Foreword     

Prof. Dr. Hartwig Haubrich 《GeoJournal》1996,39(3):233-233

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Book review     

Dr. Todor Todorov 《Environmental Geology》1992,20(3):233-233

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TS- Creator--Chronostratigraphic data base and visualisation     

Prof. James Ogg Prof. Felix Gradstein 《《幕》》2006,29(1):65-66

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Ziele und erste Ergebnisse der Ökosystemforschung Wattenmeer     

Frau Dr. Maren Kaiser 《Ocean Dynamics》1991,44(5-6):311-319

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Grenzen der Möglichkeiten des Biologischen Effekt Monitoring     

Dr. Volkert Dethlefsen 《Ocean Dynamics》1991,44(5-6):329-340

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The accessibility of a network: The great lakes corridor passenger as an example     

Dr. Abdullah R. Al.-Kandari 《GeoJournal》1986,12(3):255-266

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The star formation history of intermediate-redshift late-type galaxies     

Ignacio Ferreras  Joseph Silk  Asmus Böhm  Bodo Ziegler 《Monthly notices of the Royal Astronomical Society》2004,355(1):64-72

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Pre-collisional high pressure metamorphism and nappe tectonics at active continental margins: a numerical simulation     

Bernhard Stöckhert  Taras V. Gerya 《地学学报》2005,17(2):102-110

The evolution of a subduction channel and orogenic wedge is simulated in 2D for an active continental margin, with P-T paths being displayed for selected markers. In our simulation, subduction erosion affects the active margin and a structural pattern develops within a few tens of millions of years, with four zones from the trench into the forearc: (i) an accretionary complex of low grade metamorphic sedimentary material, (ii) a wedge of nappes with alternating upper and lower crustal provenance, and minor interleaving of oceanic or hydrated mantle material, (iii) a megascale melange composed of high pressure (HP) and ultra-high pressure (UHP) metamorphic rocks extruded from the subduction channel, and (iv) the upward tilted frontal part of the remaining lid. The P–T paths and time scales correspond to those typically recorded in orogenic belts. The simulation shows that HP/UHP metamorphism of continental crust does not necessarily indicate collision, but that the material can be derived from the active margin by subduction erosion and extruded from the subduction channel beneath the forearc during ongoing subduction.  相似文献   

A study of the Equatorial Atlantic currents using historical moored data     

Dr. Alexander B. Polonsky  Dr. Evgeniy G. Nikolaenko  Dr. Sekou Konate  Dr. Toumany Camara 《Ocean Dynamics》1993,45(4):219-254

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Late Quaternary vegetation changes around Lake Rutundu,Mount Kenya,East Africa: evidence from grass cuticles,pollen and stable carbon isotopes     

Dr M. J. Wooller  D. L. Swain  K. J. Ficken  A. D. Q. Agnew  F. A. Street-Perrott  G. Eglinton 《第四纪科学杂志》2003,18(1):3-15

Woody, subalpine shrubs and grasses currently surround Lake Rutundu, Mount Kenya. Multiple proxies, including carbon isotopes, pollen and grass cuticles, from a 755‐cm‐long core were used to reconstruct the vegetation over the past 38 300 calendar years. Stable carbon‐isotope ratios of total organic carbon and terrestrial biomarkers from the lake sediments imply that the proportion of terrestrial plants using the C₄ photosynthetic pathway was greater during the Late Pleistocene than in the Holocene. Pollen data show that grasses were a major constituent of the vegetation throughout the Late Pleistocene and Holocene. The proportion of grass pollen relative to the pollen from other plants was greatest at the last glacial maximum (LGM). Grass cuticles confirm evidence that C₄ grass taxa were present at the LGM and that the majority followed the cold‐tolerant NADP‐MEC₄ subpathway. Copyright © 2003 John Wiley & Sons, Ltd.  相似文献