To determine the locked and slip parts on a fault,we simulated the movement pattern of the fault with a combined model consisting of a negative dislocation in the locked area superimposed on a relative movement betwee...To determine the locked and slip parts on a fault,we simulated the movement pattern of the fault with a combined model consisting of a negative dislocation in the locked area superimposed on a relative movement between two sides of the fault.In this way,we determined the locked parts of faults by inversion with multiple epochs of geodetic data.In this paper,we have determined the movement patterns of four main faults in western Yunnan by inversion with two epochs of geodetic surveys and some crossing-fault observations.From the inversion result,we have identified the areas around Dali and Xiangyun to be the locked area,which is regarded as a sign of potential earthquake sources.展开更多
The scholarship in modern China is closely related to Western sinology in terms of school ties.Gu Jiegang’s launching of the"Discussion of Ancient History"movement centered on the"theory of the accumul...The scholarship in modern China is closely related to Western sinology in terms of school ties.Gu Jiegang’s launching of the"Discussion of Ancient History"movement centered on the"theory of the accumulated creation of Chinese ancient history"was a representative example.At the beginning of the movement Hu Shi and Gu Jiegang proposed the notion that,"there was no history before the Eastern Zhou Dynasty"which was indebted to the historical skepticism by Philip Van Ness Myers(American scholar)and Friedrich Hirth(German sinologist)of the same period.The idea that"the Shang Dynasty is still in the late Stone Age"advocated by Hu and Gu was also directly influenced by J.G.Andersson’s An Early Chinese Culture.Conversely,American sinologist Arthur W.Hummel Sr played a key role in introducing and evaluating the first volume of Discussion of Ancient History to Western academia.Paradoxically,while Swedish sinologis Bernhard Karlgren wrote On the Authenticity and Nature of the Tso Chuan to refute Kang Youwei’s reinterpretation of Confucian Classics(The Forged Classics of the Wang Mang Period),his work however became of value for Chinese historic doubt scholars to reaffirm the value of New Text Confucianism and advance the"Discussion of Ancient History"movement.If we would like to choose a saying to describe the relationship between the"Discussion of Ancien History"movement and Western Sinology,the Chinese proverb,"Stones from other hills may serve to polish jade of this one,"may be an appropriate choice.展开更多
Based on the data of mobile gravity observation from 1998 to 2008 in western Sichuan, spatial dynamic variation results of regional gravity field are obtained. The relationship between the gravity variation features a...Based on the data of mobile gravity observation from 1998 to 2008 in western Sichuan, spatial dynamic variation results of regional gravity field are obtained. The relationship between the gravity variation features and Wenchuan Ms8.0 earthquake is systematically analyzed. The results show： 1 ） Gravity variation is closely related to active fault tectonics, and gravity measurement can better reflect material migration following crustal tectonic activity near active fault. 2）The gravity field appeared a wider range regional gravity variation during Wenchuan earthquake occurrence. The dynamic patterns of gravity field demonstrates the evolution process of gravity field ： quasi - homogeneous state non - homogeneous state-earthquake occurrence.展开更多
Tectonic deformation of Cenozoic strata,youthful tectonontorphology,and high seismicity in the western part of Sichuan and Yunnan(Southwest China)marked intensive tectonism there during the Ceno7oic.It is a good place...Tectonic deformation of Cenozoic strata,youthful tectonontorphology,and high seismicity in the western part of Sichuan and Yunnan(Southwest China)marked intensive tectonism there during the Ceno7oic.It is a good place for studying the continental geodynamics because it is far away from those active plate boundaries surrounding the East Asian continent but near the southeastern margin of the Qinghai-Xizang(Tibet)plateau.The present study discriminated two phases of tectonic deformation with quite different styles in Cenozoic.Early compression deformation,expressed by folds,thrust,and even nappe structure,mainly occurred between the middle and late Eocene.Late extension deformation expressed by block-faulting started at least in the late Pliocene.Nonconformity,absence of strata,nonsuccessive tectonism,and inverse movement of the faults in late stages illustrated that two different deformation phases should be caused by different geodynamic processes.The early compression deformation would be related to展开更多
There’re 4 types of crustobodies and total 6.Each has its own way of evolu-tion and movement. Their combination and separation depict a complex history of geotectonics.
文摘To determine the locked and slip parts on a fault,we simulated the movement pattern of the fault with a combined model consisting of a negative dislocation in the locked area superimposed on a relative movement between two sides of the fault.In this way,we determined the locked parts of faults by inversion with multiple epochs of geodetic data.In this paper,we have determined the movement patterns of four main faults in western Yunnan by inversion with two epochs of geodetic surveys and some crossing-fault observations.From the inversion result,we have identified the areas around Dali and Xiangyun to be the locked area,which is regarded as a sign of potential earthquake sources.
文摘The scholarship in modern China is closely related to Western sinology in terms of school ties.Gu Jiegang’s launching of the"Discussion of Ancient History"movement centered on the"theory of the accumulated creation of Chinese ancient history"was a representative example.At the beginning of the movement Hu Shi and Gu Jiegang proposed the notion that,"there was no history before the Eastern Zhou Dynasty"which was indebted to the historical skepticism by Philip Van Ness Myers(American scholar)and Friedrich Hirth(German sinologist)of the same period.The idea that"the Shang Dynasty is still in the late Stone Age"advocated by Hu and Gu was also directly influenced by J.G.Andersson’s An Early Chinese Culture.Conversely,American sinologist Arthur W.Hummel Sr played a key role in introducing and evaluating the first volume of Discussion of Ancient History to Western academia.Paradoxically,while Swedish sinologis Bernhard Karlgren wrote On the Authenticity and Nature of the Tso Chuan to refute Kang Youwei’s reinterpretation of Confucian Classics(The Forged Classics of the Wang Mang Period),his work however became of value for Chinese historic doubt scholars to reaffirm the value of New Text Confucianism and advance the"Discussion of Ancient History"movement.If we would like to choose a saying to describe the relationship between the"Discussion of Ancien History"movement and Western Sinology,the Chinese proverb,"Stones from other hills may serve to polish jade of this one,"may be an appropriate choice.
基金supported by the National Natural Science Foundation(40874035)a special earthquake research project grant from China Earthquake Administration(200908029)
文摘Based on the data of mobile gravity observation from 1998 to 2008 in western Sichuan, spatial dynamic variation results of regional gravity field are obtained. The relationship between the gravity variation features and Wenchuan Ms8.0 earthquake is systematically analyzed. The results show： 1 ） Gravity variation is closely related to active fault tectonics, and gravity measurement can better reflect material migration following crustal tectonic activity near active fault. 2）The gravity field appeared a wider range regional gravity variation during Wenchuan earthquake occurrence. The dynamic patterns of gravity field demonstrates the evolution process of gravity field ： quasi - homogeneous state non - homogeneous state-earthquake occurrence.
文摘Tectonic deformation of Cenozoic strata,youthful tectonontorphology,and high seismicity in the western part of Sichuan and Yunnan(Southwest China)marked intensive tectonism there during the Ceno7oic.It is a good place for studying the continental geodynamics because it is far away from those active plate boundaries surrounding the East Asian continent but near the southeastern margin of the Qinghai-Xizang(Tibet)plateau.The present study discriminated two phases of tectonic deformation with quite different styles in Cenozoic.Early compression deformation,expressed by folds,thrust,and even nappe structure,mainly occurred between the middle and late Eocene.Late extension deformation expressed by block-faulting started at least in the late Pliocene.Nonconformity,absence of strata,nonsuccessive tectonism,and inverse movement of the faults in late stages illustrated that two different deformation phases should be caused by different geodynamic processes.The early compression deformation would be related to
文摘There’re 4 types of crustobodies and total 6.Each has its own way of evolu-tion and movement. Their combination and separation depict a complex history of geotectonics.
