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8篇 您的检索式:作者名="Cheng Fengjun"
    题名 作者 年代 出处 被引量
1Microstructure of Fe TiC surface composite produced by cast-sintering显示文摘CHENG Fengjun WANG Yisan 2007Materials Letters2007,61,7:1
2Microstructure and wear properties of Fe-VC-CrTC3 composite coating on surface of cast steel 显示文摘Cheng Fengjun Wang Yisan Yang Tinggui 2008Materials Characterization2008,59,4:1
3Microstructure of Fe–TiC surface composite produced by cast-sintering显示文摘Cheng Fengjun Wang Yisan 2006Materials Letters2006,,7:1
4E-mulsion and macromolecules templated alginate based polymer microspheres显示文摘Zhang Fengjun Cheng Guoxiang Ying Xiaoguang 0,,07:1
5Microstructure and wear properties of Fe-VC-Cr7C3 composite coating on surface of cast steel 显示文摘Cheng Fengjun Wang Yisan Yang Tinggui 2008Materials Characterization2008,59,:1
6Microstructure of Fe-TiC surfacecomposite produced by cast-sintering显示文摘Cheng Fengjun Wang Yisan 2007Materials Letters2007,61,:1
7Preliminary study of 0.14 THz water surface clutter reflectivity at near vertical incidence angle显示文摘As the development of radar systems developed for the terahertz and higher millimeter region continues to grow, the interest in the water surface and land clutter at terahertz and higher millimeter frequencies continues to increase. An empirical model of sea clutter reflectivity is described firstly, which is valid at near vertical incidence and has small average absolute deviation compared to other empirical models. Simulated results of 0.14 THz sea clutter at near vertical incidence with thismodel are shown. An indoor test-bed is constructed in order to measure 0.14 THz water surface clutter reflectivity and an experiment is carried out. Initial experimental results are presented and compared to the simulation results, which partially verifies that the empirical sea clutter model still works at 0.14 THz.AN Jianfei CHENG Binbin FENG Zheng CUI Zhenmao CHEN Fengjun LU Bin 2017太赫兹科学与电子信息学报2017,15,2:0
8New understanding and exploration direction of hydrocarbon accumulation in Termit Basin, Niger显示文摘Based on the seismic and drilling data, casting thin sections, geochemical analysis of oil and rock samples, and hydrocarbon generation history simulation, the hydrocarbon accumulation characteristics and exploration direction of Termit superimposed marine–continental rift basin are discussed. The Termit basin is superimposed with two-phase rifts(Early Cretaceous and Paleogene). The subsidence curves from two wells on the Trakes slope in the east of the basin show high subsidence rate in the Late Cretaceous, which is believed to be high deposition rate influenced by transgression. However, a weak rift may also be developed. The depositional sequences in the Termit basin were controlled by the Late Cretaceous marine transgression cycle and the Paleogene lacustrine transgression cycle, giving rise to two types of superimposed marine–continental “source-sink” deposits. The marine and continental mixed source rocks developed universally in the whole basinduring the marine transgression period, and are overlaid by the Paleogene Sokor 1 reservoir rocks and Sokor 2 caprocks developed during the lacustrine transgression period, forming the unique superimposed marine–continental basin in WCARS. The early low geothermal gradient in the Termit basin resulted in the late hydrocarbon generated by the source rock of Upper Cretaceous Yogou in Paleogene. Mature source rock of Upper Cretaceous Donga developed in the Trakes slope, so that the double-source-supply hydrocarbon and accumulation models are proposed for the Trakes slope in which formed the oil fields. Due to virtue of the newly proposed hydrocarbon accumulation model and the exploration activities in recent years in the Termit superimposed marine–continental rift basin, an additional effective exploration area of about 2500 km2has been confirmed in the east of the basin. It is believed that potential domains such as Sokor 1, Donga and Upper Cretaceous lithologic traps in the southeast of the basin are key expected targets for exploration and frontier evaluation in future.YUAN Shengqiang DOU Lirong CHENG Dingsheng MAO Fengjun PAN Chunfu ZHENG Fengyun JIANG Hong PANG Wenzhu LI Zaohong 2023Petroleum Exploration and Development2023,50,2:0
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