Objective： To explore the clinical effects of electroacupuncture（EA） at Zusanli（ST 36） and Fenglong（ST 40） in treating senile dementia. Methods： A total of 74 patients were randomly divided into an EA group an...Objective： To explore the clinical effects of electroacupuncture（EA） at Zusanli（ST 36） and Fenglong（ST 40） in treating senile dementia. Methods： A total of 74 patients were randomly divided into an EA group and a medication group based upon the random digital table, 37 cases in each group. EA at Zusanli（ST 36） and Fenglong（ST 40） was given in the EA group, once every day, for six treatments per week. Donepezil Hydrochloride Tablets were given to the medication group, 5 mg per time and once a day in the former four weeks, 10 mg per time and once a day after 4 weeks, oral administration before sleep at night. The courses of the treatment were 12 weeks in both groups. The scores of mini-mental state examination（MMSE） and Barthel index（BI） were observed before and after the treatment, for processing the comparative analysis of the clinical effects after the course of the treatment. Results： The total effective rate was 86.5% in the EA group and 70.3% in the medication group. The therapeutic effect was better in the EA group than that in the medication group, and the difference between the two groups was statistically significant（P〈0.05）. MMSE and BI scores after the treatment in the two groups were all elevated than those of the same groups before the treatment（P〈0.05, P〈0.01）. The improving situation was obviously better in the EA group than that in the medication group, and the difference between the two groups was statistically significant（P〈0.05）. Conclusion： EA at Zusanli（ST 36） and Fenglong（ST 40） is affirmative in the therapeutic effect for senile dementia and can also improve the cognitive function and enhance the patients＇ quality of life.展开更多
The Altyn Tagh Fault and the Altyn Mountain define respectively the tectonic and geographical northern edges of the Tibetan Plateau, and figure prominently in the growth and rising mechanism of the plateau. The rhombu...The Altyn Tagh Fault and the Altyn Mountain define respectively the tectonic and geographical northern edges of the Tibetan Plateau, and figure prominently in the growth and rising mechanism of the plateau. The rhombus-shaped Altyn Mountain has long been thought to have an intimate relation with the Altyn Tagh Fault; however, its formation mechanism remains unclear and debatable. In this paper, we focus on the EW-trending uplifts in the Altyn Mountain, and investigated three Cenozoic sedimentary sections in the vicinity of the EW-trending uplifts located along the southern side of the central segment of the Altyn Tagh Fault. Magnetostratigraphy and pollen analysis were used to constrain ages of the sediments. Clast composition of conglomerate and paleocurrents obtained from clast imbrications were applied to determine the provenance. We also established a geological section parallel to the Altyn Tagh Fault on sedimentary facies across the northwestern Qaidam Basin. The results indicate that these en-echelon EW-trending uplifts formed as early as ca. 36 Ma and were preferred to be under the control of basal shear of the Altyn Tagh Fault in the middle-lower crust, symbolizing the early uplift of the Altyn Mountain during the Cenozoic. Left-slip along the Altyn Tagh Fault occurring during the Miocene and afterwards displaced and altered these uplifts, shaping the Altyn Mountain to its present fabric.展开更多
文摘Objective： To explore the clinical effects of electroacupuncture（EA） at Zusanli（ST 36） and Fenglong（ST 40） in treating senile dementia. Methods： A total of 74 patients were randomly divided into an EA group and a medication group based upon the random digital table, 37 cases in each group. EA at Zusanli（ST 36） and Fenglong（ST 40） was given in the EA group, once every day, for six treatments per week. Donepezil Hydrochloride Tablets were given to the medication group, 5 mg per time and once a day in the former four weeks, 10 mg per time and once a day after 4 weeks, oral administration before sleep at night. The courses of the treatment were 12 weeks in both groups. The scores of mini-mental state examination（MMSE） and Barthel index（BI） were observed before and after the treatment, for processing the comparative analysis of the clinical effects after the course of the treatment. Results： The total effective rate was 86.5% in the EA group and 70.3% in the medication group. The therapeutic effect was better in the EA group than that in the medication group, and the difference between the two groups was statistically significant（P〈0.05）. MMSE and BI scores after the treatment in the two groups were all elevated than those of the same groups before the treatment（P〈0.05, P〈0.01）. The improving situation was obviously better in the EA group than that in the medication group, and the difference between the two groups was statistically significant（P〈0.05）. Conclusion： EA at Zusanli（ST 36） and Fenglong（ST 40） is affirmative in the therapeutic effect for senile dementia and can also improve the cognitive function and enhance the patients＇ quality of life.
基金supported by Chinese National Key Scientific and Technological Projects (Grant Nos. 2011ZX05009-001 and2011ZX05003-002)
文摘The Altyn Tagh Fault and the Altyn Mountain define respectively the tectonic and geographical northern edges of the Tibetan Plateau, and figure prominently in the growth and rising mechanism of the plateau. The rhombus-shaped Altyn Mountain has long been thought to have an intimate relation with the Altyn Tagh Fault; however, its formation mechanism remains unclear and debatable. In this paper, we focus on the EW-trending uplifts in the Altyn Mountain, and investigated three Cenozoic sedimentary sections in the vicinity of the EW-trending uplifts located along the southern side of the central segment of the Altyn Tagh Fault. Magnetostratigraphy and pollen analysis were used to constrain ages of the sediments. Clast composition of conglomerate and paleocurrents obtained from clast imbrications were applied to determine the provenance. We also established a geological section parallel to the Altyn Tagh Fault on sedimentary facies across the northwestern Qaidam Basin. The results indicate that these en-echelon EW-trending uplifts formed as early as ca. 36 Ma and were preferred to be under the control of basal shear of the Altyn Tagh Fault in the middle-lower crust, symbolizing the early uplift of the Altyn Mountain during the Cenozoic. Left-slip along the Altyn Tagh Fault occurring during the Miocene and afterwards displaced and altered these uplifts, shaping the Altyn Mountain to its present fabric.
