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521.
Chemical structure of immature sulfur-rich kerogen and composition of immature sulfur-rich crude oil in Jianghun oil field
have been studied. In molecular level, crude oil differs from thermolysed and chemolysed products of kerogen but does resemble
the bitumen in immature sulfur-rich source rock. Therefore, immature sulfur-rich oil may be derived from the expelling of
bitumen rather than from thermal cracking of kerogen. 相似文献
522.
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
523.
A new interpretation of the Himalayan orogenic belt 总被引:2,自引:0,他引:2
524.
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
525.
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
526.
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
527.
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
528.
Fuzzy metric and convergences based on the symmetric difference 总被引:1,自引:0,他引:1
529.
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
530.
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