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Evaluating mountain water scarcity on the county scale: a case study of Dongchuan District, Kunming, China 被引量:2
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作者 LI Jie DENG Wei ZHANG Ji-fei 《Journal of Mountain Science》 SCIE CSCD 2019年第4期744-754,共11页
Mountain water, which contributes 50% to 90% to the lower reaches of the watershed, has a considerably low utility efficiency. The water accessibility could be a quantitative measure of water scarcity in the mountains... Mountain water, which contributes 50% to 90% to the lower reaches of the watershed, has a considerably low utility efficiency. The water accessibility could be a quantitative measure of water scarcity in the mountains. It can be used effectively for emergency water shortage planning and water resource management. In the present study, Dongchuan District, a typical county in the Hengduan Mountains in Yunnan province of Southwest China, was selected as the study area, and the minimal cumulative resistance(MCR) model was used to simulate the least-cost path(LCP) from 1255 point features of natural villages, as well as 12,368 dryfield centroids, to their respective surrounding river systems, which serve as a source for emergency drinking water and irrigation during droughts. The average length of the LCP for each administrative village was calculated to represent the accessibility to water sources for agricultural production and daily life in these mountain villages. The distribution of population and dryfields, as well as other geographic elements, were analyzed to classify the degree of water scarcity in these villages. The results indicate that the area facing the highest risk of water shortage for agricultural irrigation is located in northern Dongchuan, in particular along the two sides of the Xiaojiang Valley, and that the area with the highest risk of water shortage for daily life needs is located along the Xiaojiang Valley. 展开更多
关键词 WATER SCARCITY MOUNTAINS WATER ACCESSIBILITY MCR model dongchuan District
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Platinum-group element geochemistry of mafic rocks from the Dongchuan area,southwestern China 被引量:2
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作者 Siqi Yang Hong Zhong +2 位作者 Weiguang Zhu Wenjun Hu Zhongjie Bai 《Acta Geochimica》 EI CAS CSCD 2017年第1期52-65,共14页
Mafic intrusions and dykes are well preserved in the Yinmin and Lanniping districts, located within the western margin of the Yangtze Block, SW China. Although these mafic rocks from the two areas formed during differ... Mafic intrusions and dykes are well preserved in the Yinmin and Lanniping districts, located within the western margin of the Yangtze Block, SW China. Although these mafic rocks from the two areas formed during different periods, they share similar ranges of PGE concentration. Most of the Yinmin gabbroic dykes contain relatively high PGE concentrations (PGEs=13.9-87.0 ppb) and low S contents (0.003 %-0.020 %), higher than the maximum PGE concentrations of mafic magmas melting from the mantle. Two exceptional Yinmin samples are characterized by relatively low PGE (PGEs = 0.31-0.37 ppb)and high S (0.114 %-0.257 %) contents. In contrast, most samples from the Lanniping gabbroic intrusion have low PGE con- centrations (PGEs = 0.12-1.02 ppb) and high S contents (0.130 %-0.360 %), except that the three samples exhibit relatively high PGE (PGEs=16.3-34.8 ppb) and low S concentrations (0.014 %-0.070 %). All the Yinmin and Lanniping samples are characterized by the enrichment of PPGE relative to IPGE in the primitive-mantle normalized diagrams, and the high-PGE samples exhibit obvious Ru anomalies. This study suggests that during the ascent of the parental magma, removal of Os-Ir-Ru alloys and/or chro- mite/spinel leads to high Pd/Ir ratios and Ru anomalies for the Yinmin high-PGE samples and relatively lower Pd/lr ratios and Ru anomalies for the Lanniping low-PGE samples. We propose that the magmas parental to the Yinmin gabbroic dykes are initially S-unsaturated, and subsequently, minor evolved magma reached sulfur saturation and led to sulfide segregation. Although the Lanniping parental magmas are originally not saturated in S, the high Cu/Pd ratios (3.8× 10^4 to 3.2 × 10^6) for most of the Lanniping samples indicate the S-saturated state and sulfide segregation. A calculation shows that the PGE-poor magmas might have experienced 0.01%-0.1%sulfidesegregationinthemagma chamber. Therefore, our study provides a possible opportunity to discover PGE-enriched sulfide mineralization some- where near or within the Lanniping mafic intrusion. 展开更多
关键词 Mafic intrusions and dykes PLATINUM groupelement Sulfide saturation dongchuan area
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Zircon U–Pb Ages and Lu–Hf Isotope of the Dongchuan Group in Central Yunnan, China, and their Geological Significance 被引量:2
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作者 HAN Kunying ZHANG Heng +3 位作者 DING Xiaozhong REN Liudong SHI Chenglong PANG Jianfeng 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2020年第4期1093-1116,共24页
On the southwestern margin of the Yangtze Block, the Dongchuan Group consists of slightly metamorphosed sedimentary rocks, including silty slate, argillaceous slate, clayey slate, arkose, dolomite, and minor volcanic ... On the southwestern margin of the Yangtze Block, the Dongchuan Group consists of slightly metamorphosed sedimentary rocks, including silty slate, argillaceous slate, clayey slate, arkose, dolomite, and minor volcanic rocks. To date, it is still a controversy over the depositional age and stratigraphic sequence of the Dongchuan Group. In this study, we analyzed five samples of meta-sedimentary rocks and one sample of meta-tuff from the Yinmin, Luoxue and Etouchang Formations of the Dongchuan Group in the Yuxi region for detrital zircon U-Pb ages and Lu-Hf isotope. The detrital zircon ages of the meta-sediments vary from 3073 to 1703 Ma, mainly clustered at three periods, from 1889 to 1840, 2490 to 2008 and 2878 to 2844 Ma. The youngest age peak of all the samples is ~1859 Ma, with the εHf(t) values of the zircons ranging from-20.3 to +4.3 and more than 90% being negative, indicating that the Paleoproterozoic crustal accretion on the southwestern margin of the Yangtze Block was dominated by reworking of the ancient crustal materials involved in the assembly and breakup of the Columbia supercontinent. Another important age range is between 2490 Ma and 2008 Ma, with εHf(t) values from-14.7 to +8.9 and 70% of them are negative, suggesting that the magmatism in the source area was also dominated by reworking and recycling of the ancient crustal materials, with minor juvenile mantle substances added. The detritus was probably derived from the Paleoproterozoic crystalline basement in the southern Yuxi region. The oldest peak age is ~2847 Ma and the εHf(t) values are from-7.7 to +7.0 with 50% of both positive and negative values, demonstrating a possible ~2.85 Ga ancient continental nucleus on the southwestern margin of the Yangtze Block and substantial growth in juvenile crust materials during this period. Besides, the weighted average age of the zircons from the meta-tuff of the Etouchang Formation is 1677 ± 14 Ma. Combining the previous research data and this study, we can constrain the depositional age of the Dongchuan Group in central Yunnan Province to the period from the late Paleoproterozoic to early Mesoproterozoic, slightly earlier than that of the Dongchuan Group in the Dongchuan area near to the southwestern Sichuan Province. The depositional age of the Dongchuan Group is older than that of the Kunyang Group. 展开更多
关键词 ZIRCON depositional age Lu-Hf isotope dongchuan Group Kunyang Group Yangze Block
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SUPERPOSING-REWORKING METALLOGENESIS OF JINNINGIAN MAFIC VOLCANIC-INTRUSION COMPLEX IN DONGCHUAN COPPERFIELD 被引量:1
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作者 Liu Jishun Wu Yanzhi 《Transactions of Nonferrous Metals Society of China》 SCIE EI CAS CSCD 1996年第1期1-5,共5页
Mafic"intrusive rocks",distributed greatly within Dongchuan strata-bound copperfield and really comprising volcanic,subvolcanic and volcano plutonic rocks,should be termed as volcanic-intrusive complex(VIC).... Mafic"intrusive rocks",distributed greatly within Dongchuan strata-bound copperfield and really comprising volcanic,subvolcanic and volcano plutonic rocks,should be termed as volcanic-intrusive complex(VIC).Geology and geochemistry of Jinningian VIC and its relation to Cu ores reaffirm that VIC play an important role in mineralizations,which are not only vein bonanzas deduced from coose beds,but also new orebodies occurred within VIC.Bonanzas of superposing-reworking type and orebodies of magmatic liquation-differentiation type in the depth are suggested to be found in the largely developing VIC area. 展开更多
关键词 volcanic-intrusive complex Jinningian period superposing-reworking dongchuan COPPERFIELD
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Ecological Compensation-assisted Relocation in Extreme Poverty-stricken Counties in China’s Ecologically Vulnerable Areas: Taking Dongchuan District of Yunnan Province as an Example
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作者 Feng QIU Zisheng YANG 《Asian Agricultural Research》 2019年第8期34-44,共11页
Ecology-oriented poverty alleviation is not only a livelihood project that affects the vast majority of rural people but also a major project to win the fight against poverty. It is also an indispensable income compon... Ecology-oriented poverty alleviation is not only a livelihood project that affects the vast majority of rural people but also a major project to win the fight against poverty. It is also an indispensable income component for the relocation of poor farmers. Dongchuan District,located at the intersection of Jinsha River and Xiaojiang River,is one of the key counties for poverty alleviation and development in China with a wide range of poverty and extreme poverty. The incidence of poverty reached 24. 36%. The ecology is fragile,and earthquake outbreaks frequently. Dongchuan District is a national key monitoring and defense area for earthquakes. A large number of goafs,subsidence areas and geological hazard areas have been formed in the mining area. The number of dangerous houses is large,and ' it has no way of supporting its own inhabitants' is the key point,difficulty and focus of the county’s poverty alleviation. Relocation is a must-have measure to move away from poverty. It is also complex system engineering,which is policy-oriented and difficult. Since 2017,Dongchuan District has regarded relocation has the top priority for poverty alleviation. It has strictly implemented national,provincial and municipal policies,focused on the overall goal of ' moving,securing and getting rich',and strongly promoted the relocation work for poverty alleviation. Obvious social,economic and ecological benefits have been achieved. Successful relocation,combined with ecology-oriented poverty alleviation and other targeted poverty alleviation measures,Dongchuan District’s fight against poverty has achieved a decisive victory. At the end of December 2018,the incidence of poverty in the region fell to 1. 09%,and 129 poor villages( including 86 extremely poor villages) had been successfully lifted out of poverty. This paper analyzes and condenses the specific practices,main achievements,benefits,successful experiences and implications of the region’s relocation combined with ecology-oriented poverty alleviation model,so as to provide necessary reference for the innovation of relocation in poverty-stricken counties of Yunnan Province and similar provinces( cities,districts). 展开更多
关键词 Ecologically VULNERABLE area POVERTY alleviation ECOLOGICAL compensation RELOCATION dongchuan DISTRICT
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Poverty Alleviation through Employment Promotion in Extreme Poverty-stricken Areas in Western China: A Case Study of Targeted Poverty Alleviation through Employment Promotion in Awang Town,Dongchuan District
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作者 Yi LOU Zisheng YANG 《Asian Agricultural Research》 2019年第7期55-62,共8页
Poverty alleviation through employment promotion is to promote the poor households to get rid of poverty through promoting employment to increase income. It is the most effective and direct way out of poverty. Dongchu... Poverty alleviation through employment promotion is to promote the poor households to get rid of poverty through promoting employment to increase income. It is the most effective and direct way out of poverty. Dongchuan District, located in the alpine valley area of northeastern Yunnan, is a typical extreme poverty-stricken county in China. Under its jurisdiction, Awang Town is a mountainous township with a wide area of poverty and an extreme poverty. The incidence of poverty in 2015 reached 35.39%. In recent years, through the implementation of various policies to combat poverty, combined with the advantages as a traditional "hometown of migrant labor", focusing on employment- promoting poverty alleviation work, Awang Town has made certain achievements in poverty alleviation work. By the end of 2018, the poverty rate in the town fell to 0.57%, marking a major victory in the town s fight against poverty. Through field investigations, this article summarizes the main practices of Awang Town to carry out employment-promoting targeted poverty alleviation, analyzes the poverty alleviation achievements and successful experience of the town s employment-promoting targeted poverty alleviation work and discusses the promotion and application of this model so as to provide reference Yunnan Province and other poverty-stricken areas to carry out employment-promoting poverty alleviation. 展开更多
关键词 EXTREME POVERTY-STRICKEN areas POVERTY alleviation though employment promotion Model POVERTY alleviation achievements Awang TOWN dongchuan District
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Investigation on the Green Planting Situation of Dongchuan Barren Hills in Kunming City
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作者 Haifan WANG 《Agricultural Biotechnology》 CAS 2018年第5期252-255,共4页
Dongchuan District of Kunming City has undulating terrain with large fluctuations, fragile ecological environment, low rainfall and high evaporation, coupled with frequent debris flow activities, resulting in very low... Dongchuan District of Kunming City has undulating terrain with large fluctuations, fragile ecological environment, low rainfall and high evaporation, coupled with frequent debris flow activities, resulting in very low forest coverage rate in Dongchuan. In this study, a comprehensive and systematic investigation was carried out to the green planting of barren hills in Dongchuan District from January to June, 2016. The results showed that the major planting tree species in the region with an altitude of less than 1 600 m were Leucaena leucocephala, Cupressus torulosa, L. leucocephala, C. torulosa, Celtis yunnanensis, Melia azedarach , among which L. leucocephala had become of pioneer tree species of afforestation in the Dongchuan dry-hot valley. The major planting tree species at the altitude of 1 600-2 500 m were C. torulosa, Sabina chinensis, Alnus nepalensis, C. yunnanensis, and Pinus armandi , and at the altitude of over 2 500 m, the major tree species were Sabina chinensis, Abies georgei var. smithii, P.densata. Based on the investigation, suggestions were proposed for the existing problems in the greening and planting of Dongchuan barren hills, in order to provide certain theoretical basis for the sustainable development of forestry in Dongchuan. 展开更多
关键词 dongchuan Ecological environment Barren hill Green planting
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Isotope Geochemistry of the Dongchuan Copper Deposit, Yunnan, SW China: Stratigraphic Chronology and Application of Lead Isotopes in Geochemical Exploration 被引量:12
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作者 常向阳 朱炳泉 《Chinese Journal Of Geochemistry》 EI CAS 2002年第1期65-72,共8页
In this paper the Pb-Pb isochron method was used to determine the isotopic ages of the Luoxue Formation dolomites (1716±56 Ma), the Heishan Formation carbonaceous slates (1607±128 Ma) of the middle sub-group... In this paper the Pb-Pb isochron method was used to determine the isotopic ages of the Luoxue Formation dolomites (1716±56 Ma), the Heishan Formation carbonaceous slates (1607±128 Ma) of the middle sub-group of the Kunyang Group and the Dayingpan Formation carbonaceous slates (1258±70Ma) of the upper sub-group of the Kunyang Group. The age of the middle sub-group of the Kunyang Group is about 1800-1600 Ma, belonging to the Late Paleo-Proterozoic, and that of the Dayingpan Formation in the upper sub-group of the Kunyang Group is about 1200-1300 Ma, belonging to the Middle Proterozoic. In addition, the Pb isotope chemical exploration techniques were used to study systematically the Pb isotopic compositions of rocks and ores across the No.14 vein in the middle segment of the No.1 pit of the Tangdan copper deposit and the result showed that the Pb isotope V\-1 values are negatively correlated with the copper contents. It is the first trial to use the systematic section method to conduct Pb isotope chemical exploration. 展开更多
关键词 铜矿床 同位素地球化学 铅同位素 云南 指示同位素 地层年代学 调查
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东川区草地蝗虫多样性与当地环境之间的关系
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作者 冯加德 王鹏 +3 位作者 王艺璇 冯丹 袁瑞玲 陈鹏 《西部林业科学》 CAS 北大核心 2024年第2期127-132,141,共7页
为探究草地蝗虫的多样性特征,以东川区的高山和河谷6个不同海拔(1 050、1 155、1 250、1 350 m、2 220及3 100 m)的草地作为采样地,通过野外随机网捕的方法对草地蝗虫进行采样,进行种类鉴定和数据分析。结果显示:东川区草地蝗虫为东洋区... 为探究草地蝗虫的多样性特征,以东川区的高山和河谷6个不同海拔(1 050、1 155、1 250、1 350 m、2 220及3 100 m)的草地作为采样地,通过野外随机网捕的方法对草地蝗虫进行采样,进行种类鉴定和数据分析。结果显示:东川区草地蝗虫为东洋区系,共有4科15属19种;高山区的草地蝗虫的Shannon-Wiener多样性指数和Pielou均匀度指数均高于河谷;河谷地区的不同海拔带中,多样性指数最高的是海拔1 155 m区域,均匀度指数最高的是海拔1 250 m区域;高山地区的不同海拔带中,多样性指数最高的是海拔2 220 m区域,均匀度指数最高的是海拔1 350 m区域。结果表明:东川区的草地蝗虫虫口密度低(平均0.08头/m2),处于有虫不成灾的状态,证明当地草原的生态系统相对稳定,其中高山区域的草地蝗虫多样性指数较高,应加强对高山地区草地的蝗虫监测。 展开更多
关键词 东川区 草地蝗虫 多样性
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积石山M6.2地震前通渭东川地震台流体观测数据异常分析
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作者 周卫东 道伟 +4 位作者 王娟 姜佳佳 田野 牛延平 苏小芸 《高原地震》 2024年第2期1-6,共6页
2023年12月18日甘肃省临夏回族自治州积石山发生M6.2地震,震前通渭东川地震台流体观测井水温和气氡浓度值出现异常。通过分析地震前后水温和气氡浓度数据,发现水温值出现“下降-保持低值-回升(震时)”的异常变化过程,气氡浓度值出现上升... 2023年12月18日甘肃省临夏回族自治州积石山发生M6.2地震,震前通渭东川地震台流体观测井水温和气氡浓度值出现异常。通过分析地震前后水温和气氡浓度数据,发现水温值出现“下降-保持低值-回升(震时)”的异常变化过程,气氡浓度值出现上升,且与水温下降有较好的对应性。因此认为水温和气氡浓度变化有可能是积石山M6.2地震的前兆异常。 展开更多
关键词 积石山M6.2地震 通渭东川地震台 水温 气氡浓度
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小江断裂带东川—寻甸段大地电磁成像及深部孕震环境 被引量:1
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作者 崔腾发 陈小斌 +4 位作者 李文军 李文巧 李鑫 谢兴兵 周磊 《地球物理学报》 SCIE EI CAS CSCD 北大核心 2023年第10期4224-4240,共17页
小江断裂带是青藏高原物质向东南方向逃逸的东边界中的一段,具有较强的地震活动性.小江断裂带东川—寻甸段经历过三次6.5级以上强震,对其深部电性结构的探测,可以为研究三次历史强震的深部孕震环境提供重要依据.大地电磁成像结果显示研... 小江断裂带是青藏高原物质向东南方向逃逸的东边界中的一段,具有较强的地震活动性.小江断裂带东川—寻甸段经历过三次6.5级以上强震,对其深部电性结构的探测,可以为研究三次历史强震的深部孕震环境提供重要依据.大地电磁成像结果显示研究区下地壳存在显著的高导结构,可能含有较高比例的熔融物质,具有较低的强度/黏度.小江断裂带在深度10 km表现为明显的结构边界,有利于断裂带的剪切变形.断裂带上的强震可能主要受上地壳高阻结构的控制.上地壳中,小江断裂带东支断裂在田坝随高阻结构向南转折;功山地区东支断裂两侧的高阻体紧靠.两个条件共同阻碍了东支断裂在局部的左旋走滑及地震破裂的传播.小江断裂带西支断裂在嵩明以北表现为上地壳三个高阻体之间的边界,坚硬的高阻体相互接触可能使断层局部存在阻碍断层走滑的构造,为强震的发生提供必要的结构条件. 展开更多
关键词 小江断裂带 大地电磁成像 孕震环境 三维电性结构 东川-寻甸段
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扬子西缘中元古界黑山组MISS构造的发现及其古环境意义 被引量:5
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作者 刘军平 刘卫东 +4 位作者 李维科 李健 何世军 莫雄 关奇 《地质论评》 CAS CSCD 北大核心 2023年第2期461-468,共8页
通过1∶5万区域地质调查及剖面研究,在扬子西缘云南东川地区黑山组发现大套流纹质凝灰质板岩夹层,获得LA-ICP-MS锆石U-Pb年龄加权平均值为1522±15 Ma,同时在中元古界黑山组泥质板岩中发现微生物成因沉积构造(MISS),通过对MISS及围... 通过1∶5万区域地质调查及剖面研究,在扬子西缘云南东川地区黑山组发现大套流纹质凝灰质板岩夹层,获得LA-ICP-MS锆石U-Pb年龄加权平均值为1522±15 Ma,同时在中元古界黑山组泥质板岩中发现微生物成因沉积构造(MISS),通过对MISS及围岩进行电子探针、XRF分析及能谱分析,研究发现MISS主要成分为P、S、Fe、Cr,明显是微生物沉积过程中形成的化合物特征;而围岩主要为Al、Si、K、Mg、Ti,为正常黏土质矿物组成元素,两者存在较大差别。笔者等发现的MISS是目前扬子西南缘已知发现的最古老的MISS;MISS在黑山组的出现表明了中元古代时期微生物群落的繁盛,反映了当时沉积环境为滨岸浅水潮上带,在凹陷的位置微生物参与形成了这样不规则的条带皱饰构造,为中元古代地层微生物区域对比、古环境研究提供重要的参考资料,对于恢复康滇裂谷盆地的生物—沉积作用和环境演化具有重要意义。 展开更多
关键词 微生物成因沉积构造 古环境 锆石U-PB 中元古界 黑山组 东川地区
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清前期西南矿区“夷民”的生存策略与边疆秩序——以东川府为中心
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作者 李培娟 《原生态民族文化学刊》 2023年第6期77-89,154,155,共15页
清康雍年间西南大规模的改土归流之后,西南地区的矿藏得到进一步开发,矿业的发展吸引了大量内地移民前往西南。云南东川府作为清代铜矿最重要的产区,围绕着矿业开发,“夷民”、移民、地方官员、彝族土目等各方势力在这里展开了频繁的交... 清康雍年间西南大规模的改土归流之后,西南地区的矿藏得到进一步开发,矿业的发展吸引了大量内地移民前往西南。云南东川府作为清代铜矿最重要的产区,围绕着矿业开发,“夷民”、移民、地方官员、彝族土目等各方势力在这里展开了频繁的交往。在这个复杂的互动过程中,少数民族并非被动地“被同化”或“随波逐流”,而是一直从自身利益出发,巧妙地周旋于各方势力间,在竞争、合作中适时地融入社会变革中。 展开更多
关键词 边疆 矿业 夷民 东川 生存策略
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云南东川铜矿带碳、氧同位素特征及成矿机制讨论
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作者 曾瑞垠 王蒙 +3 位作者 王幻 祝新友 张雄 王迪恒 《矿产勘查》 2023年第9期1595-1603,共9页
东川铜矿带地处云南东川盆地,属于沉积岩容矿层状铜矿带,发育有稀矿山式铁铜矿体、东川式铜矿体、桃园式铜矿体等多类型铜矿体。为探讨东川铜矿带的成矿机制,本文通过对东川铜矿带各类型矿体的碳、氧同位素分析,结合前人研究成果,发现... 东川铜矿带地处云南东川盆地,属于沉积岩容矿层状铜矿带,发育有稀矿山式铁铜矿体、东川式铜矿体、桃园式铜矿体等多类型铜矿体。为探讨东川铜矿带的成矿机制,本文通过对东川铜矿带各类型矿体的碳、氧同位素分析,结合前人研究成果,发现相对于赋矿白云岩,稀矿山式、东川式、桃园式铜矿体的白云石δ13C值呈降低的趋势,东川式铜矿体的包裹体δ13C值为-16.40‰~-0.20‰,桃园式铜矿体的包裹体δ13C值为-18.40‰~-4.20‰,包裹体中的δ13C值呈现明显的低值。碳、氧同位素特征说明成矿流体的碳源主要来自于海相碳酸盐的溶解作用,其次来自于有机质的氧化作用和脱羟基作用,有机质亦参与了成矿作用。含矿卤水运移到具还原性质的落雪组白云岩和黑山组炭质板岩中,与含有机质地层和含有机质流体发生氧化还原反应,形成多层位的层控铜矿床,东川铜矿带成矿机制为盆地卤水交代成矿。 展开更多
关键词 东川铜矿 碳同位素 氧同位素 有机质 成矿机制
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昆明东川区坪子地泥石流形成机制及动力学特征
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作者 崔文华 赵蓓蕾 《云南地质》 2023年第1期95-100,共6页
本文以昆明东川江西村坪子地泥石流为研究对象,在调查泥石流“地貌条件、物源条件、水文条件”的基础上,通过雨洪法、形态调查法、一次性泥石流总量计算法等多种手段,对泥石流形成条件,发育特征,形成规模等多方面调查分析并进行计算,对... 本文以昆明东川江西村坪子地泥石流为研究对象,在调查泥石流“地貌条件、物源条件、水文条件”的基础上,通过雨洪法、形态调查法、一次性泥石流总量计算法等多种手段,对泥石流形成条件,发育特征,形成规模等多方面调查分析并进行计算,对其形成机制和动力学特征进行分析,明确泥石流的形成机理、发育规模等,得出坪子地泥石流沟属于暴雨性、混合沟谷、高频、小型泥石型粘性泥石流。 展开更多
关键词 泥石流 形成机制 动力学特征 坪子地泥石流 昆明东川江西村 云南
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云南东川地区汤丹铜矿床成矿规律及对因民铜矿区的找矿启示
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作者 熊林根 罗伟 《世界有色金属》 2023年第3期58-60,共3页
随着我国经济快速发展,对各种矿产资源的需求不断增加,对铜矿勘探提出了更高的要求。根据对东川汤丹铜矿成因规律的研究,我们以因民煤矿为例开展了多层位找矿研究。据相关调查结果显示,落雪组二段青灰色白云岩和黑山组碳质板岩都出现了... 随着我国经济快速发展,对各种矿产资源的需求不断增加,对铜矿勘探提出了更高的要求。根据对东川汤丹铜矿成因规律的研究,我们以因民煤矿为例开展了多层位找矿研究。据相关调查结果显示,落雪组二段青灰色白云岩和黑山组碳质板岩都出现了不同程度的铜矿化现象,部分原生晕样品含有较高铜质量分数。可以看出,东川式层控脉状铜矿体和桃园式铜矿体的找矿潜力很大。 展开更多
关键词 云南东川地区 成矿规律 因民铜矿
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云南东川铜矿区古元古代辉绿岩地球化学——Columbia超级大陆裂解在扬子陆块西南缘的响应 被引量:36
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作者 王生伟 廖震文 +6 位作者 孙晓明 蒋小芳 周邦国 郭阳 罗茂金 朱华平 马东 《地质学报》 EI CAS CSCD 北大核心 2013年第12期1834-1852,共19页
近年研究显示,古元古代晚期,扬子陆块西南缘发生了大规模的地幔物质上涌事件。本文系统报道了康滇地区中部东川铜矿因民一落雪矿区古元古代辉绿岩的地球化学特征。主量元素中MgO含量较高,为6.16%~9.65%,Mg2+平均为72.2;富N... 近年研究显示,古元古代晚期,扬子陆块西南缘发生了大规模的地幔物质上涌事件。本文系统报道了康滇地区中部东川铜矿因民一落雪矿区古元古代辉绿岩的地球化学特征。主量元素中MgO含量较高,为6.16%~9.65%,Mg2+平均为72.2;富Na20,Na20/K20为1.3~9.8;低Si02,45.61%~49.34%;低TiOz,0.74%~2.74%;FeO/MgO小于1,表明本区辉绿岩初始岩浆相对较原始,MgO与主要组分的相关性表明岩浆早期出现过轻微的橄榄石、斜方辉石及铬铁矿、钛铁矿结晶分异。(La/Yb)。为1.66~4.37,8Eu为1.04~1.22,稀土元素球粒陨石的配分呈平缓右倾模式,出现Eu的弱正异常。富集Rb、Ba等大离子半径元素,MORB配分为向右陡倾模式,出现突出的Rb、Ba峰,Zr、Hf弱负异常,多数样品没有明显的Nb、Ta异常。eNd,为一0.2~3.8,初始87Sr/86Sr。值为0.7055-0.7084。东川地区辉绿岩的源区为尖晶石二辉橄榄岩相,为较亏损的过渡型地幔部分熔融的产物,轻度混染主要源于陆下岩石圈地幔及少量的下地壳物质。东川古元古代辉绿岩地球化学表现为明显的板内玄武岩、E—MORB和0IB的特征,表明古元古代末期,扬子陆块西南缘发生了大规模的陆内裂谷拉张事件,与全球性Columbia超级大陆裂解同步,可能与地幔柱活动密切相关。 展开更多
关键词 辉绿岩 东川铜矿 昆阳裂谷 东川群 汤丹群 Columbia超级大陆 地幔柱 东川
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云南东川望厂组熔结凝灰岩锆石SHRIMP U-Pb年龄及其意义 被引量:44
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作者 周邦国 王生伟 +9 位作者 孙晓明 廖震文 郭阳 蒋小芳 朱华平 罗茂金 刘才泽 马东 沈战武 张海 《地质论评》 CAS CSCD 北大核心 2012年第2期359-368,共10页
本文报道了云南东川地区望厂组中熔结凝灰岩锆石的SHRIMP U-Pb年龄。其中自形结构、环带清晰锆石的不一致曲线与谐和线上交点的207Pb/206Pb年龄分别为2317±13Ma(n=13,MSWD=3.3),13个点的加权平均年龄为2299±14Ma(n=13,MSWD=5.... 本文报道了云南东川地区望厂组中熔结凝灰岩锆石的SHRIMP U-Pb年龄。其中自形结构、环带清晰锆石的不一致曲线与谐和线上交点的207Pb/206Pb年龄分别为2317±13Ma(n=13,MSWD=3.3),13个点的加权平均年龄为2299±14Ma(n=13,MSWD=5.9),表明望厂组地层的沉积时代为古元古代早—中期。东川地区下四组地层与滇中昆阳群(黄草岭组—美党组)和四川会理群(淌塘组—天宝山组)的沉积时代相差近1.0Ga。为了区别于昆阳群和会理群,建议对本区下四组地层(洒海沟组、望厂组、菜园湾组、平顶山组)独立建群,即汤丹群。汤丹群是目前为止康滇地区已发现的最古老的地层建造之一,经历过古元古代中期的挤压过程(东川运动)和古元古代末期的拉张过程,可能是相对于扬子古陆核独立存在、并构成早—中元古宙Columbia超级大陆的一个小的古老陆块。 展开更多
关键词 SHRIMP U-PB测年 熔结凝灰岩 汤丹群 东川群 东川铜矿 Columbia超大陆
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云南东川地区昆阳群黑山组凝灰岩锆石SHRIMP U-Pb年龄及其地层学意义 被引量:102
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作者 孙志明 尹福光 +4 位作者 关俊雷 刘建辉 李军敏 耿全如 王立全 《地质通报》 CAS CSCD 北大核心 2009年第7期896-900,共5页
云南东川地区昆阳群的形成时代及地层层序一直令人关注,已获得的一些数据虽然具有参考意义,但高质量的SHRIMP定年还很缺乏。在东川地区昆阳群黑山组中上段发育的近180m厚的具有地层意义的晶屑、岩屑凝灰岩中采集样品D0202一件,选出锆石... 云南东川地区昆阳群的形成时代及地层层序一直令人关注,已获得的一些数据虽然具有参考意义,但高质量的SHRIMP定年还很缺乏。在东川地区昆阳群黑山组中上段发育的近180m厚的具有地层意义的晶屑、岩屑凝灰岩中采集样品D0202一件,选出锆石百余粒,获得SHRIMP U-Pb加权平均年龄为(1503±17)Ma。样品D0202的锆石Th/U大于0.48,并具清晰的振荡环带结构,均为岩浆成因的锆石,表明黑山组形成于中元古代早期。这一年龄表明昆阳群的形成时代至少大于1500Ma,为准确地标定昆阳群的时代和层序提供了新的参考依据。 展开更多
关键词 云南东川地区 昆阳群 锆石SHRIMP U-PB年龄 中元古代
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康滇地区元古宙构造运动Ⅰ:昆阳陆内裂谷、地幔柱及其成矿作用 被引量:26
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作者 王生伟 蒋小芳 +6 位作者 杨波 孙晓明 廖震文 周清 郭阳 王子正 杨斌 《地质论评》 CAS CSCD 北大核心 2016年第6期1353-1377,共25页
康滇地区是我国南方元古宙基底出露最为广泛的地区,元古宙岩浆活动频繁、成矿作用明显,是研究扬子陆块早期演化的重要窗口,也是近年研究的热点,元古宙地质演化过程争议较大。本文系统总结了发生在古元古代晚期—中元古代早期的重要构造... 康滇地区是我国南方元古宙基底出露最为广泛的地区,元古宙岩浆活动频繁、成矿作用明显,是研究扬子陆块早期演化的重要窗口,也是近年研究的热点,元古宙地质演化过程争议较大。本文系统总结了发生在古元古代晚期—中元古代早期的重要构造—岩浆—成矿事件,即昆阳裂谷。昆阳裂谷前的基底为分布在东川和滇中地区少量的古元古代早期的汤丹群,其构造变形较东川群更强烈,可能与>1800 Ma的东川运动有关。昆阳裂谷期的岩浆岩系统主体为出露在东川—会理—滇中地区基性侵入岩,其次为少量的超基性岩、变质基性火山岩和中酸性侵入岩体,具有双峰式岩浆岩组合的特征。岩浆岩的年龄为1800 Ma^1450 Ma,集中分布在1750Ma^1650 Ma,反映了昆阳裂谷持续了约400 Ma,高峰期持续将近100 Ma。昆阳裂谷期基性岩浆岩的地球化学显示为典型陆内裂谷玄武岩的地球化学性质,其中滇中武定地区辉绿岩和会理拉拉地区的变质基性火山岩还具有典型洋岛玄武岩的特征,如富碱、高TiO_2、P_2O_5、低CaO/TiO_2、Al_2O_3/TiO_2比值,Nb、Ta、Zr、Hf等高场强元素不亏损,以及有较高的[n(^(87)Sr)/n(^(86)Sr)]_i初始比值以及较高的ε_(Nd)(t)值。根据区内岩浆岩组合及地球化学特征,我们提出在古元古代晚期至中元古代早期,康滇地区发生了一次由地幔柱活动引起的陆内裂谷拉张事件,即昆阳地幔柱。昆阳陆内裂谷在1450 Ma前后在会理—东川一线发展成为了局限小洋盆,并在中元古代晚期关闭。昆阳裂谷的沉积岩系统主体为东川群、河口群和大红山群,并可能延伸到了康滇北部的里伍岩群,上述地层中火山岩、凝灰岩锆石的U-Pb年龄集中在1800Ma^1500 Ma,不同岩群岩性组合差异可能与所处构造部位有关,并导致沉积相的差异。昆阳裂谷也是一次重要的成矿事件,其形成的矿床可分为两个系列,以因民组、落雪组等沉积岩中为主的层状铜矿床(Sediment-hosted Stratiform Copper,SSC系列),主要有汤丹铜矿、落雪铜矿、狮子山铜矿、铜厂铜矿等,原生沉积型铜矿的成矿时代为约1750 Ma;其次为与昆阳裂谷期岩浆热液活动紧密相关的铁氧化物铜金矿床(Iron—Oxide—Copper—Gold,IOCG系列),主要有拉拉铁铜矿床、大红山铁铜矿床、稀矿山铁铜矿床、迤纳厂铁铜矿床等,研究程度较高的迤纳厂、稀矿山以及鹅头厂等铁铜矿床的时代集中在1700 Ma^1450 Ma。昆阳期剧烈的岩浆活动、大规模的铁、铜成矿作用以及成矿物质来源、动力学机制可能均与昆阳地幔柱活动紧密相关。 展开更多
关键词 昆阳裂谷 昆阳地幔柱 东川群 河口群 大红山群 东川式铜矿 IOCG矿床 康滇地轴
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