Dispatched by the Chinese government,a multidisciplinary team of 30 researchers collaborated with a team from Myanmar to conduct a 14-day on-site investigation.The work encompassed seismic intensity assessments,field ...Dispatched by the Chinese government,a multidisciplinary team of 30 researchers collaborated with a team from Myanmar to conduct a 14-day on-site investigation.The work encompassed seismic intensity assessments,field surveys,and loss evaluations.The paper focuses on the intensity distribution and structural damage characteristics of the 2025 M7.9 Myanmar earthquake,yielding the following key findings.(1)The seismogenic fault rupture propagated in a nearly N-S direction,with a surface rupture length of approximately 450 km.The seismic impact zone exhibited an elongated N-S distribution and a shorter E-W span,distributed like a belt around the seismogenic fault.(2)Within the seismic impact zones,existing buildings comprised five primary structural types,with timber(bamboo)structures constituting the largest proportion(≈80%in rural areas,≈50%in urban areas).The relatively low disaster losses and casualties were primarily attributable to the good seismic performance and low damage ratio of timber(bamboo)structures across varying intensity zones.(3)An anomalous zone of intensityⅨwas located at the boundary between intensityⅥandⅦregions in Nay Pyi Taw.Here,ridge topography combined with soft soil layers significantly amplified ground motion,exacerbating structural damage.(4)Directional effects of ground motion were observed,with the structural damage phenomena and peak ground acceleration(PGA)values in the N-S direction exceeding those in the E-W direction.This validates that the maximum PGA distribution of strike-slip fault earthquakes aligns with the fault strike.The research is expected to provide technical support for post-disaster reconstruction planning,site selection,and disaster mitigation strategies in Myanmar.展开更多
On March 28,2025,an M_(w) 7.7 earthquake struck near Mandalay,Myanmar,producing intense ground shaking.Strong motion recorded at a station close to the fault indicated a peak ground acceleration of 1.066 g in the vert...On March 28,2025,an M_(w) 7.7 earthquake struck near Mandalay,Myanmar,producing intense ground shaking.Strong motion recorded at a station close to the fault indicated a peak ground acceleration of 1.066 g in the vertical direction and 0.631 g in the horizontal direction.The earthquake caused collapse or severe damage of numerous buildings,resulting in thousands of fatalities and injuries,as well as substantial economic losses.The authors participated in the post-earthquake emergency response as members of the China Search and Rescue Team.During the rescue operations,an investigation into the characteristics of collapsed structures was conducted and the stability of building debris was assessed to ensure the safety of rescue efforts.Subsequently,a rapid seismic safety assessment of affected structures was carried out,including nine city residential blocks,two hospitals,and two apartments.Preliminary analyses indicate that the main causes of structural failure were insufficient cross-sectional dimensions of beams and columns,inadequate stirrup reinforcement,and lack of structural redundancy.展开更多
Traditional medicine in Myanmar has a long history,combining the local natural environment,culture,and religious beliefs to form a unique medical system.This article adopts the method of literature research,focusing o...Traditional medicine in Myanmar has a long history,combining the local natural environment,culture,and religious beliefs to form a unique medical system.This article adopts the method of literature research,focusing on the existing book“Milestones of Traditional Medicine in Myanmar”,and reviewing existing literature to analyze historical and contemporary sources.Elaborate on the question of how the history of traditional medicine in Myanmar originated and has continued to develop until now.These histories have proven that traditional medicine in Myanmar,despite facing numerous obstacles,has always been used by the people of Myanmar and has unique value,which deserves our continued attention and inheritance.展开更多
INTRODUCTION On March 28,2025,at 06:20:52 UTC,a shallow,magnitude M_(w)7.7 earthquake struck Myanmar(Burma)with an epicenter near the major city of Mandalay.This event,the strongest seismic activity recorded in Myanma...INTRODUCTION On March 28,2025,at 06:20:52 UTC,a shallow,magnitude M_(w)7.7 earthquake struck Myanmar(Burma)with an epicenter near the major city of Mandalay.This event,the strongest seismic activity recorded in Myanmar since 1950,generated intense shaking across much of the country,extended into regions of Thailand,and was felt in China's Yunnan and Guangxi provinces.展开更多
This article is based on remarks delivered by U Tin Maung Swe,Myanmar Ambassador to China,at the ASEAN-China(Beijing Municipal Administrative Center)Trade and Investment Promotion Conference,and has been edited for cl...This article is based on remarks delivered by U Tin Maung Swe,Myanmar Ambassador to China,at the ASEAN-China(Beijing Municipal Administrative Center)Trade and Investment Promotion Conference,and has been edited for clarity and readability.展开更多
Eastern Myanmar is the key position linking between SW Yunnan and northern Thailand for better understanding of Tethyan evolution.However,the actual location and evolution of the Tethyan suture zone are still unclear ...Eastern Myanmar is the key position linking between SW Yunnan and northern Thailand for better understanding of Tethyan evolution.However,the actual location and evolution of the Tethyan suture zone are still unclear in eastern Myanmar.The present study focuses on the geochronological,geochemical and zircon Lu-Hf isotopic study on the plutonic rocks,including granite,diorite and gabbroic rocks,from the Tachileik area,eastern Myanmar.These plutonic rocks yielded zircon U-Pb weighted mean ages of ca.353–355 Ma,suggesting the Early Carboniferous emplacement.The Tachileik granites are high-K calc-alkaline,weakly peraluminous and have low P2O5 contents,which are typical features of I-type granites.They have positive zircon ε_(Hf)(t)values(+4.5−+7.4)with T_(DM2) ages of 981–825 Ma,indicating a juvenile mafic lower crust source.The Tachileik gabbros and diorites show high Al_(2)O_(3) contents and Mg#,but low TiO_(2) and K_(2)O contents,belonging to tholeiitic and calc-alkaline basalt series.They are characterized by enrichments in large ion lithophile elements(LILEs,e.g.,Rb,Ba and Sr),depletions in high field strength elements(HFSEs)and distinctly negative Nb and Ta anomalies,similar to the volcanic arc basalt.The zircon Hf isotopic(+4.7−+7.1)and whole-rock geochemical data imply that the Tachileik gabros and diorites probably resulted from partial melting of lithospheric mantle in the spinel stability field within an arc-related setting.The magmatic rocks can be grouped to the Late Devonian–Early Carboniferous magmatic rock and pyroclastic rock zone from SW Yunnan to northern Thailand based on their age and geochemical characters.The zone was formed in the post-collisional extension-related tectonic setting of the Proto-Tethys.This study provides important evidences for the evolution of the Proto-Tethys in Southwest Yunnan and Southeast Asia.展开更多
On the evening of January 5,the 2025 China-Myanmar Cross-Border Spring Festival Gala was held under the theme“One River,One Family”in Dehong Prefecture,southwest China’s Yunnan Province.During the event,a ceremony ...On the evening of January 5,the 2025 China-Myanmar Cross-Border Spring Festival Gala was held under the theme“One River,One Family”in Dehong Prefecture,southwest China’s Yunnan Province.During the event,a ceremony was held for the inauguration of the“Paukphaw(‘fraternal’in Burmese)Mingalaba(‘Nice to meet you!’)”China-Myanmar People-to-People Exchange Base jointly established by the Center for Asia-Pacific under China International Communications Group(CICG Asia-Pacific)and the government of Dehong Prefecture.Distinguished vips attending the ceremony included Zhao Jun,editor-in-chief of CICG Asia-Pacific,Sun Jie,deputy secretary of the Dehong Prefecture Committee of the Communist Party of China(CPC)and chief of the Publicity Department of the Committee,U Thwin Htet Lin,Consul-General of Myanmar in Kunming,and U Ang Ruomo,chief executive officer of the Muse Township Government of Myanmar.展开更多
On March 28,2025,a catastrophic M 7.9 earthquake shook central Myanmar,causing extensive damage to buildings,significant casualties,and substantial economic loss,making it one of the most severe natural disasters Myan...On March 28,2025,a catastrophic M 7.9 earthquake shook central Myanmar,causing extensive damage to buildings,significant casualties,and substantial economic loss,making it one of the most severe natural disasters Myanmar has faced in recent years.During an on-site investigation that lasted two weeks,widely spreading liquefaction phenomena and associated damage to buildings and other facilities were investigated in 16 villages or districts in the seismic zones,involving hundreds of residential houses,two large bridges,underground storage tanks,etc.Ground fissures generated by liquefaction tore apart houses,which contributed to a significant impact on house damage.The loss of ground bearing capacity is another impact of liquefaction with regard to structural damage,causing the subsidence and tilting of houses.Several consequences of liquefaction were identified,such as lateral spreading,which demolishes houses and causes casualties,as well as damage to two large bridges as a result of lateral spreading.The cases of liquefaction following the Myanmar earthquake reported on herein provide data and lessons for future seismic desigs to help prevent such disasters in Southeast Asia.Through analyzing the phenomena and characteristics of soil liquefaction,the methods and techniques for liquefaction hazard mitigation in other countries also can be improved.展开更多
Myanmar has long been involved in the Lancang-Mekong Cooperation(LMC)mechanism,becoming the country with the most approved projects under the LMC Special Fund.Development in areas such as agriculture,animal husbandry,...Myanmar has long been involved in the Lancang-Mekong Cooperation(LMC)mechanism,becoming the country with the most approved projects under the LMC Special Fund.Development in areas such as agriculture,animal husbandry,and infrastructure has benefited significantly,and poverty has been alleviated to some extent.Although China has faced challenges in advancing poverty reduction projects within the LMC framework in Myanmar in recent years,poverty reduction cooperation between the two countries will overcome di$culties and persist.展开更多
During this year’s“two sessions”(annual meetings of China’s top legislative and political advisory bodies)from March 4 to 11,Chinese Premier Li Qiang delivered the Government Work Report on March 5,and Foreign Min...During this year’s“two sessions”(annual meetings of China’s top legislative and political advisory bodies)from March 4 to 11,Chinese Premier Li Qiang delivered the Government Work Report on March 5,and Foreign Minister Wang Yi answered questions from Chinese and foreign reporters on China’s foreign policy and foreign relations at a March 7 press conference.展开更多
During this year’s Two Sessions(annual meetings of China’s top legislative and political advisory bodies),Wei Gang,deputy to the National People’s Congress and governor of Dehong Dai and Jingpo Autonomous Prefectur...During this year’s Two Sessions(annual meetings of China’s top legislative and political advisory bodies),Wei Gang,deputy to the National People’s Congress and governor of Dehong Dai and Jingpo Autonomous Prefecture,Yunnan Province,sat down for an exclusive interview with China Report ASEAN.展开更多
On March 28,2025,an M_(w) 7.7 earthquake struck Myanmar,causing extensive damage to engineering facilities,causing thousands of casualties.In addition,at 2 km-by-2 km square,Mandalay Royal Palace,famous as an importan...On March 28,2025,an M_(w) 7.7 earthquake struck Myanmar,causing extensive damage to engineering facilities,causing thousands of casualties.In addition,at 2 km-by-2 km square,Mandalay Royal Palace,famous as an important historical and cultural relic facility,also suffered significant damage.A detailed field investigation took place after the earthquake,with subsequent analysis of post-earthquake high-resolution remote sensing images.It was found that damage was concentrated primarily to the four exterior walls of the palace.Specifically,many parts of the walls broke off or collapsed,and some of the palace gates and watchtowers on the walls were destroyed or even collapsed.The collapse rate of the palace gates was significantly higher than that of the watchtowers and palace walls,and the degree of damage to the north and south sides of the palace walls was significantly higher than that of the east or west sides.This special spatial damage distribution may be related to the strike-slip movement of the Sagaing fault.The research results not only serve as a valuable reference for understanding the ground motion characteristics of this destructive earthquake but also help learn lessons to better protect cultural relics against the effects of future earthquakes.展开更多
The March 28,2025 Myanmar earthquake generated ground shaking that was perceptible throughout Myanmar and adjacent regions.This study simulated three-component ground motions across the affected region using an improv...The March 28,2025 Myanmar earthquake generated ground shaking that was perceptible throughout Myanmar and adjacent regions.This study simulated three-component ground motions across the affected region using an improved stochastic finite-fault method to systematically assess seismic impacts.Observed near-field recordings at MM.NGU station was used to determine the reliability of the theoretically derived stress drop as input for simulation.Far-field recordings constrained the frequency-dependent S-wave quality factors(Q(f)=283.305f^(0.588))for anelastic attenuation modeling.Comparisons of peak accelerations between simulation and empirical ground-motion models showed good agreement at moderate-to-large distances.However,lower near-fault simulations indicate a weaker-than-average source effect.Analysis of simulated instrumental seismic intensity revealed key patterns.Maximum intensity(Ⅹ)occurred in isolated patches within the ruptured fault projection,correlating with shallow high-slip areas.TheⅨ-intensity zone formed a north-south elongated band centered on fault projection.Significant asymmetry inⅧ-intensity distribution perpendicular to the fault strike was observed,with a wider western extension attributed to lower shear-wave velocities west of the fault.Supershear rupture behavior enhanced ground motions,expanding intensity ranges by~20%compared to sub-shear rupture.This study reveals the integrated effects of fault geometry,slip spatial distribution,rupture velocity,and site condition in governing ground motion patterns.展开更多
After the earthquake struck Myanmar on March 28th,China NGO Network for International Exchanges(CNIE)immediately contacted the emergency management department for the registration process of non-governmental rescue fo...After the earthquake struck Myanmar on March 28th,China NGO Network for International Exchanges(CNIE)immediately contacted the emergency management department for the registration process of non-governmental rescue forces participating in earthquake relief work and guided its member organisations and partners to orderly participate in the disaster relief.展开更多
A great earthquake struck central Myanmar on March 28,2025,causing extensive and severe damage in Myanmar and neighboring countries such as Thailand.Observed waveforms indicated the possibility of supershear rupture a...A great earthquake struck central Myanmar on March 28,2025,causing extensive and severe damage in Myanmar and neighboring countries such as Thailand.Observed waveforms indicated the possibility of supershear rupture at the source of this event.To investigate this possibility,a joint source inversion using near-field and teleseismic waveforms was performed.The fault model used,with a total length of 580 km,comprises five segments with varying strike directions and dip angles.Within the first 10 s after initiation at the hypocenter,the rupture propagated southward at a high speed of 5–6 km/s.while rupture in the northern direction proceeded at a speed lower than the local S-wave velocity of 3.5 km/s.Subsequently,the rupture propagated bilaterally in both northern and southern directions at high speeds of 5–6 km/s.The largest asperity,with a maximum slip of 5–6 m,occurred in the shallow part of the fault model,approximately 240 km south of the hypocenter.Large slips of 2–3 m were also found near the southern end of the fault model.Slips on the fault plane were dominated by strike-slip components,though slips south of the largest asperity included significant dip-slip components.展开更多
On April 26,the China Foundation for Peace and Development(CFPD),in collaboration with the Shenzhen Foundation for International Exchange and Cooperation(SFIEC),the Shenzhen Ye Chenghai Charity Foundation and the Chin...On April 26,the China Foundation for Peace and Development(CFPD),in collaboration with the Shenzhen Foundation for International Exchange and Cooperation(SFIEC),the Shenzhen Ye Chenghai Charity Foundation and the China-Myanmar Economic Cooperation and Development Promotion Association(Myanmar),held a handover ceremony at Yangon Airport to donate five tons of medicine to the disasterstricken areas of Myanmar.展开更多
Along China's southwestern border,Dehong Dai and Jingpo Autonomous Prefecture in Yunnan Province shares mountains,rivers,ethnic ties,and cultural connections with Myanmar.This land,imbued with the spirit of the pa...Along China's southwestern border,Dehong Dai and Jingpo Autonomous Prefecture in Yunnan Province shares mountains,rivers,ethnic ties,and cultural connections with Myanmar.This land,imbued with the spirit of the pauk-phaw friendship(pauk-phaw means fraternal in Myanmar language),has in recent years been exploring innovative approaches to international communication with Myanmar.Centered on serving the Belt and Road Initiative(BRI)and building a China-Myanmar community with a shared future,Dehong has incorporated the vision of“Mingalaba”(auspiciousness in Myanmar language)into its cross-border communication e"orts,sharing stories of China-Myanmar friendship with people far and wide.展开更多
Over 70 years ago,China proposed the Five Principles of Peaceful Coexistence,which were first embraced by countries such as Myanmar and gradually gained traction across Asia.The Five Principles eventually became widel...Over 70 years ago,China proposed the Five Principles of Peaceful Coexistence,which were first embraced by countries such as Myanmar and gradually gained traction across Asia.The Five Principles eventually became widely recognized norms in international relations and foundational principles of international law,contributing significantly to the post-World War II international order.Decades on,the Five Principles have not faded into history.Rather,they have demonstrated renewed relevance in today’s complex global landscape.展开更多
Mesozoic ophiolites crop out discontinuously in the Indo-Myanmar Ranges in NE India and Myanmar,and represent the remnants of the Neotethyan oceanic lithosphere(Sengupta et al.,1990;Mitchell,1993).These ophiolites in ...Mesozoic ophiolites crop out discontinuously in the Indo-Myanmar Ranges in NE India and Myanmar,and represent the remnants of the Neotethyan oceanic lithosphere(Sengupta et al.,1990;Mitchell,1993).These ophiolites in the Indo-Myanmar Ranges are the southern continuation of the Neotethyan ophiolites occurring along the Yarlung Zangbo Suture Zone(YZSZ)in southern Tibet farther northwest(Mitchell,1993;Fareeduddin and Dilek,2015),as indicated by their coeval crystallization ages and geochemical compositions(Yang et al.,2012;Liu et al.,2016).The Kalaymyo ophiolite is located in the central part of the eastern Indo-Myanmar Ranges(Fig.1).composition of these ophiolites from the central Tibetan Plateau(CTP)is dominated by MORBs and minor OIBs and a distinct lack of IATs and BONs,which is inconsistent with most ophiolites worldwide(Robinson and Zhou,2008;Zhang et al.,2008).But the generation and tectonic nature of these ophiolites are still controversial.*The Kalaymyo peridotites consist mainly of harzburgites,which show typical porphyroclastic or coarse-grained equigranular textures.They are composed ofolivine(Fo=89.8–90.5),orthopyroxene(En86-91Wo1-4Fs8-10;Mg#=89.6–91.9),clinopyroxene(En46-49Wo47-50Fs3-5;Mg#=90.9–93.6)and spinel(Mg#=67.1–78.9;Cr#=13.5–31.5),and have relatively homogeneous whole-rock compositions with Mg#s of90.1–90.8 and Si O2(41.5–43.65 wt.%),Al2O3(1.66–2.66wt.%)and Ca O(1.45–2.67 wt.%)contents.TheydisplayLightRareEarthElement(LREE)-depleted chondrite-normalized REE patterns with(La/Yb)CN=0.04–0.21 and(Gd/Yb)CN=0.40–0.84,and show a slight enrichment from Pr to La with(La/Pr)CN in the range of 0.98–2.36.The Kalaymyo peridotites are characterized by Pd-enriched chondrite-normalized PGE patterns with superchondritic(Pd/Ir)CN ratios(1.15–2.36).Their calculated oxygen fugacities range between QFM–0.57 and QFM+0.90.These mineralogical and geochemical features collectively suggest that the Kalaymyo peridotites represent residual upper mantle rocks after low to moderate degrees(5–15%)of partial melting at a mid-ocean-ridge(MOR)environment.The observed enrichment in LREE and Pd was a result of their reactions with enriched MORB-like melts,percolating through these already depleted,residual peridotites.The Kalaymyo and other ophiolites in the Indo-Myanmar Ranges hence represent mid-ocean ridge(MOR)–type Tethyan oceanic lithosphere derived from a downgoing plate and accreted into a westward migrating subduction–accretion system along the eastern margin of India.展开更多
基金National Natural Science Foundation of China under Grant No.U2239252National Natural Science Foundation of China under Grant No.52279128Natural Science Foundation of Heilongjiang Province of China under Grant No.YQ2022E013。
文摘Dispatched by the Chinese government,a multidisciplinary team of 30 researchers collaborated with a team from Myanmar to conduct a 14-day on-site investigation.The work encompassed seismic intensity assessments,field surveys,and loss evaluations.The paper focuses on the intensity distribution and structural damage characteristics of the 2025 M7.9 Myanmar earthquake,yielding the following key findings.(1)The seismogenic fault rupture propagated in a nearly N-S direction,with a surface rupture length of approximately 450 km.The seismic impact zone exhibited an elongated N-S distribution and a shorter E-W span,distributed like a belt around the seismogenic fault.(2)Within the seismic impact zones,existing buildings comprised five primary structural types,with timber(bamboo)structures constituting the largest proportion(≈80%in rural areas,≈50%in urban areas).The relatively low disaster losses and casualties were primarily attributable to the good seismic performance and low damage ratio of timber(bamboo)structures across varying intensity zones.(3)An anomalous zone of intensityⅨwas located at the boundary between intensityⅥandⅦregions in Nay Pyi Taw.Here,ridge topography combined with soft soil layers significantly amplified ground motion,exacerbating structural damage.(4)Directional effects of ground motion were observed,with the structural damage phenomena and peak ground acceleration(PGA)values in the N-S direction exceeding those in the E-W direction.This validates that the maximum PGA distribution of strike-slip fault earthquakes aligns with the fault strike.The research is expected to provide technical support for post-disaster reconstruction planning,site selection,and disaster mitigation strategies in Myanmar.
基金National Natural Science Foundation of China for Distinguished Young Scholars under Grant No.52125806Scientific Research Fund of Institute of Engineering Mechanics,China Earthquake Administration under Grant No.2021B03。
文摘On March 28,2025,an M_(w) 7.7 earthquake struck near Mandalay,Myanmar,producing intense ground shaking.Strong motion recorded at a station close to the fault indicated a peak ground acceleration of 1.066 g in the vertical direction and 0.631 g in the horizontal direction.The earthquake caused collapse or severe damage of numerous buildings,resulting in thousands of fatalities and injuries,as well as substantial economic losses.The authors participated in the post-earthquake emergency response as members of the China Search and Rescue Team.During the rescue operations,an investigation into the characteristics of collapsed structures was conducted and the stability of building debris was assessed to ensure the safety of rescue efforts.Subsequently,a rapid seismic safety assessment of affected structures was carried out,including nine city residential blocks,two hospitals,and two apartments.Preliminary analyses indicate that the main causes of structural failure were insufficient cross-sectional dimensions of beams and columns,inadequate stirrup reinforcement,and lack of structural redundancy.
基金2020 Yunnan Province International Commissioner(Individual)Recognition Work Project(202003AK140041)2024 Yunnan Provincial Philosophy and Social Science Innovation Team:Research on the Exchange and Integration of Traditional Medicine in Yunnan(2024CX09)2023 Hospital-level Project of School of Basic Medical Sciences,Yunnan University of Traditional Chinese Medicine,“Comparison and Research on Traditional Medicine Treatment Methods in China and Burma”(2023CBMS009).
文摘Traditional medicine in Myanmar has a long history,combining the local natural environment,culture,and religious beliefs to form a unique medical system.This article adopts the method of literature research,focusing on the existing book“Milestones of Traditional Medicine in Myanmar”,and reviewing existing literature to analyze historical and contemporary sources.Elaborate on the question of how the history of traditional medicine in Myanmar originated and has continued to develop until now.These histories have proven that traditional medicine in Myanmar,despite facing numerous obstacles,has always been used by the people of Myanmar and has unique value,which deserves our continued attention and inheritance.
基金supported by the National Key R&D Program of the Republic of China(Nos.2023YFC3007303,2017YFB0504104)the Science and Technology Projects of Gansu Provincial(No.24JRRA1188)。
文摘INTRODUCTION On March 28,2025,at 06:20:52 UTC,a shallow,magnitude M_(w)7.7 earthquake struck Myanmar(Burma)with an epicenter near the major city of Mandalay.This event,the strongest seismic activity recorded in Myanmar since 1950,generated intense shaking across much of the country,extended into regions of Thailand,and was felt in China's Yunnan and Guangxi provinces.
文摘This article is based on remarks delivered by U Tin Maung Swe,Myanmar Ambassador to China,at the ASEAN-China(Beijing Municipal Administrative Center)Trade and Investment Promotion Conference,and has been edited for clarity and readability.
基金supported by the National Natural Science Foundation of China(No.41672222)the State Key Laboratory of Geological Process and Mineral Resources,China University of Geosciences,Wuhan.
文摘Eastern Myanmar is the key position linking between SW Yunnan and northern Thailand for better understanding of Tethyan evolution.However,the actual location and evolution of the Tethyan suture zone are still unclear in eastern Myanmar.The present study focuses on the geochronological,geochemical and zircon Lu-Hf isotopic study on the plutonic rocks,including granite,diorite and gabbroic rocks,from the Tachileik area,eastern Myanmar.These plutonic rocks yielded zircon U-Pb weighted mean ages of ca.353–355 Ma,suggesting the Early Carboniferous emplacement.The Tachileik granites are high-K calc-alkaline,weakly peraluminous and have low P2O5 contents,which are typical features of I-type granites.They have positive zircon ε_(Hf)(t)values(+4.5−+7.4)with T_(DM2) ages of 981–825 Ma,indicating a juvenile mafic lower crust source.The Tachileik gabbros and diorites show high Al_(2)O_(3) contents and Mg#,but low TiO_(2) and K_(2)O contents,belonging to tholeiitic and calc-alkaline basalt series.They are characterized by enrichments in large ion lithophile elements(LILEs,e.g.,Rb,Ba and Sr),depletions in high field strength elements(HFSEs)and distinctly negative Nb and Ta anomalies,similar to the volcanic arc basalt.The zircon Hf isotopic(+4.7−+7.1)and whole-rock geochemical data imply that the Tachileik gabros and diorites probably resulted from partial melting of lithospheric mantle in the spinel stability field within an arc-related setting.The magmatic rocks can be grouped to the Late Devonian–Early Carboniferous magmatic rock and pyroclastic rock zone from SW Yunnan to northern Thailand based on their age and geochemical characters.The zone was formed in the post-collisional extension-related tectonic setting of the Proto-Tethys.This study provides important evidences for the evolution of the Proto-Tethys in Southwest Yunnan and Southeast Asia.
文摘On the evening of January 5,the 2025 China-Myanmar Cross-Border Spring Festival Gala was held under the theme“One River,One Family”in Dehong Prefecture,southwest China’s Yunnan Province.During the event,a ceremony was held for the inauguration of the“Paukphaw(‘fraternal’in Burmese)Mingalaba(‘Nice to meet you!’)”China-Myanmar People-to-People Exchange Base jointly established by the Center for Asia-Pacific under China International Communications Group(CICG Asia-Pacific)and the government of Dehong Prefecture.Distinguished vips attending the ceremony included Zhao Jun,editor-in-chief of CICG Asia-Pacific,Sun Jie,deputy secretary of the Dehong Prefecture Committee of the Communist Party of China(CPC)and chief of the Publicity Department of the Committee,U Thwin Htet Lin,Consul-General of Myanmar in Kunming,and U Ang Ruomo,chief executive officer of the Muse Township Government of Myanmar.
基金Scientific Research Fund of Institute of Engineering Mechanics,China Earthquake Administration under Grant No.2024A03。
文摘On March 28,2025,a catastrophic M 7.9 earthquake shook central Myanmar,causing extensive damage to buildings,significant casualties,and substantial economic loss,making it one of the most severe natural disasters Myanmar has faced in recent years.During an on-site investigation that lasted two weeks,widely spreading liquefaction phenomena and associated damage to buildings and other facilities were investigated in 16 villages or districts in the seismic zones,involving hundreds of residential houses,two large bridges,underground storage tanks,etc.Ground fissures generated by liquefaction tore apart houses,which contributed to a significant impact on house damage.The loss of ground bearing capacity is another impact of liquefaction with regard to structural damage,causing the subsidence and tilting of houses.Several consequences of liquefaction were identified,such as lateral spreading,which demolishes houses and causes casualties,as well as damage to two large bridges as a result of lateral spreading.The cases of liquefaction following the Myanmar earthquake reported on herein provide data and lessons for future seismic desigs to help prevent such disasters in Southeast Asia.Through analyzing the phenomena and characteristics of soil liquefaction,the methods and techniques for liquefaction hazard mitigation in other countries also can be improved.
文摘Myanmar has long been involved in the Lancang-Mekong Cooperation(LMC)mechanism,becoming the country with the most approved projects under the LMC Special Fund.Development in areas such as agriculture,animal husbandry,and infrastructure has benefited significantly,and poverty has been alleviated to some extent.Although China has faced challenges in advancing poverty reduction projects within the LMC framework in Myanmar in recent years,poverty reduction cooperation between the two countries will overcome di$culties and persist.
文摘During this year’s“two sessions”(annual meetings of China’s top legislative and political advisory bodies)from March 4 to 11,Chinese Premier Li Qiang delivered the Government Work Report on March 5,and Foreign Minister Wang Yi answered questions from Chinese and foreign reporters on China’s foreign policy and foreign relations at a March 7 press conference.
文摘During this year’s Two Sessions(annual meetings of China’s top legislative and political advisory bodies),Wei Gang,deputy to the National People’s Congress and governor of Dehong Dai and Jingpo Autonomous Prefecture,Yunnan Province,sat down for an exclusive interview with China Report ASEAN.
基金Scientific Research Fund of Institute of Engineering Mechanics,China Earthquake Administration under Grant No.2024C26the Earthquake Science and Technology Spark Program under Grant No.XH24038YB。
文摘On March 28,2025,an M_(w) 7.7 earthquake struck Myanmar,causing extensive damage to engineering facilities,causing thousands of casualties.In addition,at 2 km-by-2 km square,Mandalay Royal Palace,famous as an important historical and cultural relic facility,also suffered significant damage.A detailed field investigation took place after the earthquake,with subsequent analysis of post-earthquake high-resolution remote sensing images.It was found that damage was concentrated primarily to the four exterior walls of the palace.Specifically,many parts of the walls broke off or collapsed,and some of the palace gates and watchtowers on the walls were destroyed or even collapsed.The collapse rate of the palace gates was significantly higher than that of the watchtowers and palace walls,and the degree of damage to the north and south sides of the palace walls was significantly higher than that of the east or west sides.This special spatial damage distribution may be related to the strike-slip movement of the Sagaing fault.The research results not only serve as a valuable reference for understanding the ground motion characteristics of this destructive earthquake but also help learn lessons to better protect cultural relics against the effects of future earthquakes.
基金National Key R&D Program of China under Grant No.2022YFC3003601。
文摘The March 28,2025 Myanmar earthquake generated ground shaking that was perceptible throughout Myanmar and adjacent regions.This study simulated three-component ground motions across the affected region using an improved stochastic finite-fault method to systematically assess seismic impacts.Observed near-field recordings at MM.NGU station was used to determine the reliability of the theoretically derived stress drop as input for simulation.Far-field recordings constrained the frequency-dependent S-wave quality factors(Q(f)=283.305f^(0.588))for anelastic attenuation modeling.Comparisons of peak accelerations between simulation and empirical ground-motion models showed good agreement at moderate-to-large distances.However,lower near-fault simulations indicate a weaker-than-average source effect.Analysis of simulated instrumental seismic intensity revealed key patterns.Maximum intensity(Ⅹ)occurred in isolated patches within the ruptured fault projection,correlating with shallow high-slip areas.TheⅨ-intensity zone formed a north-south elongated band centered on fault projection.Significant asymmetry inⅧ-intensity distribution perpendicular to the fault strike was observed,with a wider western extension attributed to lower shear-wave velocities west of the fault.Supershear rupture behavior enhanced ground motions,expanding intensity ranges by~20%compared to sub-shear rupture.This study reveals the integrated effects of fault geometry,slip spatial distribution,rupture velocity,and site condition in governing ground motion patterns.
文摘After the earthquake struck Myanmar on March 28th,China NGO Network for International Exchanges(CNIE)immediately contacted the emergency management department for the registration process of non-governmental rescue forces participating in earthquake relief work and guided its member organisations and partners to orderly participate in the disaster relief.
基金Scientific Research Fund of Institute of Engineering Mechanics,China Earthquake Administration under Grant No.2024B15National Natural Science Fundation of China under Grant Nos.U2239252 and 52478567Natural Science Foundation of Heilongjiang Province under Grant No.JQ2023E002。
文摘A great earthquake struck central Myanmar on March 28,2025,causing extensive and severe damage in Myanmar and neighboring countries such as Thailand.Observed waveforms indicated the possibility of supershear rupture at the source of this event.To investigate this possibility,a joint source inversion using near-field and teleseismic waveforms was performed.The fault model used,with a total length of 580 km,comprises five segments with varying strike directions and dip angles.Within the first 10 s after initiation at the hypocenter,the rupture propagated southward at a high speed of 5–6 km/s.while rupture in the northern direction proceeded at a speed lower than the local S-wave velocity of 3.5 km/s.Subsequently,the rupture propagated bilaterally in both northern and southern directions at high speeds of 5–6 km/s.The largest asperity,with a maximum slip of 5–6 m,occurred in the shallow part of the fault model,approximately 240 km south of the hypocenter.Large slips of 2–3 m were also found near the southern end of the fault model.Slips on the fault plane were dominated by strike-slip components,though slips south of the largest asperity included significant dip-slip components.
文摘On April 26,the China Foundation for Peace and Development(CFPD),in collaboration with the Shenzhen Foundation for International Exchange and Cooperation(SFIEC),the Shenzhen Ye Chenghai Charity Foundation and the China-Myanmar Economic Cooperation and Development Promotion Association(Myanmar),held a handover ceremony at Yangon Airport to donate five tons of medicine to the disasterstricken areas of Myanmar.
文摘Along China's southwestern border,Dehong Dai and Jingpo Autonomous Prefecture in Yunnan Province shares mountains,rivers,ethnic ties,and cultural connections with Myanmar.This land,imbued with the spirit of the pauk-phaw friendship(pauk-phaw means fraternal in Myanmar language),has in recent years been exploring innovative approaches to international communication with Myanmar.Centered on serving the Belt and Road Initiative(BRI)and building a China-Myanmar community with a shared future,Dehong has incorporated the vision of“Mingalaba”(auspiciousness in Myanmar language)into its cross-border communication e"orts,sharing stories of China-Myanmar friendship with people far and wide.
基金phased achievement of the Yunnan Provincial Philosophy and Social Sciences Innovation Team project titled Research on Ethnic Issues and Their Impact in Northern Myanmar(No.2025CX09).
文摘Over 70 years ago,China proposed the Five Principles of Peaceful Coexistence,which were first embraced by countries such as Myanmar and gradually gained traction across Asia.The Five Principles eventually became widely recognized norms in international relations and foundational principles of international law,contributing significantly to the post-World War II international order.Decades on,the Five Principles have not faded into history.Rather,they have demonstrated renewed relevance in today’s complex global landscape.
文摘Mesozoic ophiolites crop out discontinuously in the Indo-Myanmar Ranges in NE India and Myanmar,and represent the remnants of the Neotethyan oceanic lithosphere(Sengupta et al.,1990;Mitchell,1993).These ophiolites in the Indo-Myanmar Ranges are the southern continuation of the Neotethyan ophiolites occurring along the Yarlung Zangbo Suture Zone(YZSZ)in southern Tibet farther northwest(Mitchell,1993;Fareeduddin and Dilek,2015),as indicated by their coeval crystallization ages and geochemical compositions(Yang et al.,2012;Liu et al.,2016).The Kalaymyo ophiolite is located in the central part of the eastern Indo-Myanmar Ranges(Fig.1).composition of these ophiolites from the central Tibetan Plateau(CTP)is dominated by MORBs and minor OIBs and a distinct lack of IATs and BONs,which is inconsistent with most ophiolites worldwide(Robinson and Zhou,2008;Zhang et al.,2008).But the generation and tectonic nature of these ophiolites are still controversial.*The Kalaymyo peridotites consist mainly of harzburgites,which show typical porphyroclastic or coarse-grained equigranular textures.They are composed ofolivine(Fo=89.8–90.5),orthopyroxene(En86-91Wo1-4Fs8-10;Mg#=89.6–91.9),clinopyroxene(En46-49Wo47-50Fs3-5;Mg#=90.9–93.6)and spinel(Mg#=67.1–78.9;Cr#=13.5–31.5),and have relatively homogeneous whole-rock compositions with Mg#s of90.1–90.8 and Si O2(41.5–43.65 wt.%),Al2O3(1.66–2.66wt.%)and Ca O(1.45–2.67 wt.%)contents.TheydisplayLightRareEarthElement(LREE)-depleted chondrite-normalized REE patterns with(La/Yb)CN=0.04–0.21 and(Gd/Yb)CN=0.40–0.84,and show a slight enrichment from Pr to La with(La/Pr)CN in the range of 0.98–2.36.The Kalaymyo peridotites are characterized by Pd-enriched chondrite-normalized PGE patterns with superchondritic(Pd/Ir)CN ratios(1.15–2.36).Their calculated oxygen fugacities range between QFM–0.57 and QFM+0.90.These mineralogical and geochemical features collectively suggest that the Kalaymyo peridotites represent residual upper mantle rocks after low to moderate degrees(5–15%)of partial melting at a mid-ocean-ridge(MOR)environment.The observed enrichment in LREE and Pd was a result of their reactions with enriched MORB-like melts,percolating through these already depleted,residual peridotites.The Kalaymyo and other ophiolites in the Indo-Myanmar Ranges hence represent mid-ocean ridge(MOR)–type Tethyan oceanic lithosphere derived from a downgoing plate and accreted into a westward migrating subduction–accretion system along the eastern margin of India.
