Heavy clastic minerals as a criterion for the identification of island-arc environments in paleobasins of orogenic zones in the Russian Far East     

P. V. Markevich  A. I. Malinovsky 《Doklady Earth Sciences》2006,409(1):709-712

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Radiocarbon dates and palynological characteristics of sediments in Lake Melkoe, Anadyr River basin, Chukotka     

Academician of the RAS N. A. Shilo  A. V. Lozhkin  P. M. Anderson  T. A. Brown  T. V. Matrosova  A. N. Kotov 《Doklady Earth Sciences》2006,407(1):230-232

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New forms of platinum group minerals in ferruginous quartzites of the Lebedyan deposit, Kursk Magnetic Anomaly (Central Russia)     

N. M. Chernyshov  S. V. Petrov 《Doklady Earth Sciences》2006,408(1):586-589

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Metamafic rocks of the Tana Belt, Kola Peninsula: Isotopic age and PT conditions     

L. L. Perchuk  J. D. Kramers  V. O. Yapaskurt  A. V. Krotov 《Doklady Earth Sciences》2006,408(1):623-626

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Channel water balance of the Lena River Cascade system     

N. E. Kosheleva  E. B. Karabanov  N. S. Kasimov  A. G. Kositskii  V. A. Bychinskii  D. Williams  S. Armstrong 《Doklady Earth Sciences》2006,411(2):1452-1456

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Geodynamic setting of gold ore deposits of the neoproterozoic bodaibo trough     

Academician of the RAS M. I. Kuz’min  V. V. Yarmolyuk  A. I. Spiridonov  V. K. Nemerov  A. I. Ivanov  G. L. Mitrofanov 《Doklady Earth Sciences》2006,407(2):397-400

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New age data on Precambrian volcanic rocks of the khakdon group, eastern Kolyma region     

A. K. Khudoley  V. I. Tkachenko  D. I. Matukov  N. G. Berezhnaya  S. A. Sergeev 《Doklady Earth Sciences》2006,411(2):1357-1361

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Uniform approximation of geophysical fields on a sphere by trigonometric polynomials     

A. V. Frolov  V. I. Tsvetkov 《Doklady Earth Sciences》2006,408(1):682-685

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Platinum-and gold-bearing rodingites of the Ust’-Dep ophiolite block (middle Amur region)     

V. P. Molchanov  L. P. Plyusnina  Corresponding Member of the RAS A. I. Khanchuk  S. S. Zimin  R. A. Oktyabr’skii 《Doklady Earth Sciences》2006,407(1):250-253

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Simulation of the Holocene climate evolution in Northern Africa: The termination of the African Humid Period   总被引：2，自引：0，他引：2  

H. Renssen  V. Brovkin  T. Fichefet  H. Goosse 《Quaternary International》2006,150(1):95

The Holocene climate evolution in Northern Africa is studied in a 9000-yr-long transient simulation with a coupled atmosphere–ocean–vegetation model forced by changes in insolation and atmospheric greenhouse gas concentrations. The model simulates in the monsoonal domains a significant decrease in precipitation under influence of the orbitally forced reduction in summer insolation. In the Western Sahara region, the simulated mid-Holocene transition from humid to arid conditions (the termination of the African Humid Period) is highly non-linear with the occurrence of centennial-scale climate fluctuations due to the biogeophysical feedback between precipitation and vegetation cover. This result is in agreement with proxy data from the Western Sahara region. The other monsoonal regions experience a more gradual climate evolution that linearly follows the insolation forcing, which appears in disagreement with available lake level records.  相似文献