Timing of the onset of collision in the Central and Northern Urals     

G. A. Petrov  Yu. L. Ronkin  A. V. Maslov  I. A. Svyazhina  A. V. Rybalka  O. P. Lepikhina 《Doklady Earth Sciences》2008,422(1):1050-1055

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First geochronological data on felsic lavas from the Ezop-Yamalin volcanoplutonic zone,Khingan-Okhotsk volcanogenic belt     

I. M. Derbeko  A. A. Sorokin  V. A. Ponomarchuk  A. V. Travin  A. P. Sorokin 《Doklady Earth Sciences》2008,419(1):231-234

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Submarine slump folds and gravitational normal faults in Quaternary sediments on the northern slope of the Derbent Basin (Caspian Sea)     

L. I. Lobkovskii  V. E. Verzhbitskii  L. R. Merklin  A. G. Roslyakov  A. S. Polyakov  O. V. Levchenko  S. A. Kovachev  A. S. Zverev  A. D. Mutovkin  V. A. Putans  N. V. Libina  V. Yu. Slobodyan  G. N. Mar  S. V. Gontarev 《Doklady Earth Sciences》2008,420(1):681-685

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Formation conditions of copper porphyry mineralization in the Kadica-Bukovik ore district,eastern Macedonia     

A. V. Volkov  G. Tasev  V. Yu. Prokof’ev  T. Serafimovski  I. N. Tomson  A. A. Sidorov 《Doklady Earth Sciences》2008,421(1):769-773

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Structure features of convective channels from thermal sources in Mutnovskii volcano (South Kamchatka)     

Yu. A. Manshtein  S. B. Bortnikova  A. K. Manshtein  G. M. Gavrilenko  I. V. Vernikovskaya  N. P. Sez’ko 《Doklady Earth Sciences》2008,423(2):1404-1409

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Pyrometamorphic rocks of the spurrite-merwinite facies as indicators of hydrocarbon discharge zones (the Hatrurim formation,Israel)     

E. V. Sokol  I. S. Novikov  S. N. Zateeva  V. V. Sharygin  Ye. Vapnik 《Doklady Earth Sciences》2008,420(1):608-614

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Biological structures in Archean and lower Proterozoic rocks of the Kursk Magnetic Anomaly and Kola Peninsula     

V. I. Sirotin  A. V. Zhabin 《Doklady Earth Sciences》2008,419(2):378-380

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Quantitative criteria for identifying phases and zones of subaqueous lithogenesis of clayey sediments     

E. I. Tkachuk 《Doklady Earth Sciences》2008,419(2):381-383

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Investigation of the stable isotope fractionation in speleothems with laboratory experiments     

E. Wiedner  D. Scholz  A. Mangini  D. Polag  C. Mühlinghaus  M. Segl 《Quaternary International》2008,187(1):15

Many speleothems show evidence for calcite precipitation under disequilibrium conditions. To improve the understanding of these kinetic processes, several laboratory experiments were performed to study the fractionation of stable oxygen and carbon isotopes during the precipitation of calcite. Carbonate was precipitated under controlled conditions from both a body of standing water (beaker experiments) and a solution flowing along a channel (channel experiments) at a relative humidity of 100%. Slow degassing of CO₂, simulated by the beaker experiments, results in δ¹⁸O values in equilibrium with the solution. In contrast, the δ¹³C values show a significant enrichment, inversely proportional to the height of the solution in the beakers. Fast degassing of CO₂, simulated by the channel experiments, showed an enrichment of both δ¹³C and δ¹⁸O and a slope of Δδ¹³C/Δδ¹⁸O of 1.4±0.6. These results represent experimental evidence for the Hendy effect, which is manifested in (i) a progressive increase in δ¹⁸O and δ¹³C away from the growth axis and (ii) a positive correlation between δ¹⁸O and δ¹³C along a single growth layer of a stalagmite.  相似文献   

Millennial-scale climatic and environmental oscillations in the Sea of Okhotsk in response to global changes during the last 190 Ka     

S. A. Gorbarenko  N. Harada  M. I. Malakhov  Yu. P. Vasilenko  A. A. Bosin  E. L. Gol’dberg 《Doklady Earth Sciences》2008,423(2):1410-1413

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