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31.
The development of soft‐sediment deformation structures in clastic sediments is now reasonably well‐understood but their development in various deltaic subenvironments is not. A sedimentological analysis of a Pleistocene (ca 13·1 to 15 10Be ka) Gilbert‐type glaciolacustine delta with gravity‐induced slides and slumps in the Mosty‐Danowo tunnel valley (north‐western Poland) provides more insight, because the various soft‐sediment deformation structures in these deposits were considered in the context of their specific deltaic subenvironment. The sediments show three main groups of soft‐sediment deformation structures in layers between undeformed sediments. The first group consists of deformed cross‐bedding (inclined, overturned, recumbent, complex and sheath folds), large‐scale folds (recumbent and sheath folds) and pillows forming plastic deformations. The second group comprises pillar structures (isolated and stress), clastic dykes with sand volcanoes and clastic megadykes as examples of water‐escape structures. The third group consists of faults (normal and reverse) and extensional fissures (small fissures and neptunian dykes). Some of the deformations developed shortly after deposition of the deformed sediment, other structures developed later. This development must be ascribed to hydroplastic movement in a quasi‐solid state, and due to fluidization and liquefaction of the rapidly deposited, water‐saturated deltaic sediments. The various types of deformations were triggered by: (i) a high sedimentation rate; (ii) erosion (by wave action or meltwater currents); and (iii) ice‐sheet loading and seasonal changes in the ablation rate. Analysis of these triggers, in combination with the deformational mechanisms, have resulted – on the basis of the spatial distribution of the various types of soft‐sediment deformation structures in the delta under study – in a model for the development of soft‐sediment deformation structures in the topsets, foresets and bottomsets of deltas. This analysis not only increases the understanding of the deformation processes in both modern and ancient deltaic settings but also helps to distinguish between the various subenvironments in ancient deltaic deposits. 相似文献
32.
Palaeo- and Neo-Tethyan-related magmatic and metamorphic units crop out in Konya region in the south central Anatolia. The Neotethyan assemblage is characterized by mélange and ophiolitic units of Late Cretaceous age. They tectonically overlie the Middle Triassic–Upper Cretaceous neritic to pelagic carbonates of the Tauride platform. The metamorphic sole rocks within the Konya mélange crop out as thin slices beneath the sheared serpentinites and harzburgites. The rock types in the metamorphic sole are amphibolite, epidote-amphibolite, garnet-amphibole schist, plagioclase-amphibole schist, plagioclase-epidote-amphibole schist and quartz-amphibole schist. The geochemistry of the metamorphic sole rocks suggests that they were derived from the alkaline (seamount) and tholeiitic (E-MORB, IAT and boninitic type) magmatic rocks from the upper part of the Neotethyan oceanic crust. Four samples from the amphibolitic rocks yielded 40Ar/39Ar isotopic ages, ranging from 87.04 ± .36 Ma to 84.66 ± .30 Ma. Comparison of geochemistry and geochronology for the amphibolitic rocks suggests that the alkaline amphibolite (seamount-type) cooled below 510 ± 25 °C at 87 Ma whereas the tholeiitic amphibolites at 85 Ma during intraoceanic thrusting/subduction. When all the evidence combined together, the intraoceanic subduction initiated in the vicinity of an off-axis plume or a plume-centered spreading ridge in the Inner Tauride Ocean at 87 Ma. During the later stage of the steady-state subduction, the E-MORB volcanics on the top of the down-going slab and the arc-type basalts (IAT/boninitic) detached from the leading edge of the overriding plate, entered the subduction zone after ~2 my and metamorphosed to amphibolite facies in the Inner Tauride Ocean. Duration of the intraoceanic detachment (~87 Ma) and ophiolite emplacement onto the Tauride-Anatolide Platform (Tav?anl? Zone), followed by subsequent HP/LT metamorphism (~82 Ma) spanned ~5 my in the western part of the Inner Tauride Ocean. 相似文献
33.
Andrzej W. Wernik Mariusz Pożoga Marcin Grzesiak Andrzej Rokicki Marek Morawski 《Acta Geophysica》2008,56(4):1129-1146
As a partial contribution to the International Polar Year, the Space Research Centre of the Polish Academy of Sciences has
installed on the Polish Polar Station, located in the region of the Hornsund Bay in southern Spitsbergen, the equipment intended
to monitor ionospheric scintillation and total electron content. We describe the equipment setup and the aims of the experiment.
As an illustration of data analysis, we present the reconstruction of irregular structure of the ionosphere from the complex
amplitude data, and the estimate of the form and drift of diffraction pattern based on the spaced receiver measurements. 相似文献
34.
Matyasovszky István Makra László Tusnády Gábor Csépe Zoltán Nyúl László G. Chapman Daniel S. Sümeghy Zoltán Szűcs Gábor Páldy Anna Magyar Donát Mányoki Gergely Erostyák János Bodnár Károly Bergmann Karl-Christian Deák Áron József Thibaudon Michel Albertini Roberto Bonini Maira Šikoparija Branko Radišić Predrag Gehrig Regula Rybníček Ondřej Severova Elena Rodinkova Victoria Prikhodko Alexander Maleeva Anna Stjepanović Barbara Ianovici Nicoleta Berger Uwe Seliger Andreja Kofol Weryszko-Chmielewska Elżbieta Šaulienė Ingrida Shalaboda Valentina Yankova Raina Peternel Renata Ščevková Jana Bullock James M. 《Theoretical and Applied Climatology》2018,133(1-2):277-295
Theoretical and Applied Climatology - The drivers of spatial variation in ragweed pollen concentrations, contributing to severe allergic rhinitis and asthma, are poorly quantified. We analysed the... 相似文献
35.
Roderick J. Mclntosh Boubacar Hama Diaby Tér’ba Togola 《Natural Resources Research》1997,6(2):111-129
There is a civilization at risk. In the middle of West Africa, just south of the Sahara, where the Niger River spills into
a vast floodplain (the Middle Niger), an indigenous urban civilization emerged around two thousand years ago. The story of
that civilization is just beginning to be uncovered from the thousands of tells (ancient settlement mounds) that litter the
Middle Niger, but archaeologists have until recently been loosing the race with the looters who plunder these sites for ancient
statues and bronze art. The nation of Mali, and the local community of Jenne at the epicenter of this looting recently invented
effective shields for the remains of this civilization, protections against local looters in the employ of a syndicate of
wealthy European antiquities dealers. In the person of the new, democratically-elected archaeologist-President, the nation
has articulated a vision of Mali’s future linked to the preservation of its past. The government has promulgated effective
regulations and education programs, and initiated with the United States the world’s first bilateral import ban between a
major “source” and a major “market” nation. This 1993 bilateral accord has become a prototype for many nations. In that same
year, Mali established a Cultural Mission at Jenne to reinforce local pride in a local past. This local pride, in only a short
period, has turned into a total protection of some 200 sites within a ten-kilometer radius of Jenne. These indigenous actions
have, in less than a decade, transformed the nonrenewable archaeological resources of the Jenne region from surely one of
the world’s most endangered, to a case study in local and national protection 相似文献
36.
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38.
ZBIGNIEW PASŁAWSKI 《水文科学杂志》2013,58(3):295-301
ABSTRACT The occurrence of cyclic fluctuations and trends in water levels has been tested by examining a long-term series of mean annual water levels in 11 outflow lakes, mostly groove lakes, located in Northern Poland between 14° E and 23° E and situated at different altitudes up to 120 m above sea level. Analysis of the occurrence of cyclic fluctuations of water levels has been carried out by means of mass curves. The regression method together with the moving average method applied to 10-year values of mean annual water levels were used to establish the trend in water levels. On the basis of the research completed, it has been stated that long-term fluctuations of mean annual water levels of the lakes under investigation, in spite of the absence of a distinct periodicity, are characterized by a cycle with a 23-year period. The studies of the trends of mean annual water levels revealed a negative tendency ranging from—0·059 to—0·402 cm per annum. 相似文献
39.
Łydżba Dariusz Różański Adrian Sevostianov Igor Stefaniuk Damian 《Acta Geotechnica》2022,17(11):5059-5072
Acta Geotechnica - We evaluate thermal conductivity of the skeleton of porous sandstone from the measurements of the effective thermal conductivities of dry and saturated specimens provided by... 相似文献
40.
Zenon Nieckarz Andrzej Kuak Stanisaw Ziba Marek Kubicki Stanisaw Michnowski Piotr Baraski 《Atmospheric Research》2009,91(2-4):184-187
This work presents the results of a comparison between the global storm activity rate IRS and electric field intensity E0Z. The permanent analysis of the IRS may become an important tool for testing Global Electric Circuit models. IRS is determined by a new method that uses the background component of the first 7 Schumann resonances (SR). The rate calculations are based on ELF observations carried out in 2005 and 2006 in the observatory station “Hylaty” of the Jagiellonian University in the Eastern Carpathians (Kułak, A., Zięba, S., Micek, S., Nieckarz, Z., 2003. Solar variations in extremely low frequency propagation parameters: I. A two-dimensional telegraph equation (TDTE) model of ELF propagation and fundamental parameters of Schumann resonances, J. Geophys. Res., 108, 1270, doi:10.1029/2002JA009304). Diurnal runs of the IRS rate were compared with diurnal runs of E0Z amplitudes registered at the Earth's surface in the Geophysical Observatory of the Polish Academy of Sciences in Świder (Kubicki, M., 2005. Results of Atmospheric Electricity and Meteorological Observations, S. Kalinowski Geophysical Observatory at Świder 2004, Pub. Inst. Geophysics Polish Academy of Sciences, D-68 (383), Warszawa.). The days with the highest values of the correlation coefficient (R) between amplitudes of both observed parameters characterizing atmosphere electric activity are shown. The seasonal changes of R, IRS and E0Z are also presented. 相似文献