一种信息量和专家证据权重法耦合的成矿预测方法     

陈广洲  徐晓春  汪家权 《测绘科学》2013,38(1):146-149

本文选取安徽石台县丁香地区,以铜多金属矿为例,分析该区的地、物、化、遥数据,选择7个预测变量进行成矿定位预测研究。利用客观成矿预测法-信息量法进行计算,得到成矿预测变量所占的信息量,归一化得到变量的客观权重,依据专家知识,获得上述变量的主观权重,随后,采用D-S证据理论将上述主、客观权重进行融合得到综合权重,并采用该综合权重结合专家证据权重法获得单元格的后验概率,制作成矿有利度的分级色阶图。预测结果表明:该法能有效地综合来自主、客观方面的知识,预测结果更加科学、合理。与单纯的信息量法、专家证据权重法相比,取得了更好的成矿预测效果。  相似文献   

雅鲁藏布江表层沉积物地球化学元素研究   总被引：4，自引：0，他引：4  

陈鹏飞  李潮流  康世昌  张强弓  高少鹏 《地球化学》2012,(4):387-392

雅鲁藏布江流域还没有大的工业污染源,仍然属于自然河流.对雅鲁藏布江16个表层沉积样品的全样、小于20μm 和小于63μm 粒级的32种元素含量进行了测定,并分析了与人类活动密切相关的元素 Cr、Mn、Fe、Co、Ni、Cu、Zn、As、Cd 和 Pb 的含量分布特征,以及这些元素含量与粒径之间的关系.结果表明,多数元素(Cs 除外)与西藏土壤元素背景值相差不大, B、Cr、Ni、As 和 Cs 含量高于中国陆壳元素丰度值,但这些元素主要来源于该流域富含这些元素的页岩、片岩和千枚岩等母岩.由于相似的地球化学行为,沉积物中 Cr、Mn、Fe、Co、Ni、Cu、Zn 之间显著正相关;除 Pb、As 外,一些元素(如 Zn、Ni)与沉积物的粒径显著负相关  相似文献   

珊瑚礁海水pH变化及其对海洋酸化的意义     

陈雪霏  韦刚健  邓文峰  邹洁琼 《热带地理》2016,36(1):41-47

珊瑚钙质骨骼δ11B重建的海水pH时间变化序列显示：珊瑚礁海水pH的长期变化具有显著的年际―年代际波动周期,并且这些波动是区域海洋气候过程和珊瑚礁海水生物活动共同作用的结果。珊瑚礁生态系统中的生物活动（光合呼吸作用和钙化作用）控制着海水碳酸盐系统的组成,调节着海水pH的变化。这一过程在全球气候环境变化和区域海气过程的影响下,一起作用于珊瑚礁海水pH的变化,因而使得不同海域的珊瑚礁海水对海洋酸化的响应有所差别。研究珊瑚礁生物活动在长时间尺度上对海水pH的作用对认识珊瑚礁海水酸化机理十分重要,同时也是了解珊瑚礁生态系统如何响应海洋酸化的重要手段。  相似文献   

珠江三角洲环境梯度上葫芦藓中硫、氮含量 和δ13C、δ15N的差异及其环境指示     

吴清华  闵兴玲  周永章  卢强 《热带地理》2013,33(5):542-548

以华南地区广泛分布的葫芦藓为研究对象,以珠江三角洲环境梯度上的中心城区广州、近郊区肇庆及边缘区怀集3个地理单元作为样品采集地,对样本葫芦藓植物中的硫、氮元素含量和δ13C、δ15N的组成进行了研究。结果表明：葫芦藓植物中硫含量与工业化程度表现出正相关关系,其中硫含量广州、肇庆和怀集依次为2 485.86、1 778.15、1 339.84 mg/kg;葫芦藓氮含量与工业化程度表现出正相关关系,广州、肇庆和怀集依次为 2 106.50mg/kg、2 007.39mg/kg和1 661.88 mg/kg;葫芦藓的C/N值与交通量呈负相关关系,其中C/N值广州为18.377,肇庆18.513,怀集23.905,3地C/N值大小差异揭示了从广州到怀集的环境梯度上,大气氮的主要组份发生了变化,即广州大气中的氮元素来源以工业排放的NOx-N（硝态氮）为主,怀集大气中的氮元素来源以农业排放的NHx-N（铵态氮）为主。  相似文献   

重庆中坝遗址地层Na-Ca元素含量揭示的制盐业兴衰史     

朱诚  姜逢清  马春梅  徐伟峰  黄林燕  郑朝贵  李兰  孙智彬 《地理学报(英文版)》2008,18(3):328-340

Based on dynastic period division and AMS ^14 C dating performed on the sedimentary layers at Zhongba and Yuxi sites,and also the analysis of Na,Ca and Mg of 201 sedimentary samples from Zhongba site and that of Ca and Na in 47 sedimentary samples from Yuxi by using an inductively coupled plasma-mass spectrometry（ICP）,we found that there were 35 time periods when the contents of Ca and Na were reversely correlated,i.e.whenever the content of Ca was the highest,the content of Na was the lowest,and vice versa. Among them,there were 21 time periods when the content of Ca was the highest,and Na was the lowest,indicating that there were about 21 prosperous periods of ancient salt production at Zhongba site since 3000BC.Other 14 time periods with the peak values of Na while the low values of Ca indicate 14 declined periods of salt production at Zhongba site since 3000BC.The conclusion obtained from the reverse relationship between Ca and Na contents in this paper is consistent with that＂the salt production at Zhongba site started in the new stone age,developed in the Xia and Shang dynasties,reached at the heyday in periods from the Western Zhou to the Han Dynasties,maintained stable to develop in the Tang and the Song dynasties,and gradually declined after the Song Dynasty because the sea salt were conveyed into Sichuan region,however,still had production in the 1970s-1980s＂,educed from archeological exploration.All the above mentioned results indicate that there is a reverse relationship obviously between the contents of Na and Ca in sediments at Zhongba site for ancient salt production,which can be used to reveal the process of rise and decline of ancient salt industry at Zhongba site.  相似文献   

Diets of alpine galaxias (Galaxias paucispondylus Stokell) and longjawed galaxias (G. prognathus Stokell) in a South Island,New Zealand,high‐country stream     

M. L. Bonnett  P. M. Sagar  C. R. Docherty 《新西兰海洋与淡水研究杂志》2013,47(4):453-458

Thedietsofthealpinegalaxias(Galaxias paucispondylus Stokell, 1938) and the longjawed galaxias (G. prognathus Stokell, 1940) were studied in Deep Creek, a high‐country stream in the central South Island of New Zealand. Both species are small, slender fish with entirely freshwater life cycles. Their diets were very similar and consisted of aquatic invertebrates, dominated by the larvae of Deleatidium spp. (Ephemeroptera), Hydrobiosis spp. (Trichoptera), and Chironomidae (Diptera). Although diets partly reflected what was available in the stream, both fish selected soft‐bodied prey in preference to cased or harder shelled prey. Both species are probably nocturnal feeders.  相似文献   

论地缘政治学的核心——地理要素   总被引：2，自引：0，他引：2  

刘新华 《世界地理研究》2009,18(1):6-12

近代以来,以领土为物质基础的民族或者国家间的竞争和合作均发生在特定的地理空间之内。人们对地理空间与民族或者国家间相互关系影响的认识反映在国际关系理论中。就是地缘政治学,换言之,地缘政治是在对国际上各种政治力量及其相互关系进行地理空间分析的基础上,为维护国家利益制定适当的对外政策和战略的一种理论。地缘政治最基本的内核是地理要素．即地理位置、国土幅员、邻国、地形与气候、资源以及距离等。科学认识地缘政治学基本的地理要素．是正确把握、运用地缘政治学的先决条件。  相似文献   

旅游网络地图及其研究内容探析   总被引：1，自引：0，他引：1  

吴增红  陈毓芬 《测绘科学技术学报》2006,23(6):440-443

旅游网络地图的研究对网络地图的发展以及网络时代旅游业的发展都有着非常重要的意义.由于缺乏基于地图学和旅游学的旅游网络地图研究,旅游网络地图的发展受到影响.首先探讨了旅游网络地图的概念及特点,然后对大量旅游网站进行了旅游网络地图的现状调查,分析了存在的主要问题,最后针对这些问题并结合旅游网络地图的发展趋势,提出了旅游网络地图设计的主要研究内容及研究思路.  相似文献   

Tourmaline geochemistry and boron isotopic variations as a guide to fluid evolution in the Qiman Tagh W-Sn belt,East Kunlun,China     

Zhen Zheng  Yanjing Chen  Xiaohua Deng  Suwei Yue  Hongjin Chen  Qingfei Wang 《地学前缘(英文版)》2019,10(2):569-580

The Qiman Tagh W-Sn belt lies in the westernmost section of the East Kunlun Orogen, NW China, and is associated with early Paleozoic monzogranites, tourmaline is present throughout this belt. In this paper we report chemical and boron isotopic compositions of tourmaline from wall rocks, monzogranites, and quartz veins within the belt, for studying the evolution of ore-forming fluids. Tourmaline crystals hosted in the monzogranite and wall rocks belong to the alkali group, while those hosted in quartz veins belong to both the alkali and X-site vacancy groups. Tourmaline in the walk rocks lies within the schorl-dravite series and becomes increasingly schorlitic in the monzogranite and quartz veins. Detrital tourmaline in the wall rocks is commonly both optically and chemically zoned,with cores being enriched in Mg compared with the rims. In the Al-Fe-Mg and Ca-Fe-Mg diagrams,tourmaline from the wall rocks plots in the fields of Al-saturated and Ca-poor metapelite, and extends into the field of Li-poor granites, while those from the monzogranite and quartz veins lie within the field of Li-poor granites. Compositional substitution is best represented by the MgFe_(-1), Al(NaR)_(-1), and AlO(Fe(OH))_(-1) exchange vectors. A wider range of δ~(11)B values from -11.1‰ to -7.1‰ is observed in the wall-rock tourmaline crystals, the B isotopic values combining with elemental diagrams indicate a source of metasediments without marine evaporates for the wall rocks in the Qiman Tagh belt. The δ~(11)B values of monzogranite-hosted tourmaline range from -10.7‰ and-9.2‰, corresponding to the continental crust sediments, and indicate a possible connection between the wall rocks and the monzogranite. The overlap in δ~(11)B values between wall rocks and monzogranite implies that a transfer of δ~(11)B values by anataxis with little isotopic fractionation between tourmaline and melts. Tourmaline crystals from quartz veins have δ~(11)B values between -11.0‰ and-9.6‰, combining with the elemental diagrams and geological features, thus indicating a common granite-derived source for the quartz veins and little B isotopic fractionation occurred. Tourmalinite in the wall rocks was formed by metasomatism by a granite-derived hydrothermal fluid, as confirmed by the compositional and geological features.Therefore, we propose a single B-rich sedimentary source in the Qiman Tagh belt, and little boron isotopic fractionation occurred during systematic fluid evolution from the wall rocks, through monzogranite, to quartz veins and tourmalinite.  相似文献   

Geochemical Constraints on the Origin and Evolution of Spring Waters in the Changdu‐Lanping‐Simao Basin,Southwestern China     

QIN Xiwei  MA Haizhou  ZHANG Xiying  CHENG Huaide  HAN Jibin  LI Yongshou  MIAO Weiliang  HAI Qingyu 《《地质学报》英文版》2019,93(4):1097-1112

Chemical and isotopic data were measured for 51 leached brine springs in the Changdu-Lanping-Simao Basin (CD-LP-SM), China. The predominance of Cl and Na, saturation indices of carbonate minerals, and Na/Cl and Ca/SO4 ratios of ~1 suggest that halite, sulphate, and carbonate are the solute sources. Integration of geochemical, δ18O, and δD values suggests that springs are mainly derived from meteoric water, ice-snow melt, and water-rock interactions. B concentrations range from 0.18 to 11.9 mg/L, with δ11B values of ?4.37‰ to +32.39‰, indicating a terrestrial source. The δ11B-B relationships suggest B sources of crustal origin (marine carbonates with minor crust-derived volcanics); we did not identify a marine or deep mantle origin. The δ11B values of saline springs (+4.61‰ to +32.39‰) exceed those of hot (?4.37‰ to +4.53‰) and cold (?3.47‰ to +14.84‰) springs; this has contributed to strong water-rock interactions and strong saturation of dissolved carbonates. Conversely, the global geothermal δ11B-Cl/B relationship suggests mixing of marine and non-marine sources. The δ11B-Cl/B relationships of the CD-LP-SM are similar to those of the Tibet geothermal belt and the Nangqen Basin, indicating the same B origin. These differ from thermal waters controlled by magmatic fluids and seawater, suggesting that B in CD-LP-SM springs has a crustal origin.  相似文献