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排序方式: 共有142条查询结果,搜索用时 15 毫秒
71.
Textural evolution of synthetic fluid inclusions in quartz during reequilibration,with applications to tectonic reconstruction 总被引:4,自引:0,他引:4
Experimental reequilibration of synthetic 10 wt% NaCl-H2O inclusions in natural quartz reveals that reequilibration textures show distinct differences depending upon the P-T path
followed by the inclusion after formation. These differences combined with other geological information may be used to determine
whether the sample (rock) followed a dominantly isothermal or isobaricP-T path following entrapment. The intensity and style of inclusion reequilibration features is related to the direction and
magnitude of the departure of theP-T path from the original isochore for the inclusion. Thus, fluid inclusion reequilibration textures not only permit inclusionists
to determine whether the rocks followed an isothermal or isobaric retrogradeP-T path, but also the magnitude of departure of this path from one that is isochoric.
Editorial responsibility: J. Touret 相似文献
72.
This paper shows how static failure loads can be used to predict impact failure of granules. A theoretical model is presented that gives the maximum force experienced during impact and equates this to experimentally measured static failure load to define a critical impact velocity for impact failure. A granule will fail if the predicted theoretical maximum force during impact due to the impact velocity is greater than the real force required to produce failure in that particular granule. 相似文献
73.
Geomagnetism and Aeronomy - The possible relationship between the 60-year variation in global temperature with an amplitude of 0.35°C and the corresponding cycle at the location of Jupiter and... 相似文献
74.
Geomagnetism and Aeronomy - Solar-climatic correlations were examined over the timescales, corresponding to solar cycles of Schwabe, Hale and Gleissberg, during the last 3–4 centuries using... 相似文献
75.
M. G. Ogurtsov 《Astronomy Letters》2018,44(4):278-288
The solar modulation potential has been reconstructed from data on the 10Be concentration in south and central Greenland ice over more than 500 last years. These two reconstructions, along with fourteen others obtained by various authors from data on the cosmogenic isotopes 14C and 10Be, have been investigated in the time interval 1630–1840 encompassing the Maunder and Dalton minima. The information contained in these sixteen paleoreconstructions has been generalized. The available data on the concentration of cosmogenic isotopes in terrestrial archives suggest that the solar activity in the first part of theMaunder minimum (1645–1680) was lower than that at the Dalton minimum (1792–1827), while in the second part (1680–1715) it was considerably lower. At the same time, at the beginning of theMaunder minimum (1645–1660) the solar activity could reach levels exceeding noticeably the estimates based on telescopic observations. Possible causes of these discrepancies and the directions of further research are discussed. 相似文献
76.
Maxim G. Ponomarjov 《Astrophysics and Space Science》2000,274(1-2):423-429
In this paper a method is concerned which makes it possible to describe numerically and analytically the most famous structures
in the non-equilibrium ionosphere, such as stratified and yacht sail like structures, flute jets, wakes and clouds. These
problems are of practical interest in space sciences, astrophysics and in turbulence theory, and also of fundamental interest
since they enable one to concentrate on the effects of the ambient electric and magnetic fields. Disturbances of charged particle
flows due to the ambient flow interactions with bodies are simulated with taking into account the ambient magnetic field effect.
The effects of interactions between solid surfaces and the flows was simulated by making use of an original image method.
The flow disturbances were described by the Boltzmann equation. In the case of the ambient homogeneous magnetic field the
Boltzmann equation is solved analytically. The case of diffuse reflection of particles by surface is considered in detail.
The disturbances of charged particle concentration are calculated in 3D space. The contours of constant particle concentration
obtained from numerical simulations illustrate the dynamics of developing stratifications and flute structures in charged
particle jets and feffect. The wakes under the ambient magnetic field effect. The basic goal of this paper is to present the
method and to demonstate its possibility for simulations of turbulence, plasma jets, wakes and clouds inthe ionosphere and
Space when effects of electric and magnetic fields are taken into account.
This revised version was published online in July 2006 with corrections to the Cover Date. 相似文献
77.
Investigation of active faults is crucial for the seismic hazard assessment and, in the case of volcanic belts, it provides a deeper understanding of the interactions between volcanism and tectonic faulting. In this study, we report the results of the first paleoseismological and tephrochronological investigation undertaken on Holocene faulting in Kamchatka's volcanic belts. The studied trenches and additional excavations are located along the axial fault zone of the Eastern Volcanic Front, where the earlier dated tephra layers provide a robust age control of the faulting events. Electron microprobe analysis of glass from 22 tephra samples permitted correlations among the disparate tephra profiles for constructing a summary tephra sequence. The latter, together with published geochronological data, allowed the construction of a Bayesian age model. Detailed examination of the tephra layers deformed by faulting allowed us to reconstruct and date six faulting events with the offsets of 1 to 20 cm indicating paleoearthquakes with magnitudes of Mw < 5.4. Holocene crustal seismicity of the Eastern Volcanic Front manifests temporal clustering rather than a uniform flux of events. However, no correlation between dated seismic events and the largest Holocene eruptions of proximal volcanoes was observed. 相似文献
78.
Polina Vakhrameeva Maxim Portnyagin Vera Ponomareva Peter M. Abbott Tatiana Repkina Anna Novikova Andreas Koutsodendris Jörg Pross 《第四纪科学杂志》2020,35(4):493-504
The generation of reliable age models for palaeoenvironmental and archaeological records in the Eurasian Arctic is often problematic when using conventional dating techniques. Tephrochronology can potentially improve the chronologies of such records and synchronise disparate sedimentary archives. However, to date, systematic tephra studies are lacking for this region. This paper presents the first cryptotephra data from the White Sea region (northwestern Russia) based on a peat core spanning the past ~1800 years. We identify seven geochemical glass populations that derive from six Icelandic volcanoes and correlate four of them to north European tephra isochrons; these include Askja ad 1875, the basaltic component of the ad 877 Landnám tephra, and tephras BTD-15 (c. ad 1750–1650) and SL-2/SB-2 (ad 803–767) from unknown eruptions of Katla and Snæfellsjökull, respectively. The remaining three populations originate from Grímsvötn, Hekla and Katla; however, their attribution to individual eruptions remains ambiguous. These findings highlight the potential to extend the Late Holocene tephrochronological framework of northern Europe to the west Eurasian Arctic. The detection of at least three basaltic tephras in the core suggests that basaltic shards can be transported over larger distances than previously known and that peatlands are well suited to preserve such components. 相似文献
79.
O. M. Raspopov V. A. Dergachev G. I. Zaitseva M. G. Ogurtsov 《Geomagnetism and Aeronomy》2013,53(8):917-921
It is shown that, over the past ~10000 years (the Holocene), deep Maunder type solar minima have been accompanied by sharp climate changes. These minima occurred every 2300–2400 years. It has been established experimentally that, at ca 4.0 ka BP, there occurred a global change in the structure of atmospheric circulation, which coincided in time with the discharge of glacial masses from Greenland to North Atlantic and a solar activity minimum. The climate changes that took place at ca 4.0 ka BP and the deep solar activity minimum that occurred at ca 2.5 ka BP affected the development of human society, leading to the degradation and destruction of a number of ancient civilizations. 相似文献
80.