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951.
北祁连中西段发育三套早古生代蛇绿岩及相应的基性、超基性岩,呈北、中、南三条带状分布。区内金的活化、迁移主要受控于超基性岩带和与其分布近于一致的两条韧性剪切带,金矿化主要发生在强蚀变超基性岩体内、岩体与围岩接触带、断裂破碎蚀变带内。根据包裹体测温及成分测定、稳定同位素特征资料及超基性岩中金丰度值等分析,金矿物质主要来自超基性岩,流体来源于深部,其成因属与超基性岩有关的韧性剪切带型金矿床。 相似文献
952.
本文利用COS-B和HEAO-B卫星资料对Geminga脉冲星进行了守时性分析和谱分析,结果进一步证实了Geminga脉冲星是一颗具有强γ辐射,弱X辐射的γ射线脉冲星. 相似文献
953.
南海区多鱼种声学评估工作程序 总被引:3,自引:0,他引:3
总结了利用SimradEK50 0声学系统进行了南海区多鱼种资源评估经验 ,介绍了多鱼种声学评估的工作流程 ,包括调查方案制定、声学数据采集、映像分析、积分值分配、资源量的计算方法等关键过程 ,同时及在工作中应该注意的细节。 相似文献
954.
A preliminary application GIS in glaciological research along the traverse route from Zhongshan Station to Dome A, Antarctica 总被引:1,自引:0,他引:1
1 IntroductionGeographicalinformationsystem (GIS)isanefficientwayandimportanttechniquetomanage,displayandanalyzeAntarcticspatialdata.GIScanbeusedtomakeandre newmapproductsquickly ,evaluateenvironment,supportlogisticmanagementandfieldoperation,providechancetoextractnewknowledge,andtopromoteinformationex changeamongnationsunderthedemandoftheMadridProtocol(AADC 2 0 0 1 ;MAGIC1 998;1 999) .WorkingGroupofGeodesyandGeographicInformation (WG GGI)ofScientificCommitteeonAntarcticResearch (… 相似文献
955.
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
956.
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
957.
958.
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
959.
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