2012 Vol. 32 No. 6
Grain size distribution and end-member-modeling algorithm analysis (EMMA) were conducted for the 117 bottom sediments taken from the radial sand ridge field (RSRF) of the South Yel...
2012, 32(6): 1-8.
Suspended sediment concentration (SSC), as the basis for sediment flux balance, is an important parameter in marine sedimentology. Based on the survey and hydrological observations...
2012, 32(6): 9-15.
Modern sedimentation rates for 16 cores recovered from the Beibu Gulf were measured with the 210Pb method. The results show that there are 3 types of 210Pb vertical distribution pa...
2012, 32(6): 17-26.
According to the data collected from drilling holes and tidal current observations, using numerical simulation methods, the environmental capacity for sea sand mining is studied in...
2012, 32(6): 27-34.
The South China Sea is located at a juncture among the Eurasian, the Indian-Australian and the Pacific plates, being the largest continental marginal sea along the East Asian conti...
2012, 32(6): 35-53.
The South China Sea was formed in Cenozoic. Basins in the South China Sea could be divided into different types, such as continental shelf basins, continental slope basins and deep...
2012, 32(6): 55-78.
There are a lot of Cenozoic basins from west to east in the northern margin of the South China Sea, including the Beibu Gulf, the Qiongdongnan, the Pearl River Mouth and the Taixin...
2012, 32(6): 79-93.
A series of medium and small-scale Cenozoic sedimentary basins are developed in the western South China Sea.They are, from north to south, the Yinggehai, the Zhongjiannan, the Wan'...
2012, 32(6): 95-111.
There are many small and medium-sized Cenozoic sedimentary basins in the southern South China Sea, such as the Nanweixi Basin, the Beikang Basin, the Liyue Basin, the Zengmu Basin,...
2012, 32(6): 113-127.
The east part of the South China Sea is located at the convergence zone between the Eurasian Plate and the Pacific Plate (the Philippine Sea Plate). To the east of the South China ...
2012, 32(6): 129-147.
A climatic proxy system is constructed on the basis of the color reflectance data of the core MZ01 using first derivative and factors analysis method, and a high-resolution climati...
2012, 32(6): 149-158.
In the Dongying Sag, reservoirs were formed in different pressure systems.The geochemical heterogeneity of hydrocarbons in the reservoir could be affected by hydrocarbon migration ...
2012, 32(6): 159-164.
Two sediment cores were recovered from the Bosten Lake in order to investigate the changes in both the lake system and source of organic materials during the last 200 years.Based o...
2012, 32(6): 165-171.
The Qianliyan fracture, located in the south of the Qianliyan uplift, is the boundary fault between the north depression and the Qianliyan uplift as a major fault controlling the f...
2012, 32(6): 173-178.
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