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971.
新疆、青海、西藏数字地震台网和新疆和田台阵都十分清晰、完整地记录到2014年2月12日新疆于田MS7.3地震的波形,故采用区域地震台网和地震台阵联合定位的方法来精确测定该地震的震源位置。具体定位时采用了以下技术:①根据MS7.3地震震中的位置,360o等方位均匀选取台站,平均每隔约15o取1个台站参与初始定位;②将于田台的记录波形旋转至径向和切向上精确测定S波的到时,并以此控制震中距;③测定震中位置时采用的速度模型,是以震源为中心、半径约为1.0o范围内发生的历史地震资料为基础,重新拟合后获得的速度模型;④利用和田地震台阵记录的主震波形资料,经波形聚束方法处理后进行方位角测定,并以此方位角修正震中位置;⑤采用确定性方法测定震源深度。最终得到新疆于田MS7.3地震主震的震中位置为36.197oN、82.467oE,震源深度为12km,发震时刻为2014年2月12日17:19:48.2。  相似文献   
972.
多龙矿集区位于班公湖-怒江成矿带西段北侧、羌塘地块南缘,是我国近年来发现的最大斑岩-浅成低温热液型Cu(Au)矿集区。地堡是多龙矿集区最西南边缘的矿床,资源潜力巨大,有望达到超大型规模,但研究程度薄弱。本次工作对地堡Cu(Au)矿开展了锆石U-Pb测年、流体包裹体、地球化学等方面的研究,为推动资源勘查和矿集区成矿规律的总结提供理论依据。含矿斑岩锆石206 Pb/238 U平均加权年龄为111.2±0.4Ma(MSWD=0.67),与矿集区成矿岩浆活动时限一致,是矿集区重要组成部分。石英脉流体包裹体显示矿床主成矿期成矿流体温度集中于140~382℃,主要集中在240~280℃。成岩阶段石英斑晶中Ⅰ型包裹体盐度范围为0.2%~20.7%NaCleqv.,含盐子晶包裹体盐度为33.6%NaCleqv.和43.9%NaCleqv.;成矿阶段不含石膏石英脉Ⅰ型包裹体盐度范围为0.2%~20.8%NaCleqv.,黄铁矿石英脉Ⅰ型包裹体盐度范围为1.1%~11.1%NaCleqv.,石膏中Ⅰ型包裹体盐度范围为0.5%~9.3%NaCleqv.。对钻孔DNZK6428样品进行主微量元素测试并进行因子分析计算,结果表明F1、F2、F3代表成岩阶段,因子主成分为Y-Ho-Er-Tm-Yb-Dy-Lu-Tb-Eu-Gd-Sm-La-Ce-Pr-Nd-SiO_2-Al_2O_3-CaO等,F4和F5代表铜金矿化阶段,因子主成分为Sn-Sb-Ba-Fe_2O_3-Sr-|SiO_2|-Ni-Cu-U-In-Cd-Au-Zn。黄铁矿δ34SV-CDT值总体较为集中,呈"双峰塔式"分布,变化范围为-7.8‰~4.1‰,均值为-4.23‰,为深源岩浆硫,硫的来源接近地幔硫。矿床粒状黄铁矿Co/Ni比值为0.207~10.775,平均值4.39,脉状黄铁矿Co/Ni比值为0.353~23.155,平均值3.802,均为热液成因。矿相学与岩相学研究结果显示矿床具明矾石和硫砷铜矿典型高硫化浅成低温热液矿床的矿物组合,地堡Cu(Au)矿为高硫型浅成低温热液矿床。  相似文献   
973.
Yunjie Song  Xun Shi 《GeoJournal》2017,82(3):597-608
The exploration of the spatial association between Medicare physician spending and population densities and sizes could possibly facilitate the investigation of the causal mechanisms beneath the variation in medical care. We acquired the U.S. Medicare physician expenditures and regional demographic and geographic data in 2006 from the Dartmouth Atlas of Health Care. Six geographic units—states, counties, Hospital Referral Regions, Hospital Service Areas, Metropolitan Statistical Areas, and state non-Metropolitan Statistical Areas—were used as units of study. Pearson correlation analysis, multivariable regression, and partial correlation analysis were employed. Among six geographic units, Pearson correlation coefficients between Medicare physician expenditures and logarithmic population densities ranged from 0.42 to 0.63 (p < 0.05 for all), and between the expenditures and logarithmic population sizes from 0.31 to 0.65 (p < 0.05 for all). When population health, differential demand, market structure, and data reporting bias were controlled, population densities and sizes were positively associated with Medicare physician expenditures in most models. Population densities and sizes could explain considerable amounts of regional variation in Medicare physician spending. We concluded that Medicare physician spending was contingent on population densities and sizes. Because population densities and sizes are produced by more fundamental qualities such as natural environments and resources and thus are not easily manipulated, they are suggestive in health policy studies. Further research might investigate population distribution associated properties such as geographic distribution of health care resources, spatial dynamics of medical technology distribution, and cultural and psychological factors.  相似文献   
974.
Bifurcation of unsaturated soils into a localized shear band is a ubiquitous failure mode of partially saturated soils. The density and degree of saturation have major impacts on the inception of localized deformations in unsaturated soils. Unsaturated fluid flow may dramatically change the density and degree of fluid saturation of unsaturated soils. Therefore, the unsaturated fluid flow is a potential trigger for shear banding in such materials. In this paper, we derive a simplified bifurcation condition of localized deformation in unsaturated soils under the local transient condition at finite strain. This transient bifurcation condition is implemented into a nonlinear finite element code to study the inception of localized deformation in unsaturated soil specimens. Numerical simulations are conducted to study the impact of soil fabrics of density, a ‘bonding’ variable, and intrinsic permeability on the inception of localized failures via the transient bifurcation criterion. Mesh sensitivity analysis is performed to demonstrate the viscosity effect of unsaturated fluid flow on the localized deformation. Numerical simulations demonstrate that the transient bifurcation condition can detect the localized deformation triggered by the internal unsaturated fluid flow process in unsaturated soils. Copyright © 2016 John Wiley & Sons, Ltd.  相似文献   
975.
976.
Deng  Yujun  Young  Caitlin  Fu  Xinyu  Song  Jie  Peng  Zhong-Ren 《Natural Hazards》2017,85(2):1063-1088
Natural Hazards - Saltwater intrusion is a major hazard to coastal communities as it causes degradation of fresh water resources. The impact of rising sea level on the saltwater intrusion into...  相似文献   
977.
Peng  Yu  Song  Jingyi  Cui  Tiantian  Cheng  Xiang 《Natural Hazards》2017,89(1):441-456
Natural Hazards - Inner Mongolia, located in the northern China, is a natural disaster-prone region. This study is dedicated to making a comprehensive and quantitative analysis of the...  相似文献   
978.
Rivers link terrestrial ecosystems and marine ecosystems, and they transport large amounts of substances into oceans each year, including several forms of silicon (Si), carbon (C), and other nutrients. However, river damming affects the water flow and biogeochemical cycles of Si, C, and other nutrients through biogeochemical interacting processes. In this review, we first summarize the current understanding of the effects of river damming on the processes of biogeochemical Si cycle, especially the source, composition, and recycling process of biogenic silica (BSi). Then, we introduce dam impacts on the cycles of C and some other nutrients. Dissolved silicon in rivers is mainly released from phytolith dissolution and silicate weathering. BSi in suspended matter or sediments in most rivers mainly consists of phytoliths and mainly originates from soil erosion. However, diatom growth and deposition in many reservoirs formed by river interception may significantly increase the contribution of diatom Si to total BSi, and thus significantly influence the biogeochemical Si, C, and nutrient cycles. Yet the turnover of phytoliths and diatoms in different rivers formed by river damming is still poorly quantified. Thus, they should be further investigated to enhance our understanding about the effects of river damming on global biogeochemical Si, C and nutrient cycles.  相似文献   
979.
南海中西部地貌单元划分及其特征和成因分析   总被引:1,自引:0,他引:1  
南海中西部处于南海北部和南部的过渡带,夹持于印支地块和南海海底扩张中心之间,其特殊的地貌对于研究整个南海地质地貌有重要意义。本文基于广州海洋地质调查局在南海中西部海洋地质调查项目获取的水深、底质调查及地震剖面数据,结合该海域以往研究成果,提取了有关地貌的信息,编制了南海中西部地貌图。把研究区划分出陆架、陆坡和深海盆地三个二级地貌单元,以及水下岸坡、水下浅滩、海岭、峡谷、麻坑、阶地、盆地、海台、海山、深海扇、深海平原等众多次级地貌单元。文章详细描述了该海域各地貌单元的特征,提出了断层、火山、构造隆起和浊流等地质作用是本区地貌形成的主要因素。  相似文献   
980.
在前期详细地质调查的基础上,对郧西盆地进行针对性的浅层地震反射勘探,并利用地震发射结果来确定断层位置及构造特征。该研究对南水北调中线核心水源区地震安全系统的建设有一定意义。  相似文献   
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