The West Kunlun orogenic belt(WKOB) along the northern margin of the Tibetan Plateau is important for understanding the evolution of the Proto-and Paleo-Tethys oceans. Previous investigations have focused on the igneo...The West Kunlun orogenic belt(WKOB) along the northern margin of the Tibetan Plateau is important for understanding the evolution of the Proto-and Paleo-Tethys oceans. Previous investigations have focused on the igneous rocks and ophiolites distributed mostly along the Xinjiang-Tibet road and the China-Pakistan road, and have constructed a preliminary tectonic model for this orogenic belt. However, few studies have focused on the so-called Precambrian basement in this area. As a result, the tectonic affinity of the individual terranes of the WKOB and their detailed evolution process are uncertain. Here we report new field observations, zircon and monazite U-Pb ages of the "Precambrian basement" of the South Kunlun terrane(SKT) and the Tianshuihai terrane(TSHT), two major terranes in the WKOB. Based on new zircon U-Pb age data, the amphibolite-facies metamorphosed volcanosedimentary sequence within SKT was deposited during the late Neoproterozoic to Cambrian(600-500 Ma), and the flysch-affinity Tianshuihai Group, as the basement of the TSHT, was deposited during the late Neoproterozoic rather than Mesoproterozoic. The rock association of the volcano-sedimentary sequence within SKT suggests a large early Paleozoic accretionary wedge formed by the long-term lowangle southward subduction of the Proto-Tethys Ocean between Tarim and TSHT. The amphibolitefacies metamorphism in SKT occurred at ca. 440 Ma. This ca. 440 Ma metamorphism is genetically related to the closure of the Proto-Tethys Ocean between Tarim and the Tianshuihai terrane, which led to the assembly of Tarim to Eastern Gondwana and the final formation of the Gondwana. Since the late Paleozoic to early Mesozoic, the northward subduction of the Paleo-Tethys Ocean along the HongshihuQiaoertianshan belt produced the voluminous early Mesozoic arc-signature granites along the southern part of NKT-TSHT. The Paleo-Tethys ocean between TSHT and Karakorum closed at ca. 200 Ma, as demonstrated by the monazite age of the paragneiss in the Kangxiwa Group. Our study does not favor the existence of a Precambrian basement in SKT.展开更多
Objective To investigate the efficacy of hematopoietic stem cell(HSC) transplantation via the hepatic artery vs.the portal vein for end-stage liver disease(ESLD).Methods Patients with hepatic decompensation were prosp...Objective To investigate the efficacy of hematopoietic stem cell(HSC) transplantation via the hepatic artery vs.the portal vein for end-stage liver disease(ESLD).Methods Patients with hepatic decompensation were prospectively recruited from September 2010 to September 2012 to receive HSC transplantation via the hepatic artery or the portal vein.Liver function was examined at 3,6,and 12 months after transplantation.Liver biopsy results were analyzed using the Knodell score.Results Eighty patients(58 males and 22 females) were enrolled in the study.The Child-Pugh score was grade B in 69 cases,and grade C in the remaining 11 cases.HSC transplantation was performed via the portal vein in 36 patients and via the hepatic artery in 44 patients.ALT levels decreased while serum albumin levels increased significantly in both groups at 6 and 12 months after HSC transplantation(P<0.05 compared with pre-transplantation levels).Total bilirubin levels decreased significantly in both groups at 3,6,and 12 months after HSC transplantation(P<0.05 compared with pre-transplantation levels).Additionally,prothrombin time decreased in both groups at 12 months after HSC transplantation(P<0.05 compared with pre-transplantation level).There were no significant differences in ALT,total bilirubin and prothrombin time between the two groups either before or after transplantation.Moreover,Knodell score decreased significantly at 6 and 12 months.Histological examination showed that liver cell edema,degeneration,necrosis,and inflammation were significantly relieved at 3,6,and 12 months after transplantation.The incidence of portal vein thrombosis,upper gastrointestinal bleeding,and hepatic encephalopathy were 1.25%,3.75%,and 2.5% respectively.The one-year survival rate was 100%.Conclusions Autologous HSC transplantation improves liver function and histology in ESLD patients.The administration route of HSC has no significant impact on the efficacy of transplantation.展开更多
基金funded by the National 305 Project of China (2018A03004-1, 2015BAB05B01-02)the Fundamental Research Fund for Central Universities(B16020127)
文摘The West Kunlun orogenic belt(WKOB) along the northern margin of the Tibetan Plateau is important for understanding the evolution of the Proto-and Paleo-Tethys oceans. Previous investigations have focused on the igneous rocks and ophiolites distributed mostly along the Xinjiang-Tibet road and the China-Pakistan road, and have constructed a preliminary tectonic model for this orogenic belt. However, few studies have focused on the so-called Precambrian basement in this area. As a result, the tectonic affinity of the individual terranes of the WKOB and their detailed evolution process are uncertain. Here we report new field observations, zircon and monazite U-Pb ages of the "Precambrian basement" of the South Kunlun terrane(SKT) and the Tianshuihai terrane(TSHT), two major terranes in the WKOB. Based on new zircon U-Pb age data, the amphibolite-facies metamorphosed volcanosedimentary sequence within SKT was deposited during the late Neoproterozoic to Cambrian(600-500 Ma), and the flysch-affinity Tianshuihai Group, as the basement of the TSHT, was deposited during the late Neoproterozoic rather than Mesoproterozoic. The rock association of the volcano-sedimentary sequence within SKT suggests a large early Paleozoic accretionary wedge formed by the long-term lowangle southward subduction of the Proto-Tethys Ocean between Tarim and TSHT. The amphibolitefacies metamorphism in SKT occurred at ca. 440 Ma. This ca. 440 Ma metamorphism is genetically related to the closure of the Proto-Tethys Ocean between Tarim and the Tianshuihai terrane, which led to the assembly of Tarim to Eastern Gondwana and the final formation of the Gondwana. Since the late Paleozoic to early Mesozoic, the northward subduction of the Paleo-Tethys Ocean along the HongshihuQiaoertianshan belt produced the voluminous early Mesozoic arc-signature granites along the southern part of NKT-TSHT. The Paleo-Tethys ocean between TSHT and Karakorum closed at ca. 200 Ma, as demonstrated by the monazite age of the paragneiss in the Kangxiwa Group. Our study does not favor the existence of a Precambrian basement in SKT.
基金Supported by the Science&Technology Department of Sichuan Province(2010FZ0098,2011HH0022)Chengdu Bureau of Science and Technology(10GGYB883SF)the Scientific Research Foundation of the Health Department of Sichuan Province(100487,100489)
文摘Objective To investigate the efficacy of hematopoietic stem cell(HSC) transplantation via the hepatic artery vs.the portal vein for end-stage liver disease(ESLD).Methods Patients with hepatic decompensation were prospectively recruited from September 2010 to September 2012 to receive HSC transplantation via the hepatic artery or the portal vein.Liver function was examined at 3,6,and 12 months after transplantation.Liver biopsy results were analyzed using the Knodell score.Results Eighty patients(58 males and 22 females) were enrolled in the study.The Child-Pugh score was grade B in 69 cases,and grade C in the remaining 11 cases.HSC transplantation was performed via the portal vein in 36 patients and via the hepatic artery in 44 patients.ALT levels decreased while serum albumin levels increased significantly in both groups at 6 and 12 months after HSC transplantation(P<0.05 compared with pre-transplantation levels).Total bilirubin levels decreased significantly in both groups at 3,6,and 12 months after HSC transplantation(P<0.05 compared with pre-transplantation levels).Additionally,prothrombin time decreased in both groups at 12 months after HSC transplantation(P<0.05 compared with pre-transplantation level).There were no significant differences in ALT,total bilirubin and prothrombin time between the two groups either before or after transplantation.Moreover,Knodell score decreased significantly at 6 and 12 months.Histological examination showed that liver cell edema,degeneration,necrosis,and inflammation were significantly relieved at 3,6,and 12 months after transplantation.The incidence of portal vein thrombosis,upper gastrointestinal bleeding,and hepatic encephalopathy were 1.25%,3.75%,and 2.5% respectively.The one-year survival rate was 100%.Conclusions Autologous HSC transplantation improves liver function and histology in ESLD patients.The administration route of HSC has no significant impact on the efficacy of transplantation.
