The Ji De Sheng She Yao tablet (季德胜蛇药片）is a drug for snake-bites and insect bites. According to recent reports, this drug has been used to treat herpes zoster, hepatitis B, parotitis, nephrotic syndrome, acute ...The Ji De Sheng She Yao tablet (季德胜蛇药片）is a drug for snake-bites and insect bites. According to recent reports, this drug has been used to treat herpes zoster, hepatitis B, parotitis, nephrotic syndrome, acute conjunctivitis, recurrent aphtha, urticaria, etc.1 with good therapeutic effects. More than half of the AIDS patients suffered from herpes zoster. The area of skin lesion in AIDS patients is larger than that of the patients without AIDS and the pain lasts longer. Many cases have keloids and depigmentation for months, even severe pain till their death. Routine therapeutic methods are not satisfactory in therapeutic effects. The expert group of traditional Chinese medicine for cooperative research on AIDS used Ji De Sheng She Yao tablets (季德胜蛇药片) to treat AIDS complicated by herpes zoster for the first time and the results are reported as follows.展开更多
Herpes zoster,a herpetic disease caused by virus,usually occurs in spring and autumn.If treated properlywith western or Chinese medicines,the herpes may getscarred and healed in 2 to 3 weeks,but the constantneuralgia ...Herpes zoster,a herpetic disease caused by virus,usually occurs in spring and autumn.If treated properlywith western or Chinese medicines,the herpes may getscarred and healed in 2 to 3 weeks,but the constantneuralgia in the primary herpetic areas may remain forweeks or even for months.Characterized by prickingpain,or sharp or vague pain,with paroxysmalexacerbation,it is usually milder in the daytime展开更多
The Xiannvshan fault zone, lying along the western margin of the Huangling anticline, is one of the most important fault zones in the Three Gorges reservoir area. The fault experienced strong activity during the Cenoz...The Xiannvshan fault zone, lying along the western margin of the Huangling anticline, is one of the most important fault zones in the Three Gorges reservoir area. The fault experienced strong activity during the Cenozoic Era. The question of whether the fault zone goes through the Yangtze River has been one of the key problems faced in previous studies as it has a significant influence upon the assessment of geological hazards and earthquake stability in the reservoir area. Based on tectonic and geomorphic observations along the fault zone between the Baixianchi village in Changyang county and Huangkou village in Zigui town, together with the comparisons between the geology in Guizhou and Quyuan town in the north bank of the Yangtze River and the Xiannvshan fault zone, it is suggested that the north end of this fault zone is located around Huangkou village and does not go through the Yangtze rivers northward. The evidence is as follows: ① On the basis of field data collection, it is found that the Xiannvshan Fault zone, which stretches 80km, underwent thrust movement in the Cenozoic period, resulting in ravines and fault scarps, topographically. Whereas, on the northern bank of the Yangtze River, faults are rarely found, and most of the faults are developed in the Jurassic strata,without topographical effects. Therefore, the Xiannvshan Fault zone has not stretched to the north bank of the Yangtze River. ② The fault gouge and tectonite zone were found developed on the Xiannvshan Fault zone at Baixianchi village, but only a tectonite zone was found at Zhouping village. There are also some branch faults close to the northern end of the fault zone. So, the activity of the fault zone weakened from south to north in Cenozoic. The fault zone extends northward and dies out at Huangkou. It doesn't stretch forward any longer as indicated by continuous strata, sparse joints, and small folds, etc.展开更多
文摘The Ji De Sheng She Yao tablet (季德胜蛇药片）is a drug for snake-bites and insect bites. According to recent reports, this drug has been used to treat herpes zoster, hepatitis B, parotitis, nephrotic syndrome, acute conjunctivitis, recurrent aphtha, urticaria, etc.1 with good therapeutic effects. More than half of the AIDS patients suffered from herpes zoster. The area of skin lesion in AIDS patients is larger than that of the patients without AIDS and the pain lasts longer. Many cases have keloids and depigmentation for months, even severe pain till their death. Routine therapeutic methods are not satisfactory in therapeutic effects. The expert group of traditional Chinese medicine for cooperative research on AIDS used Ji De Sheng She Yao tablets (季德胜蛇药片) to treat AIDS complicated by herpes zoster for the first time and the results are reported as follows.
文摘Herpes zoster,a herpetic disease caused by virus,usually occurs in spring and autumn.If treated properlywith western or Chinese medicines,the herpes may getscarred and healed in 2 to 3 weeks,but the constantneuralgia in the primary herpetic areas may remain forweeks or even for months.Characterized by prickingpain,or sharp or vague pain,with paroxysmalexacerbation,it is usually milder in the daytime
基金funded by Geological Disaster Preventing Project of the Third Stage of Three Gorges Project of Ministry of Land and Resources,China (SXKY3-5)the Basic Research Project of the National Non-profit Research Institutes,Institute of Geology,CEA(IGCEA1001)
文摘The Xiannvshan fault zone, lying along the western margin of the Huangling anticline, is one of the most important fault zones in the Three Gorges reservoir area. The fault experienced strong activity during the Cenozoic Era. The question of whether the fault zone goes through the Yangtze River has been one of the key problems faced in previous studies as it has a significant influence upon the assessment of geological hazards and earthquake stability in the reservoir area. Based on tectonic and geomorphic observations along the fault zone between the Baixianchi village in Changyang county and Huangkou village in Zigui town, together with the comparisons between the geology in Guizhou and Quyuan town in the north bank of the Yangtze River and the Xiannvshan fault zone, it is suggested that the north end of this fault zone is located around Huangkou village and does not go through the Yangtze rivers northward. The evidence is as follows: ① On the basis of field data collection, it is found that the Xiannvshan Fault zone, which stretches 80km, underwent thrust movement in the Cenozoic period, resulting in ravines and fault scarps, topographically. Whereas, on the northern bank of the Yangtze River, faults are rarely found, and most of the faults are developed in the Jurassic strata,without topographical effects. Therefore, the Xiannvshan Fault zone has not stretched to the north bank of the Yangtze River. ② The fault gouge and tectonite zone were found developed on the Xiannvshan Fault zone at Baixianchi village, but only a tectonite zone was found at Zhouping village. There are also some branch faults close to the northern end of the fault zone. So, the activity of the fault zone weakened from south to north in Cenozoic. The fault zone extends northward and dies out at Huangkou. It doesn't stretch forward any longer as indicated by continuous strata, sparse joints, and small folds, etc.
