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It has long been debated that the Dabie orogenic belt belongs to the North China or Yangtze craton. In recent years, eastern
China has been suggested, based on the Pb isotopic compositions of Phanerozoic ore and Mesozoic granitoid K-feldspar (revealing
the crust Pb) in combination with Meso-Cenozoic basalts (revealing the mantle Pb), being divided into the North China and
Yangtze Pb isotopic provinces, where the crust and mantle of the Yangtze craton are characterized by more radiogenic Pb. In
this sense, previous researchers suggested that the pro-EW-trending Dabie crogenic belt with less radiogenic Pb in the crust
was part of the North China craton. In this paper, however, the Late Cretaceous basalts in the central and southern parts
of the Dabie orogenic belt are characterized by some more radiogenic Pb (206Pb/204Pb=17.936−18.349,207Pb/204Pb=15.500−15.688,208Pb/204Pb=38.399−38.775) and a unique U-Th-Pb trace element system similar to those of the Yangtze craton, showing that the Mesozoic
mantle is of the Yangtze type. In addition, the decoupled Pb isotopic compositions between crust and mantle were considerably
derived from their rheological inhomogeneity, implying a complicated evolution of the Dabie orogenic belt.
The study was funded by the National Natural Science Foundation of China (No. 49794043) and the Open Laboratory of Constitution,
Interaction and Dynamics of the Crust-Mantle System, China. 相似文献
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Jean S. Kane 《Geostandards and Geoanalytical Research》2002,26(1):7-29
As in all fields of sample analysis, reference materials play a large role in supporting measurements in the geosciences. While a rather large number of materials are in distribution (> 380), not all are equally effective or fit-for-purpose in supporting laboratory data quality and thereby assuring the desired comparability of measurements between laboratories. Equally important, reference values that are not fit-for-purpose cannot be used effectively to establish traceability links between laboratory measurements and national and international standards. The needed fitness-for-purpose is not achieved for reference values either when more than one reference value has been proposed and a consensus does not exist among users as to which should be used by all, or when reference value uncertainties are too large in comparison to those of routine laboratory measurements. The focus of this review will be, first to outline the current reality, and second to suggest ways in which certifications of RMs can be improved to provide reference values that are universally accepted and more fit-for-purpose in general laboratory use. The discussion will be illustrated largely by current uses of USGS BCR-1, NIST SRM 610 and IAEA NBS28, as these three materials are those for which the largest body of newly published data exists, according to recent bibliographies of the geoanalytical literature published annually in Geostandards Newsletter: The Journal of Geostandards and Geoanalysis. 相似文献
106.
双台河口自然保护区濒海湿地景观变化及其管理对策研究 总被引:13,自引:5,他引:13
从国内外湿地研究进展看,濒海湿地景观变化及其管理对策研究得到人们越来越广泛的重视。以辽宁双台河自然保护区为研究区域,利用1994和1997年两期TM数据进行GIS数据处理,通过各种类型的湿地景观在该时段的面积变化得到保护区濒海湿地景观的动态变化特征,并在变化原因分析的基础上提出了一些相应的保护区管理对策,以便更好地为湿地保护和管理提供决策依据。 相似文献
107.
坝上高原安固里淖粒度年纹层与环境变化 总被引:9,自引:2,他引:9
在安固里淖湖心区获取一未扰动沉积物样柱,分析发现了由冬季风搬运物与湖心沉积共同形成的粒度年纹层,建立了纹层年表,恢复了安固里淖湖区8507aB.P,以来的环境变化过程。8507-5429aB.P。冬季风活动较弱,后期的所波动;5429-3244aB.P.冬季风活动较强,3244-2494aB.P。冬季风活动减弱;2494-1165aB.P。冬季风活动略有增强;1165aB.P以来,冬季风活动减弱。安固里小淖粒度年纹层反映的冬季风变化情况与我国北方地区同期的环境变化和海平面变化有很好的对应关系。 相似文献
108.
Soil erosion assessment and prediction play critical roles in addressing problems associated with erosion control or soil conservation. The past dynamics of soil erosion can provide valuable information for us to understand the relations of soil erosion to environmental change and anthropogenic activity. The present paper has compared Holocene climatic changes in northwestern China with those in southern Norway, and investigated the past dynamics of erosion activity during the Holocene. Modern soil erosion on the Loess Plateau is a combination of the intensive natural erosion and human-induced erosion, the latter being four times greater than the former. Because of global warming and increasing human activities, climate on the Loess Plateau is becoming dryer and more unstable, causing an enhanced erosion problem and water scarcity. In the arctic-alpine region of southern Norway, however, the global warming and regional wetting caused expansion of the largest European ice cap. This has accentuated the erosion in that region, with a higher frequency of avalanches and debris flows. 相似文献
109.
以位于内蒙古鄂尔多斯高原上的伊金霍洛旗为研究区域,以景观生态学的数量分析方法为基本手段,在土地利用现状分类体系下,以其1984、1991和1998年3个年度的土地利用图为基础。从区域和斑块类型两个尺度上,对其景观格局进行了数量分析。结果表明,在三个典型年度。天然草地为伊金霍洛旗的景观基质,景观格局指数的所有变化均是在此基础上发生和演变的。从整个景观尺度的格局指数变化情况显示,伊金霍洛旗景观的破碎化程度在增加;同时景观的异质性程度在下降,景观愈来愈有少数景观斑块类型所控制。而在斑块类型这一尺度上的格局指数变化说明,不同类型斑块的复杂性的变化趋势基本相同,即均有不同程度的增长,但增加幅度有限;同时还说明,不同类型斑块内部其大小差异的幅度在不断缩小。但从不同年度的变化情况来看,无论是区域还是不同的斑块类型,其格局指数的变化并不与总体的变化趋势同步。 相似文献
110.
The River Ganga in the central Gangetic plain shows the incision of 20 m of Late Quaternary sediments that form a vast upland terrace (T2). The incised Ganga River Valley shows two terraces, namely the river valley (terrace-T1) and the present-day flood plain (terrace-T0). Terrace-T1 shows the presence of meander scars, oxbow lakes, scroll plains, which suggests that a meandering river system prevailed in the past. The present-day river channel flows on terrace-T0 and is braided, sensu stricto. It is thus inferred that the River Ganga experienced at least two phases of tectonic adjustments: (1) incision and (2) channel metamorphosis from meandering to braided.Optical dating of samples from three different terraces has bracketed the phase of incision to be <6 and 4 ka. Different ages of the top of terrace-T2 show that this surface experienced differential erosion due to tectonic upwarping in the region, which also caused the river incision. River metamorphosis occurred some time during 4 and 0.5 ka. 相似文献