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411.
The Juancheng chondrite, a new meteorite falling recently in Juancheng County, Shandong Province, China, is classified as an H5 (S2) chondrite based on the compositions of olivine (Fa= 19.2, σ Fa=0.46) and low-Ca pyroxene (Fs=16.9, σ Fa=0.4). The plagioclase in the Juancheng chondrite is rich in CaO, indicating a relatively high metamorphic temperature the parent body underwent. 相似文献
412.
The relaxation of the highly vibrationally excited CO (v = 1–8) by CO2 is studied by timeresolved Fourier transform infrared emission spectroscopy (TR FTIR). 193 nm laser photolysis of the mixture
of CHBr3 with O2 generates the highly vibrationally excited CO(v) molecules. TR FTIR records the intense infrared emission of CO(v→v-1). The
vibrational populations of each level of CO(v) have been determined by the method of spectral simulation. Based on the evolution
of the time resolved populations and the differential method, 8 energy transfer rate constants of CO(v = 1–8) to CO2 molecules areobtained: (5.7±0.1), (5.9±0.1), (5.2±0.2), (3.4±0.2), (2.4±0.3), (2.2±0.4), (2.0±0.4) and (1.8±0.6) (1014 cm3 · molecule−1 · s−1), respectively. A two-channel energy transfer model can explain the feature of the quenching of CO(v) by CO2. For the lower vibrational states of CO, the vibrational energy transfers preferentially to the u3 mode of CO2 For the higher levels, the major quenching channel changes to the vibrational energy exchange between CO(v→v-1) and the u1 mode of CO2. 相似文献
413.
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
414.
High-precision timing of the Quaternary standard samples with thermal ionization mass spectrometry (TIMS) U-series method 总被引:2,自引:0,他引:2
Peng Zicheng Wang Zhaorong Sun Weidong Ma Zhibang Xia Ming Zhang Chenhui Chen Wenji Zhang Zhonglu An Zhisheng 《科学通报(英文版)》1998,43(4):333-333
Two national stalagmite standard (GBW04412, GBW04413) and one international coral standard (RKM_4) have been determined by using thermal ionization mass spectrometry (TIMS) method. The values of ( 234 U/ 238 U) act , ( 230 Th/ 234 U) act and age are all consistent in error range with the standard values obtained by using α spectrometry. 相似文献
415.
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
416.
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
417.
Osmium isotope determination on mantle-derived peridotite xenoliths from Panshishan with N-TIMS 总被引:2,自引:0,他引:2
Weidong Sun Zicheng Peng Xiachen Zhi Daogong Chen Zhaorong Wang Xinhua Zhou 《科学通报(英文版)》1998,43(7):573-573
The187Os/188Os ratios of spinel lherzolite xenoliths from Panshishan determined with N-TIMS are lower than that of the primitive mantle,
which shows depleted mantle characteristics. Their positive correlation with Al2O3/MgO suggests that the geochemical behavior of trace elements Re and Os is similar to that of Al2O3 and MgO respectively during the magmatic evolution and Re-Os isotopic system is largely immune to mantle metasomatism. A
model age of 2.8–3.4 Ga obtained by187Os/188Os-Al2O3/ MgO correlation might represent the homogeneous age of the mantle lithosphere beneath the area. 相似文献
418.
New evidence for the Qinghai-Xizang (Tibet) Plateau as a pilot region of climatic fluctuation in China 总被引:12,自引:1,他引:11
Over 40 a observed temperature data in 172 stations in China and historical proxy data were analyzed. Evidence suggested that
during 1980–1994, the warmest year appeared first in southeastern part of the Qinghai-Xizang (Tibet) Plateau (henceforth SETP)
and then gradually spread northwards and eastwards to eastern China. The climatic change on century time scale in recent 600
a shows 3 relatively warm and clod stages in China. Each warm and cold stage appeared first in Tibet Plateau (henceforth TP)
and then in the Qilian Mountains, then in the eastern parts of China. The warm and cold stages in TP were 10–60 a earlier
than in the eastern China. The facts show that TP is a pilot region of climatic fluctuation in China on the time scale shorter
than 103a. 相似文献
419.
The vibrational energy transfer from highly vibrationally excited CO to H2O molecules is studied by time-resolved Fourier transform infrared emission spectroscopy (TR FTIR). Following the 193 nm laser
photolysis of CHBr3 and O2 the secondary reactions generate CO(v). The infrared emission of CO(v → v−1) is detected by TR FTIR. The excitation of H2O molecules is not observed. By the method of the spectral simulation and the differential technique, 8 rate constants for
CO(v)/H2O system are obtained: (1.7 ±0.1), (3.4 ±0.2), (6.2 ±0.4), (8.0 ±1.0), (9.0 ±2.0), (12 ±3), (16 ±4) and (18 ±7) (1013cm3 · molecule-1· s-1). At least two reasons lead to the efficient energy transfer. One is the contributions of the rotational energy to the vibational
energy defect and the other is the result of the complex collision. With the SSH andab initio calculations, the quenching mechanism of CO(v) by H2O is suggested. 相似文献
420.