Upper Jurassic and lower cretaceous of Sanjiang-Middle Amur basin: Non-marine and marine correlation   总被引：1，自引：0，他引：1  

JinGeng Sha  JianPo Wang  Galina Kirillova  YanHong Pan  HuaWei Cai  YaQiong Wang  XiaoGang Yao  Bo Peng 《中国科学D辑(英文版)》2009,52(12):1873-1889

A comparative analysis of Late Jurassic-Early Cretaceous strata have been done for the Sanjiang-Middle Amur basin, a coal- and oil-bearing area spanning the eastern Heilongjiang of northeastern China and southeastern Far East of Russia. On the basis of various fossils occurring in the formations, particularly by means of the Tithonian-Valanginian index Buchia and the late Barremian-middle Albian indicator Aucellina assemblages, the marine and non-marine Late Jurassic-Early Cretaceous strata in the basin are correlated. The Mesozoic international chronostratigraphic chart () is established basically based on the marine rocks. To accurately date the non-marine strata, it is necessary to correlate them with the marine deposits. This study sheds new light on the dating and correlation of non-marine Upper Mesozoic. Additionally, the results would help understand the tectonics and paleogeography and thus aid the exploration of energy resources.  相似文献   

An empirical model for the calculation of spinel-melt equilibria in mafic igneous systems at atmospheric pressure: 2. Fe-Ti oxides     

Alexi A. Ariskin  Galina S. Barmina 《Contributions to Mineralogy and Petrology》1999,134(2-3):251-263

In order to develop models simulating the crystallization of Fe-Ti oxides in natural lavas, we have processed published experimental data on magnetite-melt and ilmenite-melt equilibria. These data include 62 Mt-melt and 75 Ilm-melt pairs at temperatures 1040–1150 °C, oxygen fugacities from IW to NNO+2, and bulk compositions ranging from ferrobasalts to andesites and dacites. Five major cations (Fe³⁺, Fe²⁺, Ti⁴⁺, Mg²⁺ and Al³⁺) were considered for the purpose of describing Fe-Ti oxide saturation as a function of melt composition, temperature and oxygen fugacity at 1 atmosphere pressure. The empirically calibrated mineral-melt expression based on multiple linear regressions is: ln D _i  = a/T + blog f _O2 + c + d ₁ X _Na + d ₂ X _K + d ₃ X _P, where D _i represents molar distribution coefficients of the given cations between Mt/Ilm and melt; X _Na, X _K, and X _P are the molar fractions of Na, K, and P in the melt. The empirically calibrated Mt-melt and Ilm-melt equilibria equations allowed us to develop two models for calculating crystallization temperatures of the Fe-Ti oxides in the melts with an accuracy of 10–15 °C, and compositions with an accuracy of 0.5–2 mol%. These models have been integrated into the COMAGMAT-3.5 program, improving our ability to study numerically the effects of temperature and oxygen fugacity on the stability and phase equilibria of Fe-Ti oxides. Application of this approach to the tholeiitic series of Chazhma Sill from Eastern Kamchatka (Russia) indicates oxygen fugacity conditions near NNO + 0.5. Numerical simulation of fractional crystallization of an iron-enriched basaltic andesite parent at these oxidizing conditions accurately reproduces the FeO-SiO₂ relations observed in the Chazhma suite. Received: 3 March 1998 / Accepted: 7 August 1998  相似文献   

Evidence for mid-Eemian cooling in continental climatic record from Lake Baikal     

Eugene B. Karabanov  Alexander A. Propenko  Douglas F. Williams  Galina K. Khursevich 《Journal of Paleolimnology》2000,23(4):365-371

The discussion on climatic instability observed in Greenland ice cores during the Eemian period (substage 5e) resulted in discovery of a pronounced mid-Eemian cooling event. We report that the mid-Eemian cooling is found for the first time in the biogenic silica climatic record and microfossil abundance record of Lake Baikal. Timing of this event in Lake Baikal correlates well with timing of the European pollen records and marine sedimentary records. The presence of the mid-Eemian cooling signal in the Lake Baikal record suggests a much closer link between Asian climate influenced by strong pressure fields over the vast land masses and the climate-controlling processes in the North Atlantic during interglacial periods, than what was generally believed. Furthermore, the Lake Baikal record suggests that after the mid-Eemian cooling, the climatic conditions returned close to the warmth of the 5e optimum and thus argues that the warm conditions of the last interglacial persisted in Siberia throughout 5e, and did not end with the mid-Eemian cooling as suggested by several published marine records.  相似文献   

Investigating the Balance between Timber Harvest and Productivity of Global Coniferous Forests under Global Change   总被引：2，自引：0，他引：2  

Galina Churkina  Steven Running 《Climatic change》2000,47(1-2):167-191

A widely used assumption in forestry is that thedemand for timber will exceed the maximum levelavailable from forests on a sustainable basis. In thisstudy, measurements of extracted timber and modeledforest productivity were used to investigate therelationship between harvested timber and naturalforest productivity for current conditions, and underglobal change scenario. The analysis was confined toconiferous forests and countries that have coniferousforests within their territories. Annual roundwoodproduction from the database of Food and AgricultureOrganization was used as an approximation of annualtimber harvest for each country. Annual stem primaryproductivity of coniferous forests was estimated usingthe BIOME-BGC model. Based on the current rates,annual timber extraction was extrapolated for eachcountry for the next 80 years. Then, on a countrybasis, the timber harvest was related to the modeledforest stem productivity, assuming that the area ofconiferous forest would stay unchanged for the next 80years.The results of this study suggest that globalconiferous forests currently produce more wood thanpeople consume, but that this gap will narrow in thefuture. The results also suggest that wood extractionmay reach forest regrowth by the middle of the nextcentury, even though most coniferous forests arelocated in high latitudes and may have an acceleratedstem growth associated with the joint effect ofclimate change and elevated carbon dioxideconcentration in the atmosphere.  相似文献   

Sedimentation patterns in the Selenga River delta under changing hydroclimatic conditions          下载免费PDF全文

Jan Pietroń  Jeffrey A. Nittrouer  Sergey R. Chalov  Tian Y. Dong  Nikolay Kasimov  Galina Shinkareva  Jerker Jarsjö 《水文研究》2018,32(2):278-292

The Selenga River delta (Russia) is a large (>600 km²) fluvially dominated fresh water system that transfers water and sediment from an undammed drainage basin into Lake Baikal, a United Nations Educational, Scientific, and Cultural Organization World Heritage Site. Through sedimentation processes, the delta and its wetlands provide important environmental services, such as storage of sediment‐bound pollutants (e.g., metals), thereby reducing their input to Lake Baikal. However, in the Selenga River delta and many other deltas of the world, there is a lack of knowledge regarding impacts of potential shifts in the flow regime (e.g., due to climate change and other anthropogenic impacts) on sedimentation processes, including sediment exchanges between deltaic channels and adjacent wetlands. This study uses field measurements of water velocities and sediment characteristics in the Selenga River delta, investigating conditions of moderate discharge, which have become more frequent over the past decades (at the expense of peak flows, Q > 1,350 m³ s^?1). The aims are to determine if the river system under moderate flow conditions is capable of supporting sediment export from the main distributary channels of the delta to the adjacent wetlands. The results show that most of the deposited sediment outside of the deltaic channels is characterized by a large proportion of silt and clay material (i.e., <63 μm). For example, floodplain lakes function as sinks of very fine sediment (e.g., 97% of sediment by weight < 63 μm). Additionally, bed material sediment is found to be transported outside of the channel margins during conditions of moderate and high water discharge conditions (Q ≥ 1,000 m³ s^?1). Submerged banks and marshlands located in the backwater zone of the delta accumulate sediment during such discharges, supporting wetland development. Thus, these regions likely sequester various metals bound to Selenga River sediment.  相似文献   

Historical seismogram reproductions for the source parameters determination of the 1902, Atushi (Kashgar) earthquake     

Galina Kulikova  Frank Krüger 《Journal of Seismology》2017,21(6):1577-1597

The majority of original seismograms recorded at the very beginning of instrumental seismology (the early 1900s) did not survive till present. However, a number of books, bulletins, and catalogs were published including the seismogram reproductions of some, particularly interesting earthquakes. In case these reproductions contain the time and amplitude scales, they can be successfully analyzed the same way as the original records. Information about the Atushi (Kashgar) earthquake, which occurred on August 22, 1902, is very limited. We could not find any original seismograms for this earthquake, but 12 seismograms from 6 seismic stations were printed as example records in different books. These data in combination with macroseismic observations and different bulletins information published for this earthquake were used to determine the source parameters of the earthquake. The earthquake epicenter was relocated at 39.87° N and 76.42° E with the hypocenter depth of about 18 km. We could further determine magnitudes m _B = 7.7 ± 0.3, M _S = 7.8 ± 0.4, M _W = 7.7 ± 0.3 and the focal mechanism of the earthquake with strike/dip/rake ? 260°± 20/30°± 10/90°± 10. This study confirms that the earthquake likely had a smaller magnitude than previously reported (M8.3). The focal mechanism indicates dominant thrust faulting, which is in a good agreement with presumably responsible Tuotegongbaizi-Aerpaleike northward dipping thrust fault kinematic, described in previous studies.  相似文献   

Conditions for the origin of oxidized carbonate-silicate melts: Implications for mantle metasomatism and diamond formation     

Y.V. Bataleva  Y.N. Palyanov  A.G. Sokol  Y.M. Borzdov  G.A. Palyanova 《Lithos》2012

An experimental study on the origin of ferric and ferrous carbonate-silicate melts, which can be considered as the potential metasomatic oxidizing agents and diamond forming media, was performed in the (Ca,Mg)CO₃-SiO₂-Al₂O₃-(Mg,Fe)(Cr,Fe,Ti)O₃ system, at 6.3 GPa and 1350–1650 °C. At 1350–1450 °C and ?O₂ of FMQ + 2 log units, carbonate–silicate melt, coexisting with Fe^3 +-bearing ilmenite, pyrope-almandine and rutile, contained up to 13 wt.% of Fe₂O₃. An increase in the degree of partial melting was accompanied by decarbonation and melt enrichment with CO₂, up to 21 wt.%. At 1550–1650 °C excess CO₂ segregated as a separate fluid phase. The restricted solubility of CO₂ in the melt indicated that investigated system did not achieve the second critical point at 6.3 GPa. At 1350–1450 °C and ?O₂ close to CCO buffer, Fe^2 +-bearing carbonate–silicate melt was formed in association with pyrope-almandine and Fe^3 +-bearing rutile. It was experimentally shown that CO₂-rich ferrous carbonate-silicate melt can be an effective waterless medium for the diamond crystallization. It provides relatively high diamond growth rates (3–5 μm/h) at P,T-conditions, corresponding to the formation of most natural diamonds.  相似文献   

Analysis of Diatoms of the Water Column and Bottom Sediments of Lake Shira(Khakassia,Russia)     

Galina BOLOBANSCHIKOVA  Denis ROGOZIN 《《地质学报》英文版》2014,88(Z1):56-57

正Meromictic lakes are interesting objects for study in terms of paleolimnology.The lamination of the bottom sediments well expressed in these lakes.It is related with permanent stratification of the water column.Through this  相似文献   

Supercritically accreting stellar mass black holes as ultraluminous X-ray sources     

Juri Poutanen  Galina Lipunova  Sergei Fabrika  Alexey G. Butkevich  Pavel Abolmasov 《Monthly notices of the Royal Astronomical Society》2007,377(3):1187-1194

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Gold fineness and Au/Ag ratios of pyrite-containing ores as additional indicators of physico-chemical conditions of hydrothermal ore formation     

Galina Palyanova 《Journal of Geochemical Exploration》2009

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