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261.
Genomic organization of EDSV strain AA-2 总被引:1,自引:0,他引:1
Liyu Zeng Qi Jin Jinggang Zhang Maoxiang Li Hong Li Lei Zhu Zhen Yin Yunde Hou 《科学通报(英文版)》1998,43(7):594-594
The genomic organization of egg drop syndrome virus strain AA-2 isolated in China is reported here. The genome was found to be 32 838 bp in length, approximately 2 kb shorter than those of the human subgenus C adenoviruses. Analysis of open reading frames indicated that the genes for major viral structural proteins (55 K, Penton base, pⅦ, pⅩ, pⅥ, Hexon, 100 K, pⅧ and Fiber), as well as EP, DNA polymerase and ⅣaⅡ are present in the expected locations in the genome. EDSV possesses no identifiable E3 and E4 regions and most proteins encoded by E3 and E4 regions of other adenoviruses genome were not presented in EDSV. 相似文献
262.
Under 2 100 bar of hydrostatic pressure, KNA N-glycosidase can still cleave the N-C bond of adenosine at position 4324 in
R/S domain of 28S RNA in rat ribosome, demonstrating that high pressure has no effect on the tertiary structure of S/R domain. 相似文献
263.
A new interpretation of the Himalayan orogenic belt 总被引:2,自引:0,他引:2
264.
Discovery of eclogite at northern margin of Qaidam Basin, NW China 总被引:19,自引:0,他引:19
Jingsui Yang Zhiqin Xu Haibing Li Cailai Wu Junwen Cui Jianxin Zhang Wen Chen 《科学通报(英文版)》1998,43(20):1755-1755
Eclogite was first discovered at the northern margin of the Qaidam Basin in this study. It occurs as pods in the gneiss sequence of Middle to Upper Proterozoic age and is mainly composed of garnet, omphacite, phengite and rutile. The garnets contain 44%-62% of almandine, 15%-33% of grossular and 12%-30% of pyrope molecules, and the omphacites contain 40%-46% of jadeite. Applying garnet_clinopyroxene thermometry and jadeite geobarometry, the peak conditions of eclogite facies metamorphism occurred at about (722±123)℃ and at the pressure of up to c. 22 ×10 8 Pa. 相似文献
265.
An initial attempt reveals parameters of marked electric synapse on AP perceptive neuron of leech. The width of gap between
marked AP and either neuro-or glio-process is 2–3 nm, the diameter of the hexagonal array of connexion is 8–9 nm with a central
pole of 2–2.5 nm, the same as the structure of annular lamellar bodies internalized by AP-glia processes in the AP. 相似文献
266.
Jianguo Ren Xianbin Wang Jianfa Chen Chunyuan Li Hui Yang Ziyuan Ouyang 《科学通报(英文版)》1998,43(9):761-761
The isotopic cumpositions of helium have been investigated in hot spring gases sampled from the Liaodong Peninsula. China.
The3He/4He ratios range from 0.14 Ra (0.14 times the atmospheric3He/4He ratio of 1.40 × 10-6 to 0.72 Ra.3He/4He versus4He/20Ne ratios and He contents suggest that a small amount of mantle-derived helium reaches the earth’s surface. Helium iwtope
ratios of the hot spring gases show a distribution pattern similar to the regional heat flow values, indicating that the positive
thermal anomaly occurring in the rtrea is closely associated with the presence of mantle-derived helium. The observations
described above provide some significant evidence that the molten magma originating from partial melting of the upper mantle
may have intruded into the continental crust along the activity fault. The coupling of the presence of mantle He and heat
flow anomalies to seismic activity in studied region seem to imply that there is an internal relationship between mantle degassing
and seismic activity. 相似文献
267.
Fuzzy metric and convergences based on the symmetric difference 总被引:1,自引:0,他引:1
268.
A type of recurring relations on syndrome series is presnted. After some important theorems are established, an algorithm for computing a minimal polynomial set is presented. Finally an algorithm for determining the unknown syndromes with incorporating α majority scheme is presented. 相似文献
269.
Determination of tectonic background for sedimentary basin from sandstone geochemistry 总被引:2,自引:0,他引:2
The chemical composition of sedimentary rocks is mainly controlled by source rocks. Through examining chemical composition
of terrigenous rocks, the tectonic evolution of a sedimentary basin can be modeled. The Turpan Basin belongs to a continental
sedimentary basin and its source rocks are derived from the upper continental crust. 相似文献
270.