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In order to discuss the source of ore-forming materials of the Bingdongshan lead-zinc deposit, Rb-Sr isotopes of the main ore-stage sphalerites have been analyzed by using the full dissolution method and fluid inclusions leaching method in this paper, with yielded isochion ages of 507. 7-507. 8 Ma, initial 87Sr/86Sr values of 0. 709193-0. 709220.These isoch-ron ages, representing the age of the main mineralization stage of the deposit, indicate that the deposit was formed in Early Ordovician, or the mineralization occurred in the middle Caledonian. The characteristics of initial strontium isotopic ratios of sphaleritess how that the ore-forming materials or the ore-forming fluid were provided by both of basement rocks and the Sinian carbonates. Combining with geological characteristics of the deposit and regional Pb-Zn metallogenic geological background, it is believed that the Caledonian tectonic movement played important role for the formation of lead-zinc deposits in the northern margin of the Yangtze Block. The Bingdongshan lead-zinc deposit was probably formed under the Caledonian extensional environment, through the precipitation of sulfides, in certain physic-chemical condition, from the ore-forming hydrothermal fluids which were associated with dome structure activities.  相似文献   
996.
Rapid, high-throughput and reliable methods are urgently required to accurately detect and monitor harmful algae, which are responsible for algal blooms, such as red and green tides. In this study, we successfully developed a multiplex PCR-based DNA microarray method capable of detecting nine harmful algal species simultaneously, namely Alexandrium tamarense, Gyrodinium instriatum, Heterosigma akashiwo, Karenia mikimotoi, Prorocentrum donghaiense, Prorocentrum minimum, Ulva compressa, Ulva ohnoi and Ulva prolifera. This method achieved a limit of detection (LOD) of 0.5 ng of genomic DNA (orders of magnitude of the deci-nanogram range) in the tested algae cultures. Altogether, 230 field samples from ship ballast waters and seaport waters were used to evaluate the DNA microarray. The clinical sensitivity and specificity of the DNA microarray assay in detecting field samples were 96.4% and 90.9%, respectively, relative to conventional morphological methods. This indicated that this high-throughput, automatic, and specific method is well suited for the detection of algae in water samples.  相似文献   
997.
Silver carp (Hypophthalmichthys molitrix), bighead carp (Aristichthys nobilis), grass carp (Ctenopharyngodon idella), and black carp (Mylopharyngodon piceus) are the four major Chinese carps and are commercially important aquaculture species in China. Reproduction of these carp has declined since the construction of the Three Gorges Dam (TGD) due to an altered water flow and thermal regime in the Changjiang (Yangtze) River. However, details of the changes in reproduction of the four species are not well understood. To assess the impact of the TGD on reproduction of the four carp, we investigated their eggs and larvae at Yidu City, which is 80 km below the TGD, during 2005–2012. We examined diff erences in larval abundance of the four species in the Jianli section (350 km downstream of the TGD) before (1997–2002) and after (2003–2012) construction of the TGD. Based on these observations, the first spawning date of the four species was delayed a mean of about 25 days after the dam was constructed. Mean egg abundance in the Yidu section of the river was 249 million and mean larval abundance was 464 million, which were significant decreases since the 1980s. Moreover, larval abundance in the Jianli section after the dam was constructed was significantly lower than that before construction (ANCOVA, P<0.05). The observed larval abundance accounted for only 24.66% of the predicted value in 2003 when the dam was first inundated. The present spawning grounds between the TGD and Yidu section of the river are very similar to those described in the 1980s, and some spawning grounds exist upstream of the TGD. Large free-flowing stretches upstream of the TGD and the creation of artificially flooded downstream reaches are needed to stimulate spawning and eff ectively conserve these four major Chinese carps species.  相似文献   
998.
C.Z. Yan  X. Song  Y.M. Zhou  H.C. Duan  S. Li 《Geomorphology》2009,112(3-4):205-211
Global climate change will affect the ecology and environment of the Qinghai–Tibet Plateau, thus increasing attention is being paid to the aeolian desertification that is occurring in the watershed that supplies the Longyangxia Reservoir in the upper reaches of China's Yellow River. We must assess the aeolian desertification trends before developing a plan to restore the region's degraded eco-environment. In this study, land suffered from aeolian desertification was classified into four levels (slight, moderate, severe, and extremely severe) using a series of indices. Interpretation of Landsat MSS and TM data from 1975's, 1989's, and 2005's was used to establish databases of aeolian desertified land at these three times. We then derived the aeolian desertification trends during the study period by overlaying the consecutive databases, and we analyzed the driving factors responsible for the observed aeolian desertification. The results show a total of 1,721,478.02 ha of aeolian desertified land in 2005's, accounting for 13% of the region's total area. From 1975's to 1989's, the area of aeolian desertified land increased by 229,307.26 ha, which represents a 15% increase compared to the 1975's area; and from 1989's to 2005's, the area of aeolian desertified land decreased by 19,079.87 ha, which represents a 1% decrease compared to the 1989's area. The main driving factors responsible for this increased aeolian desertification were climate factors (high wind velocity and an increase in annual temperature, combined with low precipitation and high evaporation) as well as unsustainable human activities and inappropriate policy measures. A series of key national projects initiated to combat degradation of the study area's eco-environment led to a decrease of aeolian desertified land through obvious restoration of vegetation.  相似文献   
999.
2006年7月22日09时10分21.6秒,云南省昭通市盐津县境内(28°01′N,104°08′E)发生Ms5.1地震,震源深度9km.极震区烈度为Ⅵ度,个别Ⅶ破坏点,等震线形状呈椭圆形,长轴走向北东向.地震造成22人死亡,13人重伤,35428户、151168人受灾.2006年8月25日13时51分41.1秒,盐津县(28°03′N,104°07′E)再次发生5.1级地震,震源深度7km,较7月22日地震略浅.微观震中由722地震位置向西北偏移约4km.由于震中位置基本相同,故地震灾害相互叠加,出现灾害加重现象和灾情范围扩大趋势,地震造成2人死亡,重伤7人,1万多户、4.5万多人需要紧急转移安置,房屋倒塌1500多间,其中170所学校的校舍不同程度受损.  相似文献   
1000.
At present, as the easily mining resources are being increasingly depleted, the exploitation of coal under buildings, water-bodies and railways is imminent for the sustainable production. Probability in-tegral method is a general method for mining subsidence in the coal system. Because of poor under-standing of mining subsidence for other sections, the authors suggest probability integral method for the study of coal mining under buildings, water-bodies and railways. Moreover, the calculation result of probability integral method should be corrected by numerical simulation method. Based on practical projects, the impact has been evaluated on the security of Xifeihe left embankment under coal mining. Combining with the results of probability integral method, we propose that the 600 m far from em-bankment is a good rationality. This article provides the basis for the rational exploitation of coal re-source which is a major practical problem under the premise of Water Infrastructure Security. Fur-thermore, it also can be served as a reference for the similar projects, such as mining Xiaolangdi res-ervoir area, mining Yuecheng reservoir and mining the major channels of Middle Route South to North Water Transfer.  相似文献   
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