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yangtze
Affecting factors of preferential flow in the forest of the Three Gorges area, Yangtze River
      
In order to study the factors affecting preferential flow, a 2.9 m-long, 2.6 m-deep soil profile was dug in the Quxi watershed, Yangtze River.
      
Particularly, rugose coral fauna of the Sifengya Formation represent early Telychian rugosan fauna in the Upper Yangtze region and improve the sequences of early Silurian (Llandovery) rugose coral assemblages in Yangtze region.
      
In this study, thirty-six individuals of Acheilognathus macropterus were collected from the Heilongjiang River, the Yangtze River, and the Nandujiang River.
      
The samples from the Yangtze River scattered into clades 2, 3, and 4.
      
Nd model ages are between 1.6 Ga and 2.4 Ga, which are very similar to those of the Yangtze craton, South Qinling and North Qinling belts and quite different from those of the North China craton.
      
Therefore, provenance of the sedimentary rocks in the Ganzi-Songpan block and Longmen Mountains was the Yangtze craton and/or the Qinling orogen, which evolved on the basis of the Yangtze craton.
      
The correlation between provenances and tectonostratigraphic strata of the western Yangtze craton shows that the source materials should be primarily from Neoproterozoic.
      
Molybdenum isotope composition from Yangtze block continental margin and its indication to organic burial rate
      
Although the two sets of data gained through different geochemical records in the Yangtze block show a deviation of one order of magnitude, they do display a strong correlation.
      
Northeast Sichuan basin is a Mesozoic-Cenozoic basin in the northern margin of the Yangtze plate which has a complex tectonic background and hydrocarbon accumulation history.
      
Oil geologic anomaly in the north edge of the Middle and Lower Yangtze areas based on the evidence weight method
      
Domestic varieties (except Xingguo red carp) showed less genetic diversity than the Yangtze River wild common carp in terms of allelic diversity.
      
Population differentiation was assessed and each combination of populations displayed significant differentiation (P >amp;lt; 0.05) with the exception of that between the Yangtze River wild common carp and Xingguo red carp.
      
Hydrological Regime and Morphodynamics of the Yangtze River Mouth Area
      
The features of the hydrological regime, modern morphological structure, fluviomorphological processes, and the history of formation of the Yangtze River mouth area are discussed.
      
The influence of the huge river water and sediment runoff and tides on the hydrological and morphological processes in the Yangtze River mouth is shown.
      
The possible impact of construction of the large waterworks "Three Gorges" on the hydrological and morphological processes in the Yangtze River mouth is roughly evaluated.
      
The proposed method is applied to water environment and environment quality evaluation of the Hang Jiang River, a major branch of the Yangtze River, in China.
      
cheni (Nichols, 1931) described from the Yangtze and not mentioned in literature for a long time.
      
 

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