This paper explores Mao Zedong’s early views on physical education and practice,focusing on the“Six-Section Exercise”he created.The exercise,which integrates elements from traditional health-preserving techniques,g...This paper explores Mao Zedong’s early views on physical education and practice,focusing on the“Six-Section Exercise”he created.The exercise,which integrates elements from traditional health-preserving techniques,gymnastics,boxing,and military training,was designed to promote balanced physical development,be practical and effective,and require less time per session.The paper argues that Mao Zedong’s views on physical education were grounded in the belief that it could effectively transform individuals and contribute to the creation of a strong sports nation.The paper also discusses the historical context and social trends behind the creation of the“Six-Section Exercise”,including the New Culture Movement and debates between Chinese and Western,static and dynamic,and new and old approaches to physical education.The paper concludes by suggesting that Mao Zedong’s early sports thinking has significant academic value and can provide guidance for the construction of a healthy China today.展开更多
The Zedong Terrane forms a discontinuous belt of volcanic and volcaniclastic rocks adjacent to the Yarlung Zangbo River in south eastern Tibet. It extends from Luobusa to 20km west of Zedong. The Zedong Terrane lies w...The Zedong Terrane forms a discontinuous belt of volcanic and volcaniclastic rocks adjacent to the Yarlung Zangbo River in south eastern Tibet. It extends from Luobusa to 20km west of Zedong. The Zedong Terrane lies within the Indus—Yarlung Zangbo suture zone and may represent an intra\|oceanic island arc that once lay between the Lhasa (Asian) and Himalayan (Indian) terranes. Rare fossils within the terrane indicate active volcanism during the Early Cretaceous.Ultramafic rocks of the Dazhuqu Terrane, including harzburgite and gabbro are thrust over the southern margin of the Zedong Terrane along a steep south\|dipping thrust fault. To the west of Zedong, this fault is marked by a distinctive zone of serpentinite. East of Zedong, the northernmost rocks of the terrane are thrust onto Oligocene molasse deposits of the Luobusa Formation and Cretaceous plutonic rocks of the Gangdese batholith (Lhasa Terrane). These thrusts form part of a northward directed thrust stack \| the Renbu\|Zedong thrust system of Yin et al.., (1994, 1999).展开更多
Former chairman Mao Zedong conducted extensive rural surveys during the exploration of the Chinese revolutionary road. In 1941,in order to change the state of the party's theory separating from reality,Mao Zedong ...Former chairman Mao Zedong conducted extensive rural surveys during the exploration of the Chinese revolutionary road. In 1941,in order to change the state of the party's theory separating from reality,Mao Zedong organized and published the book Rural Surveys,which provided the direction for survey and research of the party members. The survey and research are excellent tradition and style of work of the party,and also a major weapon for outstanding achievements in China's revolution and construction. Socialism with Chinese characteristics has entered a new era. Studying the Rural Surveys has important practical value for beating off the new challenges in the issues concerning agriculture,farmers,and rural areas.展开更多
The Yarlung Zangbo suture zone extends more than2000 km along southern Tibet and marks the boundary between the Indian subcontinent and Eurasia.The Zedong terrane has been not suggested to represent the vestige of suc...The Yarlung Zangbo suture zone extends more than2000 km along southern Tibet and marks the boundary between the Indian subcontinent and Eurasia.The Zedong terrane has been not suggested to represent the vestige of such an intra-oceanic arc developed within the Neo-Tethys Ocean,as a result of the northward subduction of the Neo-Tethys Ocean during the Late Jurassic.In this study,we present detailed geochemical and geochronological data of various types of magmatic rocks widely exposed in the Zedong terrane to constrain the formation age and tectonic setting of the Zedong terrane.We found that the Zedong volcanic rocks belong to high K2O calc-alkaline series,whereas the diabase and gabbro plotted in the low-K calcalkline.The basalt rocks are highly enriched in LREE and LILE,but strongly depleted in HFSE,indicating they were derived from a metasomatized mantle.Both gabbros and diabase have similar N-MORB geochemistry indicates that the cumulates were produced from MOR setting.Zircons from four samples,including the basalt rocks(158-161Ma)are older than the gabbro(131 Ma),certificate the gabbro are as the vein intrude into the basalt rocks.This suggests that the volcanic eruption and plutonic emplacement were coevally developed in the Zedonghave similar positiveεHf(t)values(+2.0 to+15.6)and(+8.6 to+18.4),indicating they were stemmed from similarly depleted mantle sources,same with the gabbro and granitic rocks from the Gangdese arc.Therefore,we proposed that the basalt rocks in the Zedong terrane were formed through partial melting of the mantle wedge metasomatized by slab-released fluids/melts.A part of hydrous basalts were underplated in the thickened lower crust beneath the Zedong terrane,which gave rise to the cumulate and granitic rocks.This suggests that the Zedong terrane represents a slice of the active continental margin developed on the southern margin of the Lhasa terrane as a result of the northward subduction of the Neo-Tethys Ocean during the Late Jurassic,although a possible intra-oceanic arc setting cannot be excluded.展开更多
When Western left-wing movement suffered setbacks in reality,its practical experience transformed into a method of text interpretation.However,rare people would ask,how could political practice revive in discourse pra...When Western left-wing movement suffered setbacks in reality,its practical experience transformed into a method of text interpretation.However,rare people would ask,how could political practice revive in discourse practice?This article aims to analyze its transition through the example of Fredric Jameson’s aesthetic application of Mao Zedong’s thoughts.The influence is manifested in three ways:First,the influence of theory—variation through the journey of the text;second,the influence of practice—transformation through the extraction of the context;third,the application of Maoism—to reserve the signifier but convert the signified.In Jameson’s view,Mao Zedong’s thoughts and practice became the focus of theorists and an idealized“otherness”.展开更多
The abundant imagery in Mao Zedong’s poetry is of great political and cultural significance and its English translation plays a major role in spreading New China’s influences worldwide.Comparison reveals that,in tra...The abundant imagery in Mao Zedong’s poetry is of great political and cultural significance and its English translation plays a major role in spreading New China’s influences worldwide.Comparison reveals that,in translations of a particular kind of imagery with supernatural meanings,some translators took a domesticating stance and Christianized some images with supernatural connotations,adding to them strong Western mythological features.It misinterprets the political and cultural connotations of the original,which is harmful to establish a proper political image and cultural confidence,and violates Mao’s translation thoughts and expectations.Christianization and its causes should be critically investigated.New boundaries should be set for foreignization and domestication methods.By viewing the relationships between the translator’s subjectivity and the author’s will,as well as the pursuit of translation effect and the defence of ideological security,new discourse will be explored to tell the Chinese stories with profound political and cultural thoughts in Mao’s poetry in a correct and well-accepted way.展开更多
Based on the bilingual corpus of Selected Works of Mao Zedong from Shaoxing University,this paper intended to study the English Translation of Chinese Idioms of the anthology.By comparing the translation of the idioms...Based on the bilingual corpus of Selected Works of Mao Zedong from Shaoxing University,this paper intended to study the English Translation of Chinese Idioms of the anthology.By comparing the translation of the idioms in different contexts,this paper analyzes the factors influencing Chinese-to-English translation,discusses the methods and strategies for translating Chinese idioms into English,and summarizes innovative conclusions.In addition to improving English proficiency,the process can enhance the learning quality of Chinese and English,translation capability,English-Chinese comparative research ability,and benefit the spreading of time-honored Chinese culture.展开更多
The Mao Zedong Zao Qi Wen Gao[Early Manuscripts of Mao Zedong]is a collection of young Mao Zedong’s manuscripts from 1912 to 1920 and is a record of his growth during his youth.It is worth mentioning that the views o...The Mao Zedong Zao Qi Wen Gao[Early Manuscripts of Mao Zedong]is a collection of young Mao Zedong’s manuscripts from 1912 to 1920 and is a record of his growth during his youth.It is worth mentioning that the views of women’s liberation and progress have a place in Mao Zedong’s early manuscripts.This study focuses on reviewing and discussing the motivation behind young Mao Zedong’s attention to women’s liberation and progress issues,his relevant views in these manuscripts,and how these views played a role in his growth into a Marxist.This study aims to explore,from the perspective of women’s studies,the thought basis and virtues that led young Mao Zedong to become a Marxist.展开更多
The Zedong ophiolites in the eastern Yarlung–Zangbo suture zone of Tibet represent a mantle slice of more than 45 km^2. This massif consists mainly of mantle peridotites, with lesser gabbros, diabases and volcanic ro...The Zedong ophiolites in the eastern Yarlung–Zangbo suture zone of Tibet represent a mantle slice of more than 45 km^2. This massif consists mainly of mantle peridotites, with lesser gabbros, diabases and volcanic rocks. The mantle peridotites are mostly harzburgite, lherzolite; a few dike-like bodies of dunite are also present. Mineral structures show that the peridotites experienced plastic deformation and partial melting. Olivine(Fo89.7–91.2), orthopyroxene(En_(88–92)), clinopyroxene(En_(45–49) Wo_(47–51) Fs_(2–4)) and spinel [Mg~#=100×Mg/(Mg+Fe)]=49.1–70.7; Cr~#=(100×Cr/(Cr+Al)=18.8–76.5] are the major minerals. The degree of partial melting of mantle peridotites is 10%–40%, indicating that the Zedong mantle peridotites may experience a multi–stage process. The peridotites are characterized by depleted major element compositions and low REE content(0.08–0.62 ppm). Their "spoon–shaped" primitive–mantle normalized REE patterns with(La/Sm)_N being 0.50–6.00 indicate that the Zedong ultramafic rocks belong to depleted residual mantle rocks. The PGE content of Zedong peridotites(18.19–50.74 ppb) is similar with primary mantle with Pd/Ir being 0.54–0.60 and Pt/Pd being 1.09–1.66. The Zedong peridotites have variable, unradiogenic Os isotopic compositions with ^(187)Os/^(188)Os=0.1228 to 0.1282. A corollary to this interpretation is that the convecting upper mantle is heterogeneous in Os isotopes. All data of the Zedong peridotites suggest that they formed originally at a mid-ocean ridge(MOR) and were later modified in supra–subduction zone(SSZ) environment.展开更多
Cu–Au mineralization is rare in the Jurassic–Early Tertiary batholiths related to the India–Asia collision. Geochemical analysis and U–Pb isotope chronology was carried out on Shuangbujiere biotite hornblende gran...Cu–Au mineralization is rare in the Jurassic–Early Tertiary batholiths related to the India–Asia collision. Geochemical analysis and U–Pb isotope chronology was carried out on Shuangbujiere biotite hornblende granodiorite from the Zedong area. Zircon grains of the biotite hornblende granodiorite show oscillatory growth zonation and have high Th/U ratios of 1.08–2.39, indicating a magmatic origin for the zircons. Geochrological test yielded a LA-ICP-MS U-Pb age of 51.5±1.0 Ma, suggesting that the emplacement age of the biotite hornblende granodiorite is Early Eocene. The Shuangbujiere biotite hornblende granodiorites have geochemical features characteristic of adakite and are associated with a calc–alkaline metaluminous I-type granite enriched in Sr, high in Mg~#(49.6–54.9) and Sr/Y, and depleted in Y and Yb. These results indicate that this intrusion formation may have been associated with crustal thickening caused by the early collision of the Indian and Eurasian Plates. As the process of crustal thickening continued, the heating of the underplated basaltic magma caused the thickened lower crust amphibolite to dehydrate the melt and form a high-K calc–alkaline adakitic melt at about 848°C. Meanwhile, magma mixing of the underplated basaltic melt and high-K calc–alkaline adakitic melt formed a high-Mg# adakite representative of the sys-collisional tectonic setting.展开更多
文摘This paper explores Mao Zedong’s early views on physical education and practice,focusing on the“Six-Section Exercise”he created.The exercise,which integrates elements from traditional health-preserving techniques,gymnastics,boxing,and military training,was designed to promote balanced physical development,be practical and effective,and require less time per session.The paper argues that Mao Zedong’s views on physical education were grounded in the belief that it could effectively transform individuals and contribute to the creation of a strong sports nation.The paper also discusses the historical context and social trends behind the creation of the“Six-Section Exercise”,including the New Culture Movement and debates between Chinese and Western,static and dynamic,and new and old approaches to physical education.The paper concludes by suggesting that Mao Zedong’s early sports thinking has significant academic value and can provide guidance for the construction of a healthy China today.
文摘The Zedong Terrane forms a discontinuous belt of volcanic and volcaniclastic rocks adjacent to the Yarlung Zangbo River in south eastern Tibet. It extends from Luobusa to 20km west of Zedong. The Zedong Terrane lies within the Indus—Yarlung Zangbo suture zone and may represent an intra\|oceanic island arc that once lay between the Lhasa (Asian) and Himalayan (Indian) terranes. Rare fossils within the terrane indicate active volcanism during the Early Cretaceous.Ultramafic rocks of the Dazhuqu Terrane, including harzburgite and gabbro are thrust over the southern margin of the Zedong Terrane along a steep south\|dipping thrust fault. To the west of Zedong, this fault is marked by a distinctive zone of serpentinite. East of Zedong, the northernmost rocks of the terrane are thrust onto Oligocene molasse deposits of the Luobusa Formation and Cretaceous plutonic rocks of the Gangdese batholith (Lhasa Terrane). These thrusts form part of a northward directed thrust stack \| the Renbu\|Zedong thrust system of Yin et al.., (1994, 1999).
基金Supported by Project of National Social Science Foundation(17BZS084)Program of Major Theoretical and Practical Issues in Shaanxi Province(2017C065)
文摘Former chairman Mao Zedong conducted extensive rural surveys during the exploration of the Chinese revolutionary road. In 1941,in order to change the state of the party's theory separating from reality,Mao Zedong organized and published the book Rural Surveys,which provided the direction for survey and research of the party members. The survey and research are excellent tradition and style of work of the party,and also a major weapon for outstanding achievements in China's revolution and construction. Socialism with Chinese characteristics has entered a new era. Studying the Rural Surveys has important practical value for beating off the new challenges in the issues concerning agriculture,farmers,and rural areas.
基金funded by grants from the Ministry of Science and Technology of China (Sinoprobe-05-02)the NSF China (Nos. 41502062, 41672046, 41202036)+2 种基金the China Geological Survey (Nos. DD20160023)grants from the Institute of Geology, Chinese Academy of Geological Sciences (J1526)IGCP-649
文摘The Yarlung Zangbo suture zone extends more than2000 km along southern Tibet and marks the boundary between the Indian subcontinent and Eurasia.The Zedong terrane has been not suggested to represent the vestige of such an intra-oceanic arc developed within the Neo-Tethys Ocean,as a result of the northward subduction of the Neo-Tethys Ocean during the Late Jurassic.In this study,we present detailed geochemical and geochronological data of various types of magmatic rocks widely exposed in the Zedong terrane to constrain the formation age and tectonic setting of the Zedong terrane.We found that the Zedong volcanic rocks belong to high K2O calc-alkaline series,whereas the diabase and gabbro plotted in the low-K calcalkline.The basalt rocks are highly enriched in LREE and LILE,but strongly depleted in HFSE,indicating they were derived from a metasomatized mantle.Both gabbros and diabase have similar N-MORB geochemistry indicates that the cumulates were produced from MOR setting.Zircons from four samples,including the basalt rocks(158-161Ma)are older than the gabbro(131 Ma),certificate the gabbro are as the vein intrude into the basalt rocks.This suggests that the volcanic eruption and plutonic emplacement were coevally developed in the Zedonghave similar positiveεHf(t)values(+2.0 to+15.6)and(+8.6 to+18.4),indicating they were stemmed from similarly depleted mantle sources,same with the gabbro and granitic rocks from the Gangdese arc.Therefore,we proposed that the basalt rocks in the Zedong terrane were formed through partial melting of the mantle wedge metasomatized by slab-released fluids/melts.A part of hydrous basalts were underplated in the thickened lower crust beneath the Zedong terrane,which gave rise to the cumulate and granitic rocks.This suggests that the Zedong terrane represents a slice of the active continental margin developed on the southern margin of the Lhasa terrane as a result of the northward subduction of the Neo-Tethys Ocean during the Late Jurassic,although a possible intra-oceanic arc setting cannot be excluded.
文摘When Western left-wing movement suffered setbacks in reality,its practical experience transformed into a method of text interpretation.However,rare people would ask,how could political practice revive in discourse practice?This article aims to analyze its transition through the example of Fredric Jameson’s aesthetic application of Mao Zedong’s thoughts.The influence is manifested in three ways:First,the influence of theory—variation through the journey of the text;second,the influence of practice—transformation through the extraction of the context;third,the application of Maoism—to reserve the signifier but convert the signified.In Jameson’s view,Mao Zedong’s thoughts and practice became the focus of theorists and an idealized“otherness”.
文摘The abundant imagery in Mao Zedong’s poetry is of great political and cultural significance and its English translation plays a major role in spreading New China’s influences worldwide.Comparison reveals that,in translations of a particular kind of imagery with supernatural meanings,some translators took a domesticating stance and Christianized some images with supernatural connotations,adding to them strong Western mythological features.It misinterprets the political and cultural connotations of the original,which is harmful to establish a proper political image and cultural confidence,and violates Mao’s translation thoughts and expectations.Christianization and its causes should be critically investigated.New boundaries should be set for foreignization and domestication methods.By viewing the relationships between the translator’s subjectivity and the author’s will,as well as the pursuit of translation effect and the defence of ideological security,new discourse will be explored to tell the Chinese stories with profound political and cultural thoughts in Mao’s poetry in a correct and well-accepted way.
基金This paper is part of the achievements of the 2021 Shanghai College Student’Innovation and Entrepreneurship Project“English Translation and Dissemination of Selected Works of Mao Zedong”(No.SH2021146).
文摘Based on the bilingual corpus of Selected Works of Mao Zedong from Shaoxing University,this paper intended to study the English Translation of Chinese Idioms of the anthology.By comparing the translation of the idioms in different contexts,this paper analyzes the factors influencing Chinese-to-English translation,discusses the methods and strategies for translating Chinese idioms into English,and summarizes innovative conclusions.In addition to improving English proficiency,the process can enhance the learning quality of Chinese and English,translation capability,English-Chinese comparative research ability,and benefit the spreading of time-honored Chinese culture.
基金Chengdu Social Science Project titled“On the Sociological Origins of How Young Mao Zedong Became a Marxist”(No.2019R19).
文摘The Mao Zedong Zao Qi Wen Gao[Early Manuscripts of Mao Zedong]is a collection of young Mao Zedong’s manuscripts from 1912 to 1920 and is a record of his growth during his youth.It is worth mentioning that the views of women’s liberation and progress have a place in Mao Zedong’s early manuscripts.This study focuses on reviewing and discussing the motivation behind young Mao Zedong’s attention to women’s liberation and progress issues,his relevant views in these manuscripts,and how these views played a role in his growth into a Marxist.This study aims to explore,from the perspective of women’s studies,the thought basis and virtues that led young Mao Zedong to become a Marxist.
基金supported by the Project IGCP–649the China Geological Survey(No.DD20160023–01)
文摘The Zedong ophiolites in the eastern Yarlung–Zangbo suture zone of Tibet represent a mantle slice of more than 45 km^2. This massif consists mainly of mantle peridotites, with lesser gabbros, diabases and volcanic rocks. The mantle peridotites are mostly harzburgite, lherzolite; a few dike-like bodies of dunite are also present. Mineral structures show that the peridotites experienced plastic deformation and partial melting. Olivine(Fo89.7–91.2), orthopyroxene(En_(88–92)), clinopyroxene(En_(45–49) Wo_(47–51) Fs_(2–4)) and spinel [Mg~#=100×Mg/(Mg+Fe)]=49.1–70.7; Cr~#=(100×Cr/(Cr+Al)=18.8–76.5] are the major minerals. The degree of partial melting of mantle peridotites is 10%–40%, indicating that the Zedong mantle peridotites may experience a multi–stage process. The peridotites are characterized by depleted major element compositions and low REE content(0.08–0.62 ppm). Their "spoon–shaped" primitive–mantle normalized REE patterns with(La/Sm)_N being 0.50–6.00 indicate that the Zedong ultramafic rocks belong to depleted residual mantle rocks. The PGE content of Zedong peridotites(18.19–50.74 ppb) is similar with primary mantle with Pd/Ir being 0.54–0.60 and Pt/Pd being 1.09–1.66. The Zedong peridotites have variable, unradiogenic Os isotopic compositions with ^(187)Os/^(188)Os=0.1228 to 0.1282. A corollary to this interpretation is that the convecting upper mantle is heterogeneous in Os isotopes. All data of the Zedong peridotites suggest that they formed originally at a mid-ocean ridge(MOR) and were later modified in supra–subduction zone(SSZ) environment.
基金financially supported by China Geological Survey(grant no.12120113095700,12120101000015001108)the National Science Foundation of China(grant no.41403039)the training program for young and middle aged backbone teachers of Chengdu Universcechnology(grant no.KYGG201502)
文摘Cu–Au mineralization is rare in the Jurassic–Early Tertiary batholiths related to the India–Asia collision. Geochemical analysis and U–Pb isotope chronology was carried out on Shuangbujiere biotite hornblende granodiorite from the Zedong area. Zircon grains of the biotite hornblende granodiorite show oscillatory growth zonation and have high Th/U ratios of 1.08–2.39, indicating a magmatic origin for the zircons. Geochrological test yielded a LA-ICP-MS U-Pb age of 51.5±1.0 Ma, suggesting that the emplacement age of the biotite hornblende granodiorite is Early Eocene. The Shuangbujiere biotite hornblende granodiorites have geochemical features characteristic of adakite and are associated with a calc–alkaline metaluminous I-type granite enriched in Sr, high in Mg~#(49.6–54.9) and Sr/Y, and depleted in Y and Yb. These results indicate that this intrusion formation may have been associated with crustal thickening caused by the early collision of the Indian and Eurasian Plates. As the process of crustal thickening continued, the heating of the underplated basaltic magma caused the thickened lower crust amphibolite to dehydrate the melt and form a high-K calc–alkaline adakitic melt at about 848°C. Meanwhile, magma mixing of the underplated basaltic melt and high-K calc–alkaline adakitic melt formed a high-Mg# adakite representative of the sys-collisional tectonic setting.
