Dr.Shau Yan Lee[李守仁]was a Baptist minister,teacher,and scholar.He worked in China and America for more than 40 years.His text books and audio materials on Chinese language studies were widely used in America and Ca...Dr.Shau Yan Lee[李守仁]was a Baptist minister,teacher,and scholar.He worked in China and America for more than 40 years.His text books and audio materials on Chinese language studies were widely used in America and Canada during the 1940s,50s and 60s.He was the first few persons to use phonograph recording to record Chinese dialects and English-Chinese vocabulary.His two academic books How to win the Chinese(1944)and China has a ten thousand mile spiritual wall(1945)attracted a lot of attention in the 1940s.According to the WorldCat,his first book had three reprints between 1944 and 1946 and was held by twenty six libraries worldwide.His second book had four reprints in 1945 and was held by twenty four libraries worldwide.The latter was also gifted and received by President Franklin D.Roosevelt(See Proulx,2006).In this memoir we will give a brief account of Lee’s education background,work experience,academic publishing,and contributions to Chinese linguistics.We will also give a brief account of his families.This account is based on sourced materials and completed to remember his contribution to society.Any information without citation is provided by his two youngest daughters Ding Jung Lee(李定中)and To Jung Lee(李道中).展开更多
The Tian Shan Mountains were formed in the result of the India-Eurasia collision, which leads to cre- ation of contrast high-mountain relief and world known seismic activity. The seismic catastrophes, recorded instrum...The Tian Shan Mountains were formed in the result of the India-Eurasia collision, which leads to cre- ation of contrast high-mountain relief and world known seismic activity. The seismic catastrophes, recorded instrumentally, have occurred to the north of the Issyk-Kul Lake region. There are also known significant earthquakes with magnitude being about 7 in western and eastern parts of the mentioned lake region. Only in the south of the Issyk-Kul depression the strong earthquakes recorded by the seismic network were not known. Our recent study in the south of the lssyk-Kul Lake region has revealed numerous active tectonic structures related to South Issyk-I（ul Fault： faults and folds, responsible for strong earthquakes＇ occurrence. These were historical and paleoseismic defornlations which led to changes in relief： fault scarps and significant rockslides. We have also found spectacular deformations in archeological monuments. All these deformations testify the location of epicentral areas of two strong historic （about llth and 16th （？） centuries AD） and paleoearthquakes （Holocene and Late Pleistocene）. Magnitude of ancient seismic events, according to parameters of the revealed fault scarps, were Ms 〉 7 and seismic intensity I 〉 IX. All revealed seismic deformations are located to adyrs （piedmonts） of the Terskey Ala-Too range bordered of the lssyk-Kul Lake depression in the south. Their formation is described by the model of a fault which rupture plane becomes shallower southward. This model is complicated by the presence of reverse thrusts. Here, we should admit the existence of a single zone of South lssyk-Kul Fault which is a long-lived feature which separates the structures with the different regime of movements during the Neotectonic time. All obtained data led us to a conclusion of significant underestimation of the seismic hazard in southern lssyk-Kul Lake region.展开更多
文摘Dr.Shau Yan Lee[李守仁]was a Baptist minister,teacher,and scholar.He worked in China and America for more than 40 years.His text books and audio materials on Chinese language studies were widely used in America and Canada during the 1940s,50s and 60s.He was the first few persons to use phonograph recording to record Chinese dialects and English-Chinese vocabulary.His two academic books How to win the Chinese(1944)and China has a ten thousand mile spiritual wall(1945)attracted a lot of attention in the 1940s.According to the WorldCat,his first book had three reprints between 1944 and 1946 and was held by twenty six libraries worldwide.His second book had four reprints in 1945 and was held by twenty four libraries worldwide.The latter was also gifted and received by President Franklin D.Roosevelt(See Proulx,2006).In this memoir we will give a brief account of Lee’s education background,work experience,academic publishing,and contributions to Chinese linguistics.We will also give a brief account of his families.This account is based on sourced materials and completed to remember his contribution to society.Any information without citation is provided by his two youngest daughters Ding Jung Lee(李定中)and To Jung Lee(李道中).
基金financial support of ISTC grants Nos.KR-2011 and G-2153
文摘The Tian Shan Mountains were formed in the result of the India-Eurasia collision, which leads to cre- ation of contrast high-mountain relief and world known seismic activity. The seismic catastrophes, recorded instrumentally, have occurred to the north of the Issyk-Kul Lake region. There are also known significant earthquakes with magnitude being about 7 in western and eastern parts of the mentioned lake region. Only in the south of the Issyk-Kul depression the strong earthquakes recorded by the seismic network were not known. Our recent study in the south of the lssyk-Kul Lake region has revealed numerous active tectonic structures related to South Issyk-I（ul Fault： faults and folds, responsible for strong earthquakes＇ occurrence. These were historical and paleoseismic defornlations which led to changes in relief： fault scarps and significant rockslides. We have also found spectacular deformations in archeological monuments. All these deformations testify the location of epicentral areas of two strong historic （about llth and 16th （？） centuries AD） and paleoearthquakes （Holocene and Late Pleistocene）. Magnitude of ancient seismic events, according to parameters of the revealed fault scarps, were Ms 〉 7 and seismic intensity I 〉 IX. All revealed seismic deformations are located to adyrs （piedmonts） of the Terskey Ala-Too range bordered of the lssyk-Kul Lake depression in the south. Their formation is described by the model of a fault which rupture plane becomes shallower southward. This model is complicated by the presence of reverse thrusts. Here, we should admit the existence of a single zone of South lssyk-Kul Fault which is a long-lived feature which separates the structures with the different regime of movements during the Neotectonic time. All obtained data led us to a conclusion of significant underestimation of the seismic hazard in southern lssyk-Kul Lake region.
