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121.
Dajing is a large-scale tin–polymetallic deposit that hosts the largest tin mine in North China. It is a hydrothermal vein-type deposit containing Sn, Cu, Pb, Zn, Ag, and minor components Co and In. The deposit consists of more than 690 veins hosted within Upper Permian sedimentary rocks.Three mineralization stages and six ore types are recognized with cassiterite constituting the dominant tin mineral. The SnO2 content of cassiterite increases in the sequence of mineralization stages shear-deformation→cassiterite–quartz→cassiterite–sulfide (or chalcopyrite–pyrite) stage, while the content of FeO, TiO2, Nb2O5, Ta2O5, and In2O5 tends to decrease with increases in NiO and Ga2O5. It is considered that the negative correlation between SnO2 and FeO, Nb2O5, Ta2O5, and In2O5 results from elemental substitutions. The early stage cassiterite is much richer in Ta and the later stage cassiterite is much poorer in Ti and Fe than is usual in hydrothermal vein type tin deposits. This is interpreted to indicate that the component of early stage cassiterite reflects a granitic magma source while the composition of later stage cassiterite has a more obvious strata source. The compositional variation of cassiterite corresponds to decreasing crystallization temperatures within each stage and between sequential stages with time. The characteristics of REE in cassiterite from two stages are in accord with that of subvolcanic rocks and the Linxi formation. It suggests that tin transported during the cassiterite–quartz stage may have originated from subvolcanic dikes (e.g., dacite porphyry), while in the cassiterite–sulfide stage, tin may have been derived from wallrock (e.g. siltstone) of the Upper Permian-age Linxi Formation.  相似文献   
122.
This paper presents a statistical analysis of the algebraic strain estimation algorithm of Shimamoto and Ikeda [Shimamoto, T., Ikeda, Y., 1976. A simple algebraic method for strain estimation from deformed eillipsoidal objects: 1. Basic theory. Tectonophysics 36, 315–337]. It is argued that the error in their strain estimation procedure can be quantified using an expected discrepancy measure. An analysis of this measure demonstrates that the error is inversely proportional to the number of clasts used. The paper also examines the role of measurement error, in particular that incurred under (i) a moment based and (ii) manual data acquisition methods. Detailed analysis of these two acquisition methods shows that in both cases, the effect of measurement error on the expected discrepancy is small relative to the effect of the sample size (number of objects). Given their relative speed advantage, this result favours the use of automated measurement methods even if they incur more measurement error on individual objects. Validation of these results is carried out by means of a simulation study, as well as by reference to studies appearing in previous literature. The results are also applied to obtain an upper bound on the error of strain estimation for various studies published in the literature on strain analysis.  相似文献   
123.
塔里木河源区冰川系统变化趋势预测   总被引:1,自引:0,他引:1  
塔里木河源区是我国冰川分布最集中的地区之一,总面积达17 745.51 km2,占全国冰川总面积的30%;同时本区又属于我国升温幅度最大的地区之一。应用冰川系统变化的功能模型,对塔里木河源区冰川系统在本世纪对气候变化的趋势进行预测。结果表明:到2050年,如气温比1961~1990年高出1.9~2.3℃,本区冰川面积将减少4%~6%,冰川径流将增加22%~34%,零平衡线将上升62~94 m;如此升温率持续到本世纪末,则本区冰川面积将减少10%~16%,冰川径流将会回落,但仍比本世纪初多11%~13%,零平衡线将上升156~233 m。  相似文献   
124.
As the diversion dike of the Middle Route of the South to North Water Transfer Project (MRSNWTP), the water quality and water quantity of Danjiangkou Reservoir is critical to the project. At present, the rates of industrial wastewater treatment and sewage discharge, which belongs to Chinese State Standard in the districts near the reservoir except Shiyan city, are less than 60% and 40% respectively. The point source pollutants will be controlled because of the project after some time, but the non-point source pollutants caused by vegetation degradation and water-soil erosion will not be controlled effectively in a long time. Water samples were collected from the Danjiangkou Reservoir during 2004 and 2005 and analyzed for trace metals, i.e., silver (Ag), aluminum (Al), arsenic (As), barium (Ba), bismuth (Bi), calcium (Ca), cadmium (Cd), cobalt (Co), chromium (Cr), copper (Cu), iron (Fe), mercury (Hg), potassium (K), lithium (Li), magnesium (Mg), manganese (Mn), molybdenum (Mo), sodium (Na), nickel (Ni), lead (Pb), antimony (Sb), selenium (Se), silicon (Si), strontium (Sr), vanadium (V), zinc (Zn), chemicophysical parameters and nutrients, i.e., temperature (T), pH, dissolved oxygen (DO), turbidity, total suspended solid (TSS), nitrate/ammonia/ammonium-nitrogen (NO3^-/NH3/NH4^+-N), total nitrogen (TN), dissolved inorganic nitrogen (DIN), total phosphorus (TP), potassium permanganate index (IMn), biochemical oxygen demand (BOD), dissolved inorganic carbon (HCO3^-). Our results are water quality belongs to Chinese standard level II, trace metals are low, but they are accumulating, and many of which, i.e., As, Pb, will endanger reservoir water security.  相似文献   
125.
A time-varying spherical harmonic model of the palaeomagnetic field for 0–7 ka is used to investigate large-scale global geomagnetic secular variation on centennial to millennial scales. We study dipole moment evolution over the past 7 kyr, and estimate its rate of change using the Gauss coefficients of degree 1 (dipole coefficients) from the CALS7K.2 field model and by two alternative methods that confirm the robustness of the predicted variations. All methods show substantial dipole moment variation on timescales ranging from centennial to millennial. The dipole moment from CALS7K.2 has the best resolution and is able to resolve the general decrease in dipole moment seen in historical observations since about 1830. The currently observed rate of dipole decay is underestimated by CALS7K.2, but is still not extraordinarily strong in comparison to the rates of change shown by the model over the whole 7 kyr interval. Truly continuous phases of dipole decrease or increase are decadal to centennial in length rather than longer-term features. The general large-scale secular variation shows substantial changes in power in higher spherical harmonic degrees on similar timescales to the dipole. Comparisons are made between statistical variations calculated directly from CALS7K.2 and longer-term palaeosecular variation models: CALS7K.2 has lower overall variance in the dipole and quadrupole terms, but exhibits an imbalance between dispersion in   g 12  and   h 12  , suggestive of long-term non-zonal structure in the secular variations.  相似文献   
126.
韧性剪切变形对岩石地球化学行为的制约一直是地质学家们探讨的课题。本文以构成北阿尔金红柳沟——拉配泉俯冲碰撞杂岩带与北阿尔金地块边界的巴什考供斜向逆冲型韧性剪切带为例,通过对韧性剪切带内花岗岩变形前后不同变形强度构造岩的地球化学组成进行对比,确定等比线斜率,探讨韧性变形对岩石体积和成分变异的影响。计算结果表明,在糜棱岩化过程中,糜棱岩化花岗岩体积亏损21%,花岗质糜棱岩体积亏损31%。质量平衡计算结果和等比线图表明,韧;陛剪切作用导致SiO2,流失量最大,A12O3、K2O及Ba、Rb、Sr等都有不同程度的丢失,显示出较强的活动性,MnO、P2O5、Sc位于等比线上或附近,表现出相对的稳定性。岩石中活动组分的变异是流体渗滤作用引起的,不活动组分的变异是体.积亏损造成的。  相似文献   
127.
东北夏季(6-8月)气温异常的时空特征分析   总被引:5,自引:0,他引:5  
利用夏季(6—8月)中国东北地区91站44a气温资料,采用谐波分析方法将该区夏季气温异常变化的年代际、年际尺度分量分离,研究时空特征,然后应用REOF进行气温异常的区划,研究局域异常变化的年代际、年际分量的变化特征。结果发现:1)东北各站夏季异常方差中,东北大部分地区的气温异常的年代际变化分量均明显大于年际变化分量。2)区域气温异常的年代际变化主要特征为线性上升趋势。大范围夏季异常高温(低温)常出现在年代际、年际异常同时为正(负)的年份。3)气温异常可划分为南部型、北部型、东部型、西部型4个型,其中南部型和西部型的年代际变化相对重要,而东部型和北部型的年际变化相对重要。  相似文献   
128.
云南省冰雹的时空分布特征   总被引:13,自引:6,他引:13       下载免费PDF全文
利用近40年的云南省冰雹资料,统计分析了云南省冰雹的时空分布特征,进一步揭示了其活动规律及主要影响因素。研究结果表明:冰雹的季节分布比较复杂,呈现出春季和夏季两个峰值的特点;冰雹的季节分布还与海拔高度有关,低海拔地区为春季多雹型,高海拔地区为夏季多雹型;滇西地区冰雹日数的年际变化特征较滇东地区显著而年代际变化特征没有东部地区站点明显;滇东地区表现出了明显的年代际变化特征,目前处于冰雹相对较少时期。从区域来看,年冰雹日数山区较坝区高,高海拔地区较低海拔地区高。  相似文献   
129.
利用山东省伏期降水量资料,用Z指数法划分山东伏期旱涝等级,评定伏期极端旱涝年,并与山东省全年、夏季降水的演变进行比较,发现伏期降水的阶段性特点比较明显,而干旱化趋势不明显,存在10年和2~3年的显著周期。  相似文献   
130.
利用1961~2000年克拉玛依的逐月平均气温、平均最高、最低气温、高温日数等资料,对克拉玛依近40年的气温变化作了较全面的分析。  相似文献   
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