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71.
Personalized routing counts on traveler’s preferences which are usually based on different criteria, such as shortest, fastest, least traffic, or less expensive (e.g., less fuel cost, toll free). However, people are increasingly becoming concerned about the adverse health effects of exposure to air pollution in chosen routes. Exposures to elevated air pollution concentrations particularly endanger children, pregnant women, elderly people, and people with asthma and other respiratory conditions. Choosing routes with least air pollution exposure (APE) is seen as one approach to minimize the level of pollution exposed, which is a major public health issue. Routing algorithms use weights on segments of road networks to find optimum routes. While existing weights are commonly distance and time, among a few others, there is currently no weight based on APE to compute least APE routes. In this paper, we present a weight function that computes weight based on APE. Two different approaches, geostatistical and non-geostatistical, were used to compute APE weight. Each approach was evaluated, and the results indicate that the APE weight is suitable for computing least APE routes.  相似文献   
72.
The Xinlu Sn‐polymetallic ore field is located in the western Nanling Polymetallic Belt in northeastern Guangxi, South China, where a number of typical skarn‐, hydrothermal vein‐type tin deposits have developed. There are two types of Sn deposits: skarn‐type and sulfide‐quartz vein‐type. The tin mineralizations mainly occur on the south side of the Guposhan granitic complex pluton and within its outer contact zone. To constrain the Sn mineralization age and further understand its genetic links to the Guposhan granitic complex, a series of geochronological works has been conducted at the Liuheao deposit of the ore field using high‐precision zircon SHRIMP U‐Pb, molybdenite Re‐Os, and muscovite Ar‐Ar dating methods. The results show that the biotite‐monzogranite, which is part of the Xinlu intrusive unit of the Guposhan complex pluton, has a SHRIMP U‐Pb zircon age of 161.0 ± 1.5 Ma. The skarn‐type ore has a 40Ar‐39Ar muscovite plateau age of 160 ± 2 Ma (same as its isochron age), and the sulfide‐quartz vein‐type ore yields an Re‐Os molybdenite isochron age of 154.4 ± 3.5 Ma. The magmatic‐hydrothermal geochronological sequence demonstrated that the hydrothermal mineralization took place immediately following the emplacement of the monzogranite, with the skarn metasomatic mineralization stage predating the sulfide mineralization stage. Geochronologically, we have compared this ore field with 26 typical Sn deposits distributed along the Nanling Polymetallic Belt, leading to the suggestion of the magmatic‐metallogenic processes in the Xinlu ore field (ca. 161–154 Ma) as a component of the Early Yanshanian large‐scale Sn‐polymetallic mineralization event (peaked at 160–150 Ma) in the Nanling Range of South China. Petrogenesis of Sn‐producing granite and Sn‐polymetallic mineralization were probably caused by crust–mantle interaction as a result of significant lithospheric extension and thinning in South China in the Late Jurassic.  相似文献   
73.
The large-scale Bayanbaolege Ag polymetallic deposit is situated in the Tuquan–Linxi Fe-Sn-Cu-Pb-Zn-Ag metallogenic sub-belt in eastern slopes of the southern Great Xing’an Range, NE China. The sulfide-quartz vein-type orebodies in the deposit are hosted primarily in the Early Cretaceous granodiorite porphyry and Late Permian strata. Three primary paragenetic stages of veining have been identified: (I) arsenopyrite- pyrite-quartz stage, (II) pyrite-sphalerite-quartz stage, and (III) galena-silver minerals (pyrargyrite, argentite, and pearceite)-calcite stage. The Rb–Sr dating of sulfides yielded an isochron age of 129.9 ± 2.9 Ma (MSWD = 2.1) for the sphalerite, which constrains the mineralization age to the Early Cretaceous. Rb and Sr concentrations in the sulfides ranged from 0.0940 to 1.0294 ppm and 0.0950–3.3818 ppm, respectively. The initial 87Sr/86Sr value of the sphalerite was 0.70852 ± 0.00018, indicating that the mineralized materials were derived from the mixed crust-mantle source area. S isotope analysis showed that the δ34S values of the sulfide samples varied in a narrow range, from −1.5‰ to +1.3‰ (mean −0.65‰), indicating a magmatic S source. Pb isotopic ratios of the sulfides (206Pb/204Pb = 18.306–18.416, 207Pb/204Pb = 15.524–15.605, 208Pb/204Pb = 38.095–38.479) and the granodiorite porphyry (206Pb/204Pb = 18.341–18.933, 207Pb/204Pb = 15.539–15.600, 208Pb/204Pb = 38.134–38.944) reflect that the ore-forming materials originated from contemporaneous magma with Early Cretaceous granodiorite porphyry. This study of the Bayanbaolege deposit and other hydrothermal deposits in the area provides compelling evidence that the widespread Mesozoic magmatism and mineralization in the southern Great Xing’an Range occurred in an intracontinental extensional tectonic setting, which was associated with the westward subduction of the paleo-Pacific plate.  相似文献   
74.
云南保山核桃坪铅-锌矿床地质特征   总被引:6,自引:0,他引:6  
保山核桃坪铅-锌矿为一中型铅-锌矿床。矿体赋存于上寒武统核桃坪组,主要受近SN向的层间断裂(F1)及次级断裂构造控制,岩石(性)控矿也十分明显,成矿作用与矽卡岩化密切相关。通过对该矿床地质特征的系统分析以及对矿床围岩蚀变、控矿因素的深入研究,认为该矿床主要矿化作用是深部高温成矿流体贯入并与围岩发生矽卡岩化蚀变,随后发生矿化作用。矿床应属矽卡岩型铅-锌矿床。  相似文献   
75.
陕西商县蔷薇辉石玉石矿床地质、工艺性质及成因   总被引:1,自引:0,他引:1  
陕西商县蔷薇辉石(粉翠)矿床是陕西省首次发现并评价的玉石矿床。蔷薇辉石产于宽坪群四岔口组中段下部二云石英片岩所夹的含锰石英白云石大理岩、含锰石英岩等含锰岩中。矿体既成层分布又相对集中。粉翠玉料质优且加工工艺性能良好。蔷薇辉石矿床的形成主要经历了沉积期和区域变质期两大阶段。成因类型属变质岩型低温变质相蔷薇辉石矿床。  相似文献   
76.
重庆酉阳坝竹坨汞、铅锌矿床地质特征及成因分析   总被引:1,自引:0,他引:1  
酉阳坝竹坨汞、铅锌矿叠生并主要呈似层状和脉状产于中寒武统高台组、石冷水组白云岩中,矿石矿物组合简单,主要有辰砂、方铅矿、闪锌矿、方解石、白云石、石英、重晶石、萤石等。矿床主要受地层、岩性及构造的控制。矿床为多期热液成矿。  相似文献   
77.
2022年北京冬奥会将在我国举办,比赛项目以雪上项目为主。赛道雪质是雪务工作的核心问题,而目前国内关于竞技型滑雪场赛道雪质研究少有涉及。通过研究以人造雪为主的河北省万龙滑雪场赛道雪质特性,了解我国竞技型雪场目前赛道现状。通过比较,找出与国际雪联要求标准赛道雪质的差距,依据赛道雪质变化特性,提出雪质保持和提升方案,并对影响雪质的要素进行风险评估,以提升我国赛事雪务工作的科研能力和技术水平,为冬奥会成功举办提供科学依据和服务。  相似文献   
78.
《Geofísica Internacional》2014,53(2):199-210
Geophysical methods are widely used in mineral exploration. This paper discusses the results of geological and geophysical studies in supergene manganese deposits of southern Brazil. Mineralized zones as described in geological surveys were characterized as of low resistivity (20Ω.m) and high chargeability (30ms), pattern found also in oxides and sulfite mineral deposits. Pseudo-3D modeling of geophysical data allowed mapping at several depths. A relationship between high chargeability and low resistivity may define a pattern for high grade gonditic manganese ore. Large areas of high chargeability and high resistivity may result in accumulation of manganese and iron hydroxides, due to weathering of the gonditic ore, dissolution, percolation and precipitation.  相似文献   
79.
张文源 《矿产与地质》1996,10(3):159-164
石缸河锡矿床在空间上,时间上和成因上与志本山花岗岩演化分异晚期形成的浅色细粒白云母花岗岩有着密切联系,属岩浆期后热液矿床。  相似文献   
80.
本文概述了金坑冲金矿地质特征,并对其矿化规律作了总结。在此基础上,依据地质类比与土壤地球化学测量成果,指出王家湾一丫头山一带,是找石英脉一蚀变岩型金矿的远景区。  相似文献   
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