组成部分 ,即 ( 1)矿床的动力学属性 ,( 2 )矿床地质学场 ,( 3 )成矿系统的演化。体现了成矿作用 (其核心为成矿作用动力学 )、空间结构 (矿床地质学场 )和时间结构 (成矿系统的演化 )三位一体的整体耦合与交织 ,从而又使该理论具有包容性。在此基础上进而归纳出“成矿动力系统在混沌边缘分形生长”的 5项判定准则以及表征这些准则的 10项相应的动力学行为特征。最后笔者提出“矿质局部活化导致成矿的发生”的命题 ,拟定了“成矿的发生”的重要科学问题 ,以“元胞非线性网络”(CNN)作为复杂性的范式 ,定量揭示成矿的发生 ,并对矿床在混沌边缘作精确定位 ,对“成矿动力系统在混沌边缘”理论作进一步的延伸、深化与发展。该理论在矿?  相似文献   

成矿动力系统在混沌边缘分形生长——一种新的成矿理论与方法论(下)   总被引：11，自引：2，他引：9  

於崇文 《地学前缘》2001,8(4):471-489

:“成矿动力系统在混沌边缘分形生长”理论是笔者将复杂性理论及非线性科学与矿床地质学相结合 ,对中国扬子古陆周缘六个矿集区的基本范式进行长期系统研究所取得的总结性成果。研究指出 ,成矿系统总体上是开放、远离平衡、时空延展的动力学系统。它们具有复杂性和自组织临界性的内禀基本属性 ,并且在混沌边缘分形生长。该理论以“地质作用与时 空结构是一切地质现象的本质与核心”的自然哲学理念作为根本立足点 ,建立起一种具有普适性的理论框架。然后进一步将其具体化为三大组成部分 ,即 ( 1)矿床的动力学属性 ,( 2 )矿床地质学场 ,( 3 )成矿系统的演化。体现了成矿作用 (其核心为成矿作用动力学 ) ,空间结构 (矿床地质学场 )和时间结构 (成矿系统的演化 )三位一体的整体耦合与交织 ,从而又使该理论具有包容性。在此基础上进而归纳出“成矿动力系统在混沌边缘分形生长”的 5项判定准则以及表征这些准则的 10项相应的动力学行为特征。最后笔者提出“矿质局部活化导致成矿的发生”的命题 ,拟定了“成矿的发生”的重要科学问题 ,以“元胞非线性网络”(CNN)作为复杂性的范式 ,定量揭示成矿的发生 ,并对矿床在混沌边缘作精确定位 ,对“成矿动力系统在混沌边缘”理论作进一步的延伸、深化与发展。该理论在?  相似文献   

Influence of Climate Change on Winter Wheat Growth in North China During 1950-2000          下载免费PDF全文

SONG Yanling  Elisabeth SIMELTON  CHEN Deliang  DONG Wenjie 《Acta Meteorologica Sinica》2005,19(4):501-510

1. IntroductionChinese agriculture has undergone tremendousstructural changes over the last decades. The averagestaple crop productivity has doubled in 25 yr while thepopulation increased by 25 % [China Statistical Year-book (CSY), 2003]. Winter wheat is one of China'smost important staple food crops, with a total farm-ing area of nearly 24 million hectares and a produc-tion exceeding 92 million ton in 2002 (CSY, 2003).Although China has been the world's largest wheatproducer since 1983 (…  相似文献   

全过程沉降量预测的Logistic生长模型及适用性研究   总被引：8，自引：0，他引：8  

徐洪钟施斌  李雪红 《岩土力学》2005,26(3):387-391

地基的全过程沉降量与时间的关系呈S形曲线，可用Logistic生长模型来描述。目前应用的Logistic生长模型，较少考虑模型的适用范围和预测精度等问题。结合工程实例，比较了模型参数估计的三种方法，研究结果表明，采用非线性回归法估计模型参数，可取得较好的预测效果；根据混沌理论，研究了模型的适用范围和预测性能。Logistic生长模型的动态行为由参数α(瞬时沉降速率)决定，当参数α的取值范围在[0，2]之内，该模型预测的最终沉降量是稳定的。  相似文献   

中国阿尔泰造山带后造山喇嘛昭花岗岩体锆石SHRIMP年龄、成因及陆壳垂向生长意义   总被引：41，自引：29，他引：41  

王涛  洪大卫童英韩宝福  石玉若 《岩石学报》2005,21(3):640-650

喇嘛昭岩体是阿尔泰造山带典型的后构造岩体,其时代问题一直没有解决。本次锆石SHRIMP定年给出 206Pb／238U年龄276±9Ma(MSWD=1．1),代表其形成年龄。这为阿尔泰后造山花岗岩和后造山作用提供了一个可靠的年代学证据。主量、微量元素地球化学特征显示该岩体具有I-A过渡的高钾钙碱性或高分异钙碱性花岗岩的特点。依据岩体构造特征、年代学、地球化学和地质背景综合分析,该岩体应为后造山岩体。该岩体Sr初始值变化于0．704-0．71659之间。εNd(T) 值为正值( 1．3- 2．8),模式年龄TDM-2为0．93-0．81Ga,与中亚造山带典型的高(正)εNd(T)值花岗岩相同。而且,其εNd (T)值略高于该地区同造山花岗岩。这说明,在具有陆壳基底的阿尔泰造山带后造山阶段,除了可能的俯冲下埋的年轻洋壳或岛弧物质外,可能有新的幔源物质参与了花岗岩的形成。这为中亚造山带后造山阶段陆壳垂向生长提供了一个证据。  相似文献