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排序方式: 共有102条查询结果,搜索用时 15 毫秒
51.
Gabriela Polonic 《Tectonophysics》1985,117(1-2)
Based on geological and geophysical data, characteristics of neotectonic activity of the eastern border of the Pannonian Depression are presented.As a result of differential tectonic movements during the Neogene-Quaternary, separate morphostructural units are subjected to subsidence and uplifting, along active faults.The local seismic activity is related, mainly, to the movements along the borders of grabens, as well as at the contact between different crustal blocks. 相似文献
52.
Hans-Rudolf Wenk Erik Rybacki Georg Dresen Ivan Lonardelli Nathan Barton Hermann Franz Gabriela Gonzalez 《Physics and Chemistry of Minerals》2006,33(10):667-676
Mechanical Dauphiné twinning in quartz has been of long-standing interest, both in single crystals and polycrystalline aggregates. This study investigates texture development in fine-grained quartz rock novaculite with no initial texture using compression experiments conducted in the Paterson gas apparatus to explore the influence of stress and temperature. Texture patterns are measured with time-of-flight neutron diffraction and hard synchrotron X-rays, analyzing diffraction data with the Rietveld method. Similar texture patterns are observed as described previously but the new results establish a profound influence of temperature and document that twinning initiates at stresses less than 50 MPa. Possibilities of using Dauphiné twinning as a paleopiezometer in quartz-bearing rocks are discussed. 相似文献
53.
Modern Diatom Assemblages in Surface Sediments from Estuarine Systemsin the Southeastern Buenos Aires Province, Argentina 总被引:1,自引:0,他引:1
Paleoecological reconstructions of Holocene sea-level changes in Argentinean coastal regions were based mainly on ecological
data gathered from other regions, as there was a lack of information on modern estuarine diatom distributions. The aim of
the present work was to assess the spatial variation of diatom assemblages in two representative estuaries of Argentina in
order to gather ecological information for paleoecological reconstructions in the region. The two selected estuaries have
different geomorphologic features and salinity regimes: Mar Chiquita Lagoon is shallow, which prevents the development of
a stable salinity gradient as it occurs in the Quequén Grande River. Surface sediment samples were taken from selected stations
representative of the environmental gradient from the inlet to the inner reaches of both estuaries. Cluster analysis defined
three diatom zones at Mar Chiquita: marine/brackish assemblages dominate the inlet (zone I), where salinity, tidal range and
current speed are higher. The brackish/freshwater tychoplankton Staurosira construens var. venter and Staurosirella pinnata dominate the inner lagoon (zone II), where environmental conditions are very variable and concentrations of suspended sediments
are higher. Brackish/freshwater euryhaline diatoms dominate the headwaters (zone III). On the other hand, the Quequén Grande
River was divided into three diatom zones: coastal taxa are distributed at the inlet (zone I), while the middle estuary (zone
II) is dominated by brackish/freshwater euryhaline taxa. At the upper estuary region (zone III), freshwater diatoms dominate,
and the halophobous Nitzschia denticula increased in abundance values. Diatom distributions were most closely related to the salinity gradient at Quequén Grande
River than at Mar Chiquita Lagoon. Fossil data of a sequence from Mar Chiquita Lagoon (Las Gallinas Creek) were compared to
the modern data set in order to search for analogies between fossil and modern diatom assemblages. DCA results showed that
fossil diatom assemblages have modern counterparts. Most diatom assemblages of Las Gallinas Creek fall within Mar Chiquita
zone III, representing a shallow brackish/freshwater environment, with low salinity fluctuations
(~1–9‰) and no tidal influence. Therefore, our modern diatom data provide useful analogs to interpret paleoenvironments in
the region. 相似文献
54.
Diana Gabriela Lope-Alzina 《Singapore journal of tropical geography》2007,28(1):21-38
This paper examines the influence of gender relations and gendered domains on maize and squash varietal selection in a village in Yucatán State, southeast Mexico. Results of the exploratory study indicate that the traditional production spaces of homegardens and agricultural fields are complementary gendered domains of varietal maintenance for both crops although with different cropping patterns, while a 'new' space, of land allocated to some families for future residential construction ( terreno ) is in the meantime a jointly worked agricultural domain. Women's labour, knowledge and preferences predominate in post-harvest processes. Fieldwork revealed that neither men nor women are independent decision-makers, planning what to grow, where and in what amounts, but that in most aspects of farming the interests of both are accommodated within the household's production spaces. 相似文献
55.
Moreno Wilmer Emilio García Soares Gabriela Borges Pires Júlio César Gall Sotelo Daniela Govoni Moura Cássio Stein 《Geotechnical and Geological Engineering》2021,39(6):4593-4613
Geotechnical and Geological Engineering - A large part of the Guarani Aquifer is located in the state of Rio Grande do Sul (Brazil) and additionally possesses a recharge area located in its central... 相似文献
56.
The influence of the El Niño Southern Oscillation (ENSO) phenomenon on monthly mean river flows of 12 rivers in the extreme south of South America in the 20th century is analysed. The original dataset of each river is divided into two subsets, i.e. warm ENSO events or El Niño, and cold ENSO events or La Niña. The elements of the subsets are composites of 24 consecutive months, from January of the year when the ENSO event begins to December of the following year. The ENSO signal is analysed by comparing the monthly mean value of each subset to the long-term monthly mean. The results reveal that, in general, monthly mean El Niño (La Niña) river flows are predominantly larger (smaller) than the long-term monthly mean in the rivers studied. The anomalies are more evident during the second half of the year in which the event starts and the first months of the following year. 相似文献
57.
de Azevedo Reis Gabriela de Souza Filho Francisco Assis Nelson Donald Robert Rocha Renan Vieira da Silva Samiria Maria Oliveira 《Natural Hazards》2020,104(2):1781-1799
Natural Hazards - Although climate change vulnerability research in general has increased over the last decade, Latin American countries have more directed more limited efforts toward vulnerability... 相似文献
58.
Two large groups of rodents inhabit South America: the hystricognaths and the murids. It has been postulated that while the former show a high degree of specialization to desert habitats, the murids are not well adapted to xeric conditions. We studied the renal structure and function of selected desert-dwelling murid and octodontid (hystricognath) rodents from Argentina to evaluate levels of adaptation to aridity. Our results show that the murids Salinomys, Andalgalomys, Calomys and Eligmodontia have the highest renal indices and urine concentration among Argentine desert rodents. The octodontid Tympanoctomys barrerae shows higher renal indices and urine osmolarity than those of its close relativesOctomys mimax and Octodontomys gliroides . We compare the renal traits of the Argentine desert murids with those of other world-desert rodents such as North American heteromyid rodents. The results show that these Argentine murid rodents posses renal adaptations to conditions which are as impressive as those of both octodontids and the classic desert-adapted heteromyids. 相似文献
59.
Gabriela Athi Frdric Marin Anne-Marie Treguier Bernard Bourls Catherine Guiavarch 《Ocean Modelling》2009,30(4):241-255
This study demonstrates the sensitivity of the near-surface properties in the tropical Atlantic Ocean to the high-frequency of the winds in numerical simulations. At intra-seasonal timescales (2–50 days), two distinct period ranges dominate the variability in the upper ocean: periods between 2 and 20 days, which are essentially wind-forced and periods between 20 and 50 days, due mostly to Tropical Instability Waves (TIWs). Using a numerical model forced by different wind fields, it is shown that the characteristics of the intra-seasonal variability in the ocean surface mixed-layer are strongly dependent on the wind forcing. Submonthly winds are shown to force large variability in the upper ocean that can strikingly decrease the amplitude of the TIWs in the mixed-layer and their imprint on the horizontal distribution of sea surface temperatures. Wind products containing too much energy at submonthly periods thus prevent wind-forced simulations from reproducing a realistic surface signature of TIWs, when compared to satellite observations of sea surface temperature. In addition, submonthly wind variability may be responsible for part of the observed interannual variability of the TIW signature in the temperature. The impact of submonthly winds is strongest in the mixed-layer: beneath the mixed-layer, all simulations show similar characteristics of the TIWs. 相似文献
60.
Gabriela Dan Nabil Sultan Bruno Savoye Jacques Deverchere Karim Yelles 《International Journal of Earth Sciences》2009,98(4):769-789
The Algerian margin is a seismically active region, where during the last century, several large magnitude earthquakes took
place. This study combines geotechnical and sedimentological data with numerical modelling to quantitatively assess the present-day
slope stability of the Algerian margin. Geotechnical laboratory tests, such as cyclic triaxial tests, oedometric tests and
vane shear tests were carried out on sediment cores collected on the study area. The liquefaction potential of a sediment
column located about 30 km from the Boumerdès earthquake epicentre of 21st May 2003 was evaluated theoretically for an earthquake
of M
w
= 6.8. We show that thin sand and silt beds such as those described on recovered sediment cores are the main cause of sediment
deformation and liquefaction during earthquakes. Numerical calculations showed that the slope failure may occur during an
earthquake characterised by a PGA in excess of 0.1g, and also that, under a PGA of 0.2g liquefaction could be triggered in shallow silty–sandy deposits. Moreover, comparison of the predicted slope failure with
failure geometries inferred from seafloor morphology showed that earthquakes and subsequent mass movements could explain the
present-day morphology of the study area. 相似文献