Objective To observe clinical effect of warm needing plus cupping at back on facial paralysis. Methods Forty cases of peripheral facial paralysis were firstly treated with warm needling. Cuánzhú （攒竹 BL 2...Objective To observe clinical effect of warm needing plus cupping at back on facial paralysis. Methods Forty cases of peripheral facial paralysis were firstly treated with warm needling. Cuánzhú （攒竹 BL 2）, Yángbái （阳白 GB 14）, Sīzhúkōng （丝竹空 TE 23）, Sìbái （四白 ST 2）, Tīnghuì （听会 GB 2）, Yìfēng （翳 风 TE 17）, Dìcāng （地仓 ST 4）, Jiáchē （颊车 ST 6）, Yíngxiāng （迎香 LI 20） and Hég （合谷 LI 4） were selected and warm needling was applied at Tīnghuì （听 会 GB 2）. Needles were retained for 30 min, once a day. Cupping at back was then applied at bilateral Fèishū （肺俞 BL 13）, Píshū （脾俞 BL 20）, Shènshū （肾 俞 BL 23） in the Bladder Meridian of Foot-Taiyang for 10 min, once a day for first five days and then once every other day. Ten days of treatment were taken as a treatment course with one day interval between courses. The efficacy was observed after two treatment courses. Results Twenty-six cases were cured, ten cases were markedly effective, three cases were effective and one case was failed. The total effective rate was 97.5% （39/40）. Conclusion From theory of coldness to treat facial paralysis, efficacy is significant with warm needling and cupping at the Bladder Meridian of Foot-Taiyang.展开更多
Much has been learned in the past 40 years about the great diversity of the internal structure and geochemical compositions of Phanerozoic ophiolites, indicating that these on-land fragments of ancient oceanic lithosp...Much has been learned in the past 40 years about the great diversity of the internal structure and geochemical compositions of Phanerozoic ophiolites, indicating that these on-land fragments of ancient oceanic lithosphere formed in distinctly different tectonic settings during their igneous evolution. Recent studies in Archean and Proterozoic greenstone belts have shown that the Precambrian rock record may also include exposures of a diverse suite of ophiolite complexes as part of craton development in the early history of the Earth. We review the salient features of the Precambrian ophiolite record to highlight what has been learned about Precambrian oceanic spreading systems since the original Penrose definition of ophiolites in 1972. Some of the diagnostic, characteristic, typical, and rare aspects of ophiolites of all ages are presented in a table in order to help determine if tectonically deformed and metamophosed sequences in Precambrian shield areas may be considered as ophiolites. The results of this comparative study are important in that they enable researchers to more realistically characterize allochthonous mafic/ultramafic rock sequences as ophiolitic or non-ophiolitic. This approach is more deterministic in contrast to some other arbitrary classification schemes requiring three or four of the Penrose-style ophiolitic units to be present in the Precambrian record for a specific rock sequence to be considered ophiolitic. Once these tectonic fragments are recognized as remnants of ancient oceanic lithosphere, great progress shall be made in understanding early Earth history. We discuss the significance and implications of the Precambrian ophiolite record to constrain the mode and nature of the plate tectonics that operated in deep time.展开更多
文摘Objective To observe clinical effect of warm needing plus cupping at back on facial paralysis. Methods Forty cases of peripheral facial paralysis were firstly treated with warm needling. Cuánzhú （攒竹 BL 2）, Yángbái （阳白 GB 14）, Sīzhúkōng （丝竹空 TE 23）, Sìbái （四白 ST 2）, Tīnghuì （听会 GB 2）, Yìfēng （翳 风 TE 17）, Dìcāng （地仓 ST 4）, Jiáchē （颊车 ST 6）, Yíngxiāng （迎香 LI 20） and Hég （合谷 LI 4） were selected and warm needling was applied at Tīnghuì （听 会 GB 2）. Needles were retained for 30 min, once a day. Cupping at back was then applied at bilateral Fèishū （肺俞 BL 13）, Píshū （脾俞 BL 20）, Shènshū （肾 俞 BL 23） in the Bladder Meridian of Foot-Taiyang for 10 min, once a day for first five days and then once every other day. Ten days of treatment were taken as a treatment course with one day interval between courses. The efficacy was observed after two treatment courses. Results Twenty-six cases were cured, ten cases were markedly effective, three cases were effective and one case was failed. The total effective rate was 97.5% （39/40）. Conclusion From theory of coldness to treat facial paralysis, efficacy is significant with warm needling and cupping at the Bladder Meridian of Foot-Taiyang.
基金supported by U.S. National Science Foundation Grants (Grant Nos. 02-07886, and 01-25925)National Natural Science Foundation of China (Grant Nos. 91014002, 40821061)Ministry of Education of China (Grant No. B07039)
文摘Much has been learned in the past 40 years about the great diversity of the internal structure and geochemical compositions of Phanerozoic ophiolites, indicating that these on-land fragments of ancient oceanic lithosphere formed in distinctly different tectonic settings during their igneous evolution. Recent studies in Archean and Proterozoic greenstone belts have shown that the Precambrian rock record may also include exposures of a diverse suite of ophiolite complexes as part of craton development in the early history of the Earth. We review the salient features of the Precambrian ophiolite record to highlight what has been learned about Precambrian oceanic spreading systems since the original Penrose definition of ophiolites in 1972. Some of the diagnostic, characteristic, typical, and rare aspects of ophiolites of all ages are presented in a table in order to help determine if tectonically deformed and metamophosed sequences in Precambrian shield areas may be considered as ophiolites. The results of this comparative study are important in that they enable researchers to more realistically characterize allochthonous mafic/ultramafic rock sequences as ophiolitic or non-ophiolitic. This approach is more deterministic in contrast to some other arbitrary classification schemes requiring three or four of the Penrose-style ophiolitic units to be present in the Precambrian record for a specific rock sequence to be considered ophiolitic. Once these tectonic fragments are recognized as remnants of ancient oceanic lithosphere, great progress shall be made in understanding early Earth history. We discuss the significance and implications of the Precambrian ophiolite record to constrain the mode and nature of the plate tectonics that operated in deep time.
