甘肃省岷县马坞金矿地质特征及找矿方向     

崔龙  刘满年 《陕西地质》2010,28(1):39-45

马坞金矿分布于岷-礼成矿带的东部,矿体产于中泥盆统浅变质碎屑岩中,受断裂破碎蚀变带的控制。围岩蚀变以中-低温热液蚀变为主,蚀变强度与金矿化强度呈正相关;矿区共圈定6条矿脉,沿走向及倾向具有尖灭再现、局部膨大缩小的特点,沿裂隙发育的矿脉金品位较高。  相似文献   

沂源县加强矿政管理的几点思考     

李成彬  崔光峰  单吉成 《山东地质》2010,(5):60-62

矿业权制度改革是一项全新的事物,改革的关键是变无序为有序、无偿为有偿。近几年来,沂源县积极推进矿业权制度改革,盘活矿业权市场,取得明显成效,该文对沂源县采取的措施和效果及工作中的体会做了详细阐述。  相似文献   

An assessment of acid rock drainage continuous monitoring technology     

K. Fytas  J. Hadjigeorgiou 《Environmental Geology》1995,25(1):36-42

In order to assess the magnitude and impact at affected mine sites of acid rock drainage (ARD), fixed-frequency sampling is often employed. This often involves manual sampling, at regular time intervals, of water and solids. It is felt that such sampling does not adequately describe the system evolution. Continuous monitoring offers a viable alternative in that it can better follow the seasonal fluctuations and high-frequency variations that characterize ARD. This paper evaluates existing continuous monitoring technology.  相似文献   

沉积环境对煤系岩石强度的影响     

葛道凯  杨起 《煤田地质与勘探》1993,21(1):5-11

分析了平顶山矿区煤系中形成于不同沉积环境的64组岩石样品的沉积特征和强度,结果表明,岩体的强度与沉积环境有着密切的成因联系。岩体强度的变化主要受控于岩性、沉积环境中能量的高低、水动力条件的变化幅度和生物发育程度4项因素。  相似文献   

Groundwater mining of bedrock aquifers in the Denver Basin – past,present, and future     

J.?E.?MooreEmail author  R.?G.?Raynolds  P.?E.?Barkmann 《Environmental Geology》2004,47(1):63-68

The Denver Basin bedrock aquifer system is an important source of water for municipal and agricultural uses in the Denver and Colorado Springs metropolitan areas. The Denver area is one of the fastest growing areas in the United States with a population of 1.2 million in 1960 that has increased to over 2.4 million by 2000. This rapid population growth has produced a corresponding increase in demand for potable water. Historically, the Denver area has relied on surface water, however, in the past 10 years new housing and recreation developments have begun to rely on groundwater from the bedrock aquifers as the surface water is fully appropriated and in short supply.The Denver Basin bedrock aquifer system consists of Tertiary and Cretaceous age sedimentary rocks known as the Dawson, Denver, Arapahoe and Laramie-Fox Hills Aquifers. The number of bedrock wells has increased from 12,000 in 1985 to 33,700 in 2001 and the withdrawal of groundwater has caused water level declines of 76 m. Water level declines for the past 10 years have ranged from 3 to 12 m per year. The groundwater supplies were once thought to last 100 years but there is concern that the groundwater supplies may be essentially depleted in 10 to 15 years in areas on the west side of the basin.Extensive development of the aquifer system has occurred in the last 25 years especially near the center of the basin in Douglas and El Paso Counties where rapid urban growth continues and surface water is lacking. Groundwater is being mined from the aquifer system because the discharge by wells exceeds the rate of recharge. Concern is mounting that increased groundwater withdrawal will cause water level declines, increased costs to withdraw groundwater, reduced well yield, and reduced groundwater storage. As the long-term sustainability of the groundwater resource is in doubt, water managers believe that the life of the Denver Basin aquifers can be extended with artificial recharge, water reuse, restrictions on lawn watering, well permit restrictions and conservation measures.  相似文献   

加卸载响应比理论用于矿震预测的初步研究   总被引：4，自引：0，他引：4  

尹祥础  尹迅飞  余怀忠  张晖辉  颜玉定 《地震》2004,24(2):25-30

加卸载响应比(LURR)理论是一种前景很好的中期地震预测方法,通常在强烈地震发生前的数月至1～2年LURR出现高值,因而LURR可以作为强烈天然地震的前兆,用此方法曾经成功地预测过Northridge地震(1994年1月17日,M6.7,美国加州),Kanto地震(1996年9月11日,M6.6,日本)及不少发生在中国的天然地震。用房山煤矿1992年8月至1993年7月的微震资料,计算了全年内7组M>2.1矿震前的加卸载响应比Y值,其中5组矿震前Y值均明显大于1(Y≥2.9)。以上结果表明,加卸载响应比理论有可能用于矿震的预测。  相似文献   

完善我国矿业立法应突出解决的几个问题     

曹爱民 《江苏地质》2006,30(2):148-152

从中外矿业立法史的回顾入手,借鉴中外矿业立法经验,指出我国现行矿业立法的不足之处,进而提出了继承我国矿业立法成果的、与国际接轨的、适合我国国情的矿业权运作与管理的立法框架。就矿业权性质、与土地使用权的协调、矿业管理规范的完善进行了论述。  相似文献   

Metal contamination of the environment by placer and primary gold mining in the Adola region of southern Ethiopia   总被引：3，自引：0，他引：3  

Worash Getaneh  Tamiru Alemayehu 《Environmental Geology》2006,50(3):339-352

Primary and placer gold mining sites in southern Ethiopia were studied to see the contribution of mining to the accumulation of metals in different environmental media. Sediment, water and plant samples were analyzed for Al, Mn, Fe, As, Ni, Cr, Cu, Co, Pb, W, Sb, Mo, Zn and V. Water parameters (pH, Eh, TDS, anions and cations) were also measured. The sediment analyses results show that the most abundant metals are Ni (average 224.7 mg/kg), Cr (199 mg/kg), Cu (174.2 mg/kg), V (167.3 mg/kg), Zn (105.5 mg/kg), Pb (61.5 mg/kg) and As (59.7 mg/kg) in the primary gold mining sites while the placer sites show high concentration of V (average 301.2 mg/kg), Cr (260.4 mg/kg), Zn (179 mg/kg), Ni (113.4 mg/kg), Cu (46.7 mg/kg), As (32.2 mg/kg) and Co (31 mg/kg). The metals Cu, Ni, W, Cr, As and Pb in primary and Sb, W, Cr, Ni, Zn, As and Mo in placer gold mining sites have geoaccumulation indexes (I _geo) from one to four indicating considerable accumulation of these metals. Waters from both primary and placer mining sites are near neutral to alkaline. Arsenic (average 92.8 μg/l), Ni (276.6 μg/l), Pb (18.7 μg/l), Sb (10.7 μg/l), Mn (1 mg/l), Fe (8.3 mg/l) and Al (23.8 mg/l) exceeded the guideline value for drinking water. Plants show high concentration of Cr (average 174.5 mg/kg), Ni (163.5 mg/kg), Zn (96 mg/kg) and W (48 mg/kg). Zinc, W, Mo, Ni and Cr show the maximum biological absorption coefficient (BAC) ranging 0.4–1.7, 0.1–104.6, 1.1–2.6, 0.2–1.6 and 0.2–3.6, respectively, and the results suggest bioaccumulation of these elements in plants. The minerals especially sulfides in the ore aggregate are the ultimate source of the metals. The release of the metals into the environmental media is facilitated (in addition to normal geologic processes) by human activities related to gold mining.  相似文献   

长江三峡工程周边地区的采矿诱发地震   总被引：8，自引：2，他引：6       下载免费PDF全文

胡毓良  杨清源 《地震地质》1998,20(4):62-360

地震观测和实地调查表明,长江三峡工程周缘广泛存在采矿诱发地震。采矿诱发地震主要是由于矿山采空区的出现使浅部地壳差应力增大岩体失稳而产生的,它们不同于天然地震。水库蓄水前应对这些地震的背景进行详细研究。在进行区域地震震情分析和预报、区域应力场及活动断裂研究时应严格加以区别  相似文献   

神府东胜矿区煤中微量元素初步研究   总被引：11，自引：2，他引：9  

窦廷焕  肖达先 《煤田地质与勘探》1998,26(3):11-15

采用神府东胜矿区廷安组５个可采煤层７３２个煤心煤样,应用光谱、原子荧光、原子吸收等分析方法,测定了煤中２３种微量元素。阐述了微量元素在煤中的含量分布和微量元素相对于地壳丰的富集系数,并对有害元素有用元素进行了初步评价。  相似文献