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421.
Discovery and character of the Kunlun-Yellow River Movement 总被引:2,自引:0,他引:2
Based on geomorphological, tectonic and sedimentary data, a Kunlun Yellow River Tectonic Movement has been recognized in 1 10-0 60 Ma B.P. This tectonic movement, which leads to uplift of the Qinghai_Xizang (Tibet) Plateau from 1 500 to 3 000-3 500 m, is periodic, abrupt and changeable in the movement rate of uplifting and slide slipping. 相似文献
422.
A new interpretation of the Himalayan orogenic belt 总被引:2,自引:0,他引:2
423.
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
424.
425.
The range and the nonextinction property of a supercritical superdiffusion and solutions of its corresponding differential
equation are studied. It is pruved that under a suitable condition, the conditioned superprocess of the supercritical superdiffusion
is a subcritical superdiffusion. 相似文献
426.
A recording phase lag between ocean and continent climate changes: Constrained by the Matuyama/Brunhes polarity boundary 总被引:6,自引:0,他引:6
The Matuyama/Brunhes polarity boundary (MBPB) is recorded in Chinese loess L8, which is associated with the glacial period.
It is proved that loess L8 is capable of recording earth’s secular variation, and the lock-in depth in Chinese loess is no
more than that of marine sediments. Comparison with the location of MBPB in Chinese loess and marine sediments, it is put
forward that there is a recording phase lag between ocean and continent climate changes. 相似文献
427.
The development of stamen is an important stage during the sexual reproduction in higher plants. Studying the genes that predominantly
or even specifically expressed in stamens will aid in undestanding the molecular mechanism of stamen development. The structure
of a rice CHS-like gene (D5) which predominantly expressed in anthers has been analysised, showing high structural similarity
with two other anther-specific genes (A1 and BA42) fromBrassica napus. Northern analysis also reveals that the three genes share a similar expression pattern and that the expression of D5 may
relate to the early development of pollens. It is concluded that D5, A1 and BA42 represent a group of diverged CHS-like genes
which are related to stamen development. 相似文献
428.
The smectite to illite transformation in active geothermal systems of New Zealand can be simulated by a first-order reaction
kinetic model, which provides direct estimates about the minumum ages of active geothermal systems themselves. The derived
kinetic values show that the smectite to illite transformation is sensitive to both temperature and time. 相似文献
429.
Fuzzy metric and convergences based on the symmetric difference 总被引:1,自引:0,他引:1
430.
The effect of lanthanum ions on the structural and conformational change of yeast tRNA Phe was studied by 1H NMR. The results suggest that the tertiary base pair (G-15)(C-48), which was located in the terminal in the augmented dihydrouridine helix (D-helix), was markedly affected by adding La 3+ and shifted 0.33 downfield. Based pair (U-8)(A-14), which is associated with a tertiary interaction, links the base of the acceptor stem to the D-stem and anchors the elbow of the L structure, shifted 0.20 upfield. Another imino proton that may be affected by La 3+ in tRNA Phe is the tertiary base pair (G-19)(C-56). The assignment of this resonance is tentative since it is located in the region of highly overlapping resonances between 12.6 and 12.2. This base pair helps to anchor the D-loop to the TΨC loop. 相似文献