Further analysis of the region of permissible motion in the problem of three bodies     

Sun Yi-sui  Luo Ding-jun 《Chinese Astronomy and Astrophysics》1981,5(3):247-254

In this paper we investigate the range of variation of the orbital inclination I between two bodies in the problem of three bodies. We give the conditions to determine whether the two bodies move in the same or opposite senses and give the maximum and minimum values of I when the three bodies are in collinear positions. We prove that the range of variation of I must attain maximum and minimum values when the bodies are collinear.  相似文献   

Early stage differentiation of thallus cells ofPorphyra haitanensis (Rhodophyta)   总被引：1，自引：0，他引：1  

Wang Sujuan  Sun Yunlong  Lu Anming  Wang Guangyuan 《中国海洋湖沼学报》1987,5(3):217-221

The early stage differentiation of thallus cells ofPorphyra haitanensis T. J. Chang et B. F. Zheng was studied. Protoplasts or single cells were isolated from the blades using enzyme mixture comprising 2% sea snail gut enzyme and 1% cellulase. The isolated protoplasts or single cells were incubated in the MES medium. The cell differentiations were examined under the microscope at intervals after incubation. Four types of cell differentiation, namely, normal, abnormal, carposporangial and spermatorangial, and rhizoidal types, were observed. Since normal cell differentiations occur mostly in small thalli 50 mm in length and middle portions of big thalli 200 mm in length, it is essential to select tissues from these two kinds of thalli essential for commercial production.  相似文献   

A tidal three-dimensional nonlinear model with variable eddy viscosity (I)—A dynamic model     

Feng Shizuo  Sun Wenxin 《中国海洋湖沼学报》1983,1(2):166-170

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Strongly peraluminous granites of Mesozoic in Eastern Nanling Range,southern China: Petrogenesis and implications for tectonics   总被引：17，自引：5，他引：12  

SUN Tao  ZHOU Xinmin  CHEN Peirong  LI Huimin  ZHOU Hongying  WANG Zhicheng & SHEN Weizhou Department of Earth Sciences  Nanjing University  Nanjing  China  Tianjin Institute of Geology  Mineral Resources  China Geological Survey  Tianjin  China 《中国科学D辑(英文版)》2005,48(2):165-174

The strongly peraluminous granites (SPGs) of Eastern Nanling Range (ENR) are a characteristic of all bearing highly aluminous minerals, such as muscovite±AI-rich biotite±tourmaline±garnet, and lack of cordierite. In respect of petrography, geochemistry, Nd isotope, and single grain zircon U-Pb dating, the representative granite bodies of them are studied. The research shows that these granites were emplaced in two stages, namely 228-225 Ma BP and J2-3 159-156 Ma BP, belonging to Indosinian and early Yanshanian periods, respectively, and they have low εNd(t) values (-10.6--11.1), high A/CNK, Rb/Sr ratios and tDM values (1887-1817 Ma), and REE's tetrad effect (TE1,3=1.13-1.34). In comparison with related geology, petrology and chronology of granites in adjacent regions, it is suggested that Indosinian SPGs of ENR formed in the circumstance of post-collisional extension 20 Ma after the major collision of Indosinian Movement (258-243 Ma BP) in Indo-China Peninsula, and early Yanshanian SPGs formed in the  相似文献   

Magma underplating and Hannuoba present crust-mantle transitional zone composition: Xenolith petrological and geochemical evidence   总被引：7，自引：0，他引：7  

FAN Qicheng    ZHANG Hongfu  SUI Jianli  ZHAI Mingguo  SUN Qian & LI Ni . Institute of Geology  Geophysics  Chinese Academy of Sciences  Beijing  China  . Institute of Geology  China Seismological Bureau  Beijing  China 《中国科学D辑(英文版)》2005,48(8):1089-1105

Studies on the deep-seated xenoliths from global volcanoes reveal that the present petrological crust-mantle boundary between the lower crust and the upper mantle actually is a transitional layer from mainly mafic granulites to ultramafic spinel lher-zolites[1,2], i.e. a transitional zone distinctive from the seismological Moho[3]. Oceanic lithosphere crust- mantle transitional zone can be established from the study on the exposed ophiolites. However, as for the continental lithosphere, since …  相似文献   

Phytoplankton succession during a red tide of Skeletonema costatum in Jiaozhou Bay of China   总被引：5，自引：0，他引：5  

Liu D  Sun J  Zou J  Zhang J 《Marine pollution bulletin》2005,50(1):91-94

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A high resolution forecast model of storm surge inundation     

LIUJuan JIANGWensheng SUNWenxin WANGYongzhi 《中国海洋大学学报(英文版)》2005,4(2):108-114

In order to forecast storm surge inundation, a two-dimensional model is established. In the model, an alternating computation sequence method is used to solve the governing equations, and the dry and wet method is introduced to treat the moving boundary. This model is easy to use. It has a friendly input interface and Arcview GIS is used as the output interface. The model is applied to the Shantou area to simulate the storm surge elevations and inundations caused by Typhoons 6903 ane 0104 using the same relevant parameters. The calculated results agree well with the observations.  相似文献   

A note on MESA and spectral analysis of the hundred-year geomagnetic data at Zo-se   总被引：1，自引：0，他引：1  

Wang Ding-yi  Sun Wei  Tschu Kang-kun 《Geophysical Journal International》1982,71(2):275-283

Summary. In the maximum entropy spectrum analysis (MESA) of geomagnetic data, the required order can be estimated by the zero-frequency half-power width (ZHW) minimum method proposed in this paper. The spectra of the data for 1876–1975 at Zo-se showed a period of 40yr, in addition to the well-known periods. The amplitudes of the variations were estimated with parabolic-sinusoidal series fitting.  相似文献   

新疆精河莱历斯高尔铜钼矿床原生地球化学异常     

孙继东  王崇礼  于风池 《地球科学与环境学报》1992,(4)

矿区处于博罗霍洛山主脊,属斑岩型铜钼矿床。斑岩体本身为矿体,钼矿在岩体内,铜矿在外接触带。通过矿区北部勘查地球化学工作表明,Mo、Cu、Pb、Ag、As原生地球化学异常规模大、连续性好,形态规则,梯度大。As、Sb、Ag具前缘特征。除Mo、Cu外,Pb、Ag具主成矿元素特征。原生异常纵向分带具轴向分带特征,分带序列有一定的典型意义。从地质、地球化学异常特征、小岩体地球化学特征以及金属预测资源初步计算认为该矿床很有远景。  相似文献   

Palynological record during the Pleistocene (between 1.05 Ma and 0.36 Ma) from ODP1144, northern South China Sea     

HUANG Fei & SUN XiangjunInstitute of Geology  Paleontology  Chinese Academy of Sciences  Nanjing  China  Institute of Botany  Chinese Academy of Sciences  Beijing  China  Key Laboratory of Marine Geology  Ministry of Education  Tongji University  Shanghai  China Correspondence should be addressed to Huang Fei 《中国科学D辑(英文版)》2004,47(1):30-36

This paper presents the pollen record from the lower section of ODP1144 (depth 501.3-225.7 m, ca. 1.05-0.36 Ma). Two pollen zones (PA and PB) and eleven pollen subzones are recognized. Within zone PB, the 11 pollen subzones (PB21-11) are defined according to the pine, fern and herb variations, and are equivalent to the marine isotope stages 21-11 (MISs 21-11). The interglacial periods are typified by an increase in pine pollen and fern spores, and a decrease in herbaceous pollen, while the patterning during the glacial periods is just the opposite. During the interglacial periods, pollen assemblages were dominated by pine similar to those of the present day, suggesting that the paleoenvironment of the interglacial periods was similar to that of the present day, whereas the glacial periods are marked by an increase in herbaceous pollen, mainly Gramineae and Cyperaceae, indicating that grassland covered the exposed continental shelf when sea level declined. Increased Artemisia percentages and the highest  相似文献