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| 1 | Study of Furoxan Derivatives for Energetic Applications显示文摘二新奇精力充沛的混合物, 3,4 二度(1,2,4-triazole-3-yl ) furoxan (BTAF ) 和 3,4 二度(1-nitro-1,2,4-triazole-3-yl ) furoxan (BNTAF ) ,被准备,他们的结构被红外, 1H NMR, 13C NMR, MS 技术和元素的分析描绘。BTAF 和 BNTAF 的性质被估计。BTAF 的预言的性能数据如下:密度(测量) 是 1.75 g/cm3,氮内容 50.9% ,形成 +419.7 kJ/mol 的爆炸速度 7277 m/s,爆炸压力 20.1 GPa 和热含量。BNTAF 的预言的表演数据如下:密度是 1.84 g/cm3,氮内容 45.2% ,形成 +841.5 kJ/mol,爆炸速度 8490 m/s 和爆炸压力的热含量 32.4 GPa。BTAF 和 BNTAF 的主要 themal 性质被 DSC 和 TG 技术分析,结果证明 BTAF 在 188.8 攠桸扩瑩摥栠杩 ? 敳敬瑣癩瑩 ? 湡 ? 湡楴楤瑳牵慢据 ? 潦 ? 敆 ? 愠潭杮攠癮物湯敭瑮污祬爠汥癥湡 ? 敭慴? 潩獮椠 ? 煡敵畯 ? 与伴随物分解融化敭楤? 吠敨洠瑥潨 ? 景 ? 扯猧瀠潬 ? 湩楤慣整 ? 桴 ? 潦浲瑡潩 ? 景ㄠ呼挠浯汰硥戠瑥敷湥 ? 愠摮吗?? | Yanan Li Zhizhong Zhang Zhongxue Ge BozhouWang Weipeng Lai Yifen Luo | 2013 | Chinese Journal of Chemistry2013，31，4： | 10 |
| 2 | Cooperation of invariant NKT cells and CD4+CD25+ T regulatory cells in prevention of autoimmune diabetes in non-obese diabetic mice treated with α- galactosylceramide显示文摘 | Weipeng Li Fang Ji Yong Zhang Ying Wang Neng Yang Hailiang Ge Fuqing Wang | 2008 | Acta Biochimica et Biophysica Sinica2008，40，5： | 5 |
| 3 | CTCs Detection and Whole-exome Sequencing Might Be Used to Differentiate Benign and Malignant Pulmonary Nodules显示文摘Background and objective Low-density computed tomography(LDCT)improved early lung cancer diagnosis but introduces an excess of false-positive pulmonary nodules data.Hence,accurate diagnosis of early-stage lung cancer remains challenging.The purpose of the study was to assess the feasibility of using circulating tumour cells(CTCs)to differentiate malignant from benign pulmonary nodules.Materials and methods 122 patients with suspected malignant pulmonary nodules detected on chest CT in preparation for surgery were prospectively recruited.Peripheral blood samples were collected before surgery,and CTCs were identified upon isolation by size of epithelial tumour cells and morphological analysis.Laser capture microdissection,MALBAC amplification,and whole-exome sequencing were performed on 8 samples.The diagnostic efficacy of CTCs counting,and the genomic variation profile of benign and malignant CTCs samples were analysed.Results Using 2.5 cells/5 m L as the cut-off value,the area under the receiver operating characteristic curve was of 0.651(95%confidence interval:0.538-0.764),with a sensitivity and specificity of 0.526 and 0.800,respectively,and positive and negative predictive values of 91.1%and 30.3%,respectively.Distinct sequence variations differences in DNA damage repair-related and driver genes were observed in benign and malignant samples.TP53 mutations were identified in CTCs of four malignant cases;in particular,g.7578115T>C,g.7578645C>T,and g.7579472G>C were exclusively detected in all four malignant samples.Conclusion CTCs play an ancillary role in the diagnosis of pulmonary nodules.TP53 mutations in CTCs might be used to identify benign and malignant pulmonary nodules. | Changdan XU Xiaohong XU Weipeng SHAO Hongliang SUN Xiaohong LIU Hongxiang FENG Xianbo ZUO Jingyang GAO Guohui WANG Xiongtao YANG Runchuan GU Shutong GE Shijie WANG Liwei GAO Guangying ZHU | 2023 | 中国肺癌杂志2023，26，6： | 1 |
| 4 | Late Quater- nary slip rate of the South Heli Shan Fault (northern Hexi Corri- dor, NW China) and its implications for northeastward growth of the Tibetan Plateau显示文摘 | Zheng Wenjun Zhang Peizheng Ge Weipeng | 2013 | Tectonics2013，32，2： | 1 |
| 5 | Discovery of the Surface Rupture Zone on the South of Helishan in Gaotai,Gansu Province显示文摘According to a new investigation in the northern Hexi corridor,the remains of two surface rupture zones were discovered on the southern margin fault of the Helishan. One rupture has a length of approximately 7km and the other 10km. The two surface rupture zones might have been produced by the latest earthquake event. On the surface rupture is continuous scarp and free face caused by the rupture. The scarp is about 1 ~ 1. 5m high and on some sites,nearly up to 2m. According to the OSL results,the latest T1 terrace and higher flood plain forming in 3000a B. P. are dislocated by the fault. The above reveals the rupture age to be later than the T1 terrace. However,in the historical data and earthquake catalogue,we didn't find related information about the fault and surface rupture in this area. The 180 A. D. Biaoshi M8. 0 earthquake and the 756 A. D. Zhangye-Jiuquan M7. 0 earthquake are documented in historical data. It is inferred by textual research that the two earthquakes are related to the northern marginal fault of Yumushan in the south of the basin. Due to a lack of reliable evidence,there are still many arguments on this inferred conclusion. Thus we hold that the two surface rupture zones were produced by one of the two large earthquakes or other unrecorded historical event. The research on the activity and surface rupture of this fault can offer valuable information for the tectonic study and strong earthquake risk estimates of this region in the future. | Zheng Wenjun Zhang Peizhen Yuan Daoyang Ge Weipeng Liu Jianhui | 2010 | Earthquake Research in China2010，24，1： | 1 |
| 6 | Textual Research on the Historical Data of the 1573 AD Minxian Earthquake in Gansu Province and Discussion on Its Seismogenic Structure显示文摘According to the detailed study of the historical earthquake records and causative structure of the Minxian M6(1/2) earthquake in 1573 {A.D.}, we have found that the most grievous disaster area lies nearby the Minxian county seat (Minzhou county at that time). So, we have identified the extremely seismic area of the 1573 {A.D.} The Minxian M6(1/2) earthquake was located in Minxian city, the intensity of the meizoseismal region is Ⅷ~Ⅸ, the epicenter is 34.4°N, 104.0°E, the location precision is Ⅱ and the deviation of location is less than or equal to 25km. Tectonically, this area lies in the transition region of stress transfer and structural transform between the east Kunlun fault and the northern margin of the west Qinling fault. The differential activity of the Lintan-Dangchang fault zone is obvious, and only parts of the segment put up Holocene activity. There are landslides and rock bursts of different sizes in the meizoseismal region. By integrated analysis, we conclude that the Minxian-Dangchang segment of the Lintan-Dangchang fault is the seismogenic structure of the 1573 A.D. M6(1/2) Minxian earthquake, in Gansu Province. | Zheng Wenjun Lei Zhongsheng Yuan Daoyang He Wengui Ge Weipeng LiuXingwang | 2007 | Earthquake Research in China2007，21，4： | 0 |
| 7 | Density Functional Theoretical Study of 5 ,5 '-Azotetrazolate Nonmetallic Salts显示文摘The structures, infrared spectra and cation stability of seven 5,5′-azotetrazolate nonmetallic salts are investigated by using B3LYP method with 6-311+G (d) basis set. The salts are guanidinium (GZT), aminoguanidinium (AGZT), diaminoguanidinium (DAGZT), triaminoguanidinium (TAGZT), azidoformamidinium (AFZT), ammonium (AZT), and hydrazinium (HZT), respectively. The calculated results indicate that the carbon and nitrogen atoms of the cations in seven nonmetallic salts are characterized to be sp2 hybrid atoms, and the ranges of characteristic absorption peaks in IR spectra of the seven nonmetallic salts are approximative consistent. All their cations are stable and their stabilities decrease with the increase in their nitrogen contents. | LAI Weipeng GE Zhongxue LIAN Peng YU Tao CHEN Xiaofang QIU Shaojun WANG Bozhou | 2013 | Defence Technology(防务技术)2013，9，2： | 0 |
| 8 | Textual Research on the July 7,1590 A. D. Southeastern Yongjing Earthquake in Gansu Province显示文摘According to historical records,in July of 1590 A.D.,a destructive earthquake occurred near Lintao county in Gansu Province,in which '… city walls and houses collapsed,and countless people and domestic animals were killed'.In the same month,Binggou town in eastern Qinghai Province(now northeastern Ledu county),was also damaged by an earthquake.These two earthquakes were listed as two different cases in the published earthquake catalogues,recorded separately as the Lintao M_S5.5 earthquake with epicentral intensity Ⅶ in Gansu Province and the Ledu M_S5.0 earthquake with epicentral intensity Ⅵ in Qinghai Province.However,based on comprehensive analysis of research on historical records and field investigations,it is concluded in this paper that these two earthquakes could be the same one with magnitude 6.5 and epicentral intensity Ⅷ~Ⅸ.Its epicenter was in the Maxian Mt.,which is located in southeastern Yongjing and its seismogenic structure might be the mid-western segments of the north fringe fault zone of Maxian Mt.of Lanzhou. | Yuan Daoyang Lei Zhongsheng Zhang Junling Ge Weipeng Liu Xingwang LiuBaichi Liang Mingjian | 2009 | Earthquake Research in China2009，23，1： | 0 |
| 9 | A Preliminary Study of Palaeo-earthquakes on the Maqu Fault of East Kunlun Fault Zone显示文摘The East Kunlun active fault is an important NWW-trending boundary fault on the northeastern margin of the Qinghai-Xizang (Tibet) Plateau. The Maqu fault is the easternmost segment of the East Kunlun active fault. Based on three trenches, four Holocene palaeo-earthquake events are identified along the Maqu fault. The latest palaeo-earthquake event is (1730±50) ~ (1802±52) a BP, the second is (3736±57) ~ (4641±60) a BP, the third is (8590±70) a BP, and the earliest is (12200±1700) ka BP. The time of the first and second palaeo-earthquake events is more reliable than that of the third and last ones. As a result, the recurrence interval of the palaeo-earthquakes on the easternmost segment of the East Kunlun active fault is approximately 2400 a, and the palaeo-earthquake elapsed time is (1730±50) ~ (1802±52) a BP. | He Wengui Xiong Zhen Yuan Daoyang Ge Weipeng Liu Xingwang | 2006 | Earthquake Research in China2006，20，4： | 0 |
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