Geology and volcanology of the Edd-Bahar Assoli area (Ethiopia)   总被引：1，自引：0，他引：1  

M. De Fino  L. La Volpe  L. Lirer 《Bulletin of Volcanology》1978,41(1):32-42

The paper presents geological and petrological data on one of the alkaline ranges developed along the borders of the Afar depression (Ethiopia). These alkaline ranges occur in a position transversal to the dominant NNW trend of the spreading zones of northern and central Afar which are characterized by magmas of tholeiitic affinity. The Edd-Bahar Assoli volcanic range consists of broad fields of basic lavas and numerous spatter cones outcropping in the area extending between 13°25′ and 13°75′ lat. N and 41°38′ and 42°15′ long. E. The mineralogical assemblage and the chemical data point to an alkaline nature for this range consisting mainly of alkali olivine basalts and basalts tending to hawaiites, the most evolved terms being largely subordinate. Petrologic differences between the Assab, Edd-Bahar Assoli and Erta Ale ranges are shown. The Edd-Bahar Assoli alkaline volcanism would be related to tectonic patterns trending both from NNW-SSE to N-S and from NE-SW to E-W. The supposed similarity with the transverse structure of the equatorial Atlantic ocean would thus not completely be ascertained in this zone. In Afar, the coexistence of an axial volcanism of tholeiitic affinity with an alkaline volcanism at the margin can better be explained by models based upon the upper mantle temperature distribution in a zone under oceanization.  相似文献   

Meteorological microseisms and stratospheric warmings     

Jan Laštovička  Reviewer A. Zátopek 《Studia Geophysica et Geodaetica》1979,23(1):98-100

Summary The meteorological microseisms recorded at Prague are found to be essentially independent of the occurrence of the major midwinter stratospheric warmings. This finding contributes to studying the downward propagation mechanism of some extraterrestrial influences.  相似文献   

Sudden ionospheric disturbances and flare activity in the course of the solar cycle no 20     

Ladislav Křivský  Jan Laštovička  Reviewer S. Krajčovič 《Studia Geophysica et Geodaetica》1979,23(4):393-394

a¶rt;a ma nu an u u (SID) u nu n a (a n¶rt; au) mu 1965–1975 . u u SID na¶rt;am nau, mum u nm R.  相似文献   

The use of laboratory measurements of electric resistivity of rocks for evaluating the magnetotelluric method     

Marcela Laštovičková  Josef Pek  Reviewer M. Hvoždara 《Studia Geophysica et Geodaetica》1979,23(1):94-98

Summary A profile model of electric resistivity as a function of depth was compiled, the initial parameters being the values of the electric resistivity determined experimentally for basaltic and eclogitic rocks from the Bohemian Massif. The curves of the apparent resistivity were computed for this model and the measure of information evaluated for the various model layers. The dominant influence of the subsurface layer was proved.  相似文献   

The response of the total electron content to the interplanetary magnetic sector boundary crossing     

František Blahák  Jan Laštovička  Revievwer L. Křivský 《Studia Geophysica et Geodaetica》1980,24(1):60-64

¶rt;m uu n ¶rt;au m uu nu mau nam aum n. mu uu auam mmmuu uuu ¶rt;u u naam. a¶rt;am auu ¶rt; uuu n ¶rt;au m u u. a auu a¶rt;am nuu amm 245 . ¶rt;aam umnmau m a¶rt;a uu.  相似文献   

Day-time ionospheric disturbances of corpuscular origin in the midlatitudeD-region     

Jan Laštovička  Josef Boška  Reviewer L. Křivský 《Studia Geophysica et Geodaetica》1980,24(2):191-196

¶rt;m uu nau mu m a nu a¶rt;u ¶rt; D-amu u. a¶rt; m nu u u. u¶rt;a a a mu nma u nma mu m (20 ¶rt; 150 ).  相似文献   

The role of various ionization sources in the A3 lf radio-wave absorption in middle latitudes     

Jan Laštovička  Reviewer J. Prokop 《Studia Geophysica et Geodaetica》1977,21(3-4):403-410

Summary The 272 kHz ionospheric absorption has been measured at the Prhonice Observatory by the A3 method (oblique incidence) for a long period. The results of the comparison of these absorption data with indices of solar, geomagnetic and cosmic ray activity are presented for large solar zenith angles. The day-time absorption (x 75° – 85°) is described well by these indices and appears to be affected particularly by direct solar Lyman- radiation. The night-time absorption (x>100°), however, is not described sufficiently by the indices used.  相似文献   

Relationship between microseisms,geomagnetic activity and ionospheric absorption of radio waves     

Jan Laštovička  Reviewer A. Zátopek 《Studia Geophysica et Geodaetica》1974,18(3):307-309

Summary Relatively good correlation between such remote phenomena as microseisms, geomagnetic activity and ionospheric absorption of radio waves has been observed. These phenomena are probably connected by a considerably increased penetration of energetic particles into the atmosphere under conditions of geomagnetic activity.  相似文献   

On the role of the solar Lyman-α radiation in ionospheric absorption at 2775 kHz     

J. Laštovička 《Pure and Applied Geophysics》1974,112(4):655-663

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Relict sand dredging for beach nourishment in the central Tyrrhenian Sea (Italy): effects on benthic assemblages     

Barbara La Porta  Monica Targusi  Loretta Lattanzi  Paola La Valle  Daniela Paganelli  & Luisa Nicoletti 《Marine Ecology》2009,30(S1):97-104

The aim of this study is to analyse the effects in space and time of relict sand-dredging activities on macrobenthic assemblages, in an area situated offshore Montalto di Castro (central Tyrrhenian Sea, Italy), and to analyse the recolonisation processes of macrobenthos in the dredged areas. The area in question is characterised by relict sand deposits (Holocenic paleo-beaches), used for beach nourishment along the Latium coast. The effects of sand extraction on benthic assemblages were investigated before, during and after three dredging operations. The sites analysed are located within the dredged areas (inside stations) and in neighbouring, not dredged, areas (outside stations). The results showed that the impact of sand extraction was confined to the dredged stations and to the areas in proximity to the dredged areas. During dredging activities, the structure of benthic assemblages within the impacted stations was characterised by low species richness and diversity. Both the direct removal of sediment and the re-suspension and consequent deposition of fine sediment affected benthic assemblages of the impacted stations. A few months after the dredgings, a recolonisation process was still observed at all the impacted stations. A gradual recolonisation process was observed at those stations affected by only one dredging, whereas a different recolonisation was observed at those stations affected by two dredgings over time. This study suggests that differences of re-colonisation processes of benthic assemblages are related to the intensity of dredging operations in terms of dredging frequency.  相似文献