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991.
正In recent years,lakes,including salted,attract the attention of researchers,also when reconstructing last climate changes using the bottom sediments(Solotchina et al.,2008,et al.).In this case the different geochemical 相似文献
992.
<正>稀土(Rare earth elements)在现代科技领域占有举足轻重的地位,是现代工业的"维生素"。我国稀土储量占世界第一,位于内蒙古自治区包头市北部的白云鄂博矿床是世界上最大的稀土矿床,其稀土氧化物储量为4800万吨,于1927年被丁道衡教授发现。至今,国内外地质学家对该矿床作了大量的研究工作,但是其成因长期仍存在很大争议,制约了相关矿床的找矿工作。争论的焦点是该矿床同时具有火成碳酸岩的地球化学特征和典型的沉积特征,并有明显的交代作用的特点。作者在白云鄂博矿床开展了长期深入的研究,积累了丰富的标本 相似文献
993.
Abstract: The Lower Cambrian Nagaur Sandstone (Marwar Supergroup) has yielded trace fossils Treptichnus, Cruziana, serially repeated Rusophycus, Diplichnites, Monomorphichnus, Bergaueria, arthropod swimming traces and leap frogging marks of Cruziana ichnofacies. This ichnofossils assemblage is dominantly preserved in fine to medium grained red sandstone beds of the Mohra Member (Nagaur Sandstone). The presence of graded rip-up clasts, current ripples, dune cross-stratification with mud drapes and tidal bundles indicates a subtidal paleoenvironment for the deposition of Nagaur Sandstone Formation, which is corroborated by the Cruziana ichnofacies trace fossil assemblage. 相似文献
994.
The influence of the Po River discharge on phytoplankton bloom dynamics along the coastline of Pesaro (Italy) in the Adriatic Sea 总被引:1,自引:0,他引:1
In recent years, eutrophic phenomena have frequently been reported in the Italian coastal waters of the northern Adriatic Sea. The aim of the present study was to determine that the phytoplankton blooms occurring along the Italian coastline in the area of Pesaro are caused by the Po River waters. In fact between October and December 2000 the nutrient load flushed into the sea from local rivers is not significant (phosphorus 10 tons and nitrogen 110 tons), instead N and P load from the Po River are: 650 and 8969 tons. The bloom episodes occurred during this period, at which time hypoxia developed on the sea bottom. The phytoplankton cell concentrations were 40.0 x 10(6) cells L(-1), and a significant presence of diatoms was observed. This issue is important in analysing the anthropogenic disturbances and environmental changes. The eutrophic seawater conditions were also analysed using the eutrophic index. 相似文献
995.
Blubber samples of Baikal seals pups (Phoca sibirica) collected in 2001 and 2002 were analyzed for persistent organochlorines (OCs) such as PCBs (polychlorinated biphenyls), DDTs (dichlorodiphenyltrichloroethane and its metabolites), HCHs (hexachlorocyclohexane isomers), CHLs (chlordane related compounds), TCPMe [tris(4-chlorophenyl)methane] and TCPMOH [tris(4-chlorophenyl)methanol]. The distribution pattern of OCs was in the following order: DDTs>PCBs>CHLs>HCHs>TCPMOH>TCPMe. Organochlorine concentrations and composition patterns in eight pup blubber samples (2002) analyzed in the present study were compared with the corresponding levels in juvenile Baikal seals from 1992 survey, and it was found that residue levels of OC compounds have declined during the 10 year period. In particular, concentrations of PCBs, HCHs and CHLs in seals collected in 2002 were approximately two times lower, while DDTs levels were three times lower than the corresponding levels in 1992. Furthermore, higher ratios of beta-HCH/HCHs and p,p(')-DDE/DDTs were found in 2002 samples. While comparing the OC levels with those in other seal pups it appeared that all the OC concentrations were lower than the levels in seals from coastal California known as one of the most polluted areas. PCB and DDT concentrations in the present specimens were higher than that in Arctic seal pups. The proportions of tri-, tetra-, penta- and hexachlorobiphenyls in pups captured in 2002 were higher than those in 1992. TEQ concentrations of non- and mono-ortho coplanar PCBs in Baikal seals collected in 2002 were higher than those in seals collected from some locations in the world, where human and industrial activities are extensive, suggesting potential for toxic implications of coplanar PCBs in Baikal seals. 相似文献
996.
997.
本文利用同步辐射X射线对一沁水盆地无烟煤样在24 keV的能量下进行了成像,并重构得到其CT切片。分别采用数字地形模型(DTM)和数据约束模型(DCM)对样品的CT切片进行分析。研究结果表明,对本文所用煤样,DTM计算得到的煤样孔隙率与真密度和视相对密度实验法测得孔隙率较为接近,但利用DTM确定的阈值进行阈值分割提取到的样品孔隙率与DTM计算所得孔隙率之间偏差较大。DCM计算得到的孔隙率与DTM计算得到的孔隙率及实验测试结果均较为接近。DCM模型考虑了样品CT成像过程中的部分体积效应,得到小于CT体元的孔隙分布信息,在一定程度上拓展了CT成像技术的表征尺度。DCM计算结果显示,煤样中孔隙更多与煤基质和矿物组分以部分占据CT体元的形式存在。 相似文献
998.
使用2002年M7.9阿拉斯加迪纳利断层地震(DFE)周围的地震形变和无震形变的观测资料,检验了余滑应该伴有颤动的假设。余滑比自发慢滑动发生得更频繁,而且已在更广泛的构造环境中观测到了。因此,伴随余滑的颤动存在与否能提供有关颤动生成的新线索。我们还搜寻了前兆颤动,即假定加速滑动导致破裂的证据。我们的搜寻在迪纳利断层地震前5天及其后3个月内的几个时段均未得到颤动。这种否定结果和一系列其他观测结果,或许都可用破裂穿透到假定的闭锁区以下到达摩擦过渡区内来解释。尽管并非独一无二,但这种解释确证了先前巨大逆冲断层和转换断层地震破裂完全延展到过渡区的模型。 相似文献
999.
1000.
The Cimmerian terrane forms an almost unbroken chain stretching >13,500 km, from central southern Europe to western Indonesia, via SE Europe, the Middle East, Afghanistan, Tibet, SW China and Myanmar. Ar-guably, it is Earth’s most spectacular example of a “sliver” terrane, dwarfing in size more recently devel-oped examples, for instance the Palawan Block in the western Philippines, and the Lord Howe Rise in the Tasman Sea. The presentation will first outline the in-triguing geological features associated with this unique tectonic entity. Following that, recently obtained results following paleomagnetic investigations of two lower Permian rift-related basalt suites will be summarized (Abor Volcanics in northeastern India and Woniusi Ba-salts in Yunnan, China). The two studies are part of a larger programme of ongoing research aimed at deducing (I) the geodynamic configuration that generated the un-usual rifting system, and (II) exactly how Cimmeria fit-ted against Gondwana prior to its dispersal in the Early Permian. The critical unit is Baoshan, which we fit against Gondwana within a narrow longitudinal belt close to where northern India and northwestern Australia were once in close proximity (Fig. 1). Furthermore, we suggest that Sibumasu lay to directly the east, offshore of Australia; Qiangtang and Lhasa almost certainly sat to the west (off northern Greater India-SE Arabia), but we are uncertain as to their exact configuration. Our findings will be compared with several rather different models that have been published in recent years. The new pa-leomagnetic constraint highlights the flexibility authors currently have in reconstructing the region, principally because of the overall lack of similar high-quality data from the various blocks. We explain how new data could resolve these ambiguities, thereby offering more robust explanations for eastern Gondwana’s late Paleozoic de-velopment. 相似文献