The Daliangshan tectonic zone is a rhombic area to the east of the Anninghe and Zemuhe fault zones in the middle segment of the Xianshuihe-Xiaojiang fault system along the southeast margin of the Qinghai-Xizang(Tibet)...The Daliangshan tectonic zone is a rhombic area to the east of the Anninghe and Zemuhe fault zones in the middle segment of the Xianshuihe-Xiaojiang fault system along the southeast margin of the Qinghai-Xizang(Tibet)Plateau.Since the Cenozoic era,the neotectonic deformation in the Daliangshan tectonic zone has presented not only sinistral slip and reverse faulting along the Daliangshan fault zone,but also proximate SN-trending crust shortening.It is estimated that the average crust shortening in the Daliangshan tectonic zone is 10.9±1.6 km,with a shortening rate of 17.8±2.2% using the method of balanced cross-sections.The crust shortening from folding occurred mainly in the Miocene and the Pliocene periods,lasting no more than 8.6 Ma.Based on this,a crust shortening velocity of 1.3±0.2 mm/a can be estimated.Compared with the left offset along the Daliangshan fault zone,it is recognized that crust shortening by folding plays an important part in transferring crustal deformation southeastward along the Xianshuihe-Xiaojiang fault system.展开更多
The Daliangshan fault zone is the eastern branch in the central section of Xianshuihe-Xiaojiang fault system. It has been neglected for a long time, partly because of no destructive earthquake records along this fault...The Daliangshan fault zone is the eastern branch in the central section of Xianshuihe-Xiaojiang fault system. It has been neglected for a long time, partly because of no destructive earthquake records along this fault zone. On the other hand, it is located on the remote and inaccessible plateau. So far it was excluded as part of the Xianshuihe-Xiaojiang fault system. Based on the interpretation of aerophotographs and field investigations, we document this fault zone in detail, and give an estimation of strike-slip rate about 3 mm/a in Late Quaternary together with age dating data. The results suggest that the Daliangshan fault zone is a newly-generated fault zone resulted from shortcutting in the central section of Xianshuihe-Xiaojiang fault system because of the clockwise rotation of the Southeastern Tibetan Crustal Block, which is bounded by the Xianshuihe-Xiaojiang fault system. Moreover, the shortcutting may make the Daliangshan fault zone replace the Anninghe and Zemuhe fault zones gradually, and finally, the later two fault zones will probably die out with the continuous clockwise rotation.展开更多
The Yi nationality, which has a population of 6.57 million, are spread over a wide area including Yunnan. Sichuan, Guizhou and Guangxi. Most of them live in the Liangshan Yi Autonomous Prefecture in Sichuan Province i...The Yi nationality, which has a population of 6.57 million, are spread over a wide area including Yunnan. Sichuan, Guizhou and Guangxi. Most of them live in the Liangshan Yi Autonomous Prefecture in Sichuan Province in compact communities.In ancient times, the forefathers of the Yis began to live and multiplied in Dianchi. Gongdu (now hi the southeast Xichang in Sichuan Province) and other places. Within the boundary of Lunan YI Autonomous County are ancient volcanic hills including the world famous Shilin (Stone Forest).The Yi nationality has its own language attd alphabet. This is China’s earliest syllabic alphabet. Developed in the 13th century, it contains some ten thousand symbols, but of these a thousand symbols are used most frequently. After the Yi language standardization program was passed in 1975. it was tested in the Yi regions in Sichuan. In 1990 a program was developed and the Yi language can now be used on computers.The book, Annats of Yi Nationality in the Southwest, records Yi history展开更多
基金the National Natural Science Foundation of China(40472109)"973"State Key Basic Research Project of China(2004CB418410)Joint Eanthquake Science Foundation of China(105066)
文摘The Daliangshan tectonic zone is a rhombic area to the east of the Anninghe and Zemuhe fault zones in the middle segment of the Xianshuihe-Xiaojiang fault system along the southeast margin of the Qinghai-Xizang(Tibet)Plateau.Since the Cenozoic era,the neotectonic deformation in the Daliangshan tectonic zone has presented not only sinistral slip and reverse faulting along the Daliangshan fault zone,but also proximate SN-trending crust shortening.It is estimated that the average crust shortening in the Daliangshan tectonic zone is 10.9±1.6 km,with a shortening rate of 17.8±2.2% using the method of balanced cross-sections.The crust shortening from folding occurred mainly in the Miocene and the Pliocene periods,lasting no more than 8.6 Ma.Based on this,a crust shortening velocity of 1.3±0.2 mm/a can be estimated.Compared with the left offset along the Daliangshan fault zone,it is recognized that crust shortening by folding plays an important part in transferring crustal deformation southeastward along the Xianshuihe-Xiaojiang fault system.
基金the National Basic Research Program of China (Grant No. 2004CB418401)the National Natural Science Foundation of China (Grant No. 40472109)+1 种基金Joint Earthquake Science Foundation of China (Grant No. 105066)Japan Grant-in Aid for Scientific Research from Japan Ministry of Education, Cul-ture, Sports, Science and Technology (Grant No. 18500776)
文摘The Daliangshan fault zone is the eastern branch in the central section of Xianshuihe-Xiaojiang fault system. It has been neglected for a long time, partly because of no destructive earthquake records along this fault zone. On the other hand, it is located on the remote and inaccessible plateau. So far it was excluded as part of the Xianshuihe-Xiaojiang fault system. Based on the interpretation of aerophotographs and field investigations, we document this fault zone in detail, and give an estimation of strike-slip rate about 3 mm/a in Late Quaternary together with age dating data. The results suggest that the Daliangshan fault zone is a newly-generated fault zone resulted from shortcutting in the central section of Xianshuihe-Xiaojiang fault system because of the clockwise rotation of the Southeastern Tibetan Crustal Block, which is bounded by the Xianshuihe-Xiaojiang fault system. Moreover, the shortcutting may make the Daliangshan fault zone replace the Anninghe and Zemuhe fault zones gradually, and finally, the later two fault zones will probably die out with the continuous clockwise rotation.
文摘The Yi nationality, which has a population of 6.57 million, are spread over a wide area including Yunnan. Sichuan, Guizhou and Guangxi. Most of them live in the Liangshan Yi Autonomous Prefecture in Sichuan Province in compact communities.In ancient times, the forefathers of the Yis began to live and multiplied in Dianchi. Gongdu (now hi the southeast Xichang in Sichuan Province) and other places. Within the boundary of Lunan YI Autonomous County are ancient volcanic hills including the world famous Shilin (Stone Forest).The Yi nationality has its own language attd alphabet. This is China’s earliest syllabic alphabet. Developed in the 13th century, it contains some ten thousand symbols, but of these a thousand symbols are used most frequently. After the Yi language standardization program was passed in 1975. it was tested in the Yi regions in Sichuan. In 1990 a program was developed and the Yi language can now be used on computers.The book, Annats of Yi Nationality in the Southwest, records Yi history
