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661.
<正>Whalfera wiszniewskii sp.nov.is described from the Late Eocene Baltic amber.The genus Whalfera is considered as the only fossil genus confidently assigned to the Rhachlberothinae.Others previously placed in this subfamily belong to Paraberothinae(except perhaps for Oisea).The Late Eocene/present Rhachiberothinae and the Cretaceous Paraberothinae are considered to be the subfamilies of Berothidae. 相似文献
662.
Vladimir Frid Dmitri Doudkinski Gady Liskevich Efim Shafran Arie Averbakh Nikolay Korostishevsky Larisa Prihodko 《Environmental Earth Sciences》2010,60(4):787-798
This paper deals with the integration of electrical resistivity tomography and geochemical methods for studying four different
fire-prone landfills. Landfill gas composition (CH4, H2S, O2, CO, CO2) and subsurface temperature were measured with the constant net 50 × 50 m from the depth 10–60 cm. 28 electrical resistivity
tomography lines were surveyed, while Wenner and Sclumberger electrode arrays were employed for all measurements. At the studied
sites the landfill gas and temperature measurements mapped gas and temperature anomalies over underground fire sources. 2D
electrical resistivity tomography lines, performed over these anomalies, showed these fire sources as high-resistivity zones.
The joint employment of the electrical imaging and geochemical survey seems to be a useful tool in carrying out diagnostic
investigations at fire-prone landfills. 相似文献
663.
Aleksandra AJNOV Vladimir SIMI Branimir JOVANIEVI Olga CVETKOVI Radovan DIMITRIJEVI Nenad GRUBIN 《《地质学报》英文版》2008,82(6)
Sediments of the western part of the Valjevo-Mionica basin (Serbia) were examined both geochemically and mineralogically to explain, on the basis of their sedimentological characteristics, the causes of changes in their qualitative and quantitative composition. A total of 62 samples obtained from the drillhole at depths up to 400 m was investigated. Using correlation of the obtained data, six geochemical zones were defined, two of which being specially distinguished by their mineralogical, geochemical and sedimentological characteristics. The first one, upper zone A, consists of banded marlstones interbedded with clay and oil shales and is characterized by presence of analcite and searlesite. These minerals and very high contents of Na2O indicate sedimentation in alkaline conditions with increased salinity in arid climate. That provided pronounced water stratification, as well as higher bioproductivity in the basin and sedimentary organic matter preservation. Therefore, the zone A sediments are characterized by high organic matter contents of the type which provides good potential for production of liquid hydrocarbons. Another specific zone, zone F, contains sediments with very high MgO, K2O and Li concentrations. Their geochemical correlation, as well as almost complete absence of illite in this zone, indicates the presence of interstratified clay mineral type illite-saponite (lithium-bearing Mg-smectite). 相似文献