A total of 80 weathering pits （gnammas）, located on granite surfaces of Qing Mountain （青山）, Hexigten （克什克腾） Global Geopark, Inner Mongolia, were identified and measured in terms of dimensional and orientat...A total of 80 weathering pits （gnammas）, located on granite surfaces of Qing Mountain （青山）, Hexigten （克什克腾） Global Geopark, Inner Mongolia, were identified and measured in terms of dimensional and orientational features. This article attempts to extract characteristics of the weathering pits by descriptive statistics and orientation rose diagrams, investigate the multi-phase evolution by the modified gnamma morphological analysis （GMA） method, and shed new light on the possible genesis and the influencing factors. Following the modified GMA method, weathering pits in Qing Mountain have been divided into six groups and compared with analogous sites to deduce their approximate age, which might be no older than 30 ka B.P., and explore the possibility that the multi-phase evolution of weathering pits may arise from responses to climate change. In consequence, we suggest that the combination of weathering, especially salt weathering, and wind erosion, both of which are closely related to climatic variation, take the main responsibility for the formation and development of weathering pits in Qing Mountain.展开更多
Nonlinear time series prediction is studied by using an improved least squares support vector machine （LSSVM） regression based on chaotic mutation evolutionary programming （CMEP） approach for parameter optimizatio...Nonlinear time series prediction is studied by using an improved least squares support vector machine （LSSVM） regression based on chaotic mutation evolutionary programming （CMEP） approach for parameter optimization. We analyze how the prediction error varies with different parameters （σ, γ） in LS-SVM. In order to select appropriate parameters for the prediction model, we employ CMEP algorithm. Finally, Nasdaq stock data are predicted by using this LS-SVM regression based on CMEP, and satisfactory results are obtained.展开更多
objective To study the clonal evolution of domestic children with lymphoid malignancies inorder to choose the optimal method for the detection of the minimal residual disease. methods To use the PCRwhich employs 22pri...objective To study the clonal evolution of domestic children with lymphoid malignancies inorder to choose the optimal method for the detection of the minimal residual disease. methods To use the PCRwhich employs 22primers and SSCP, investigating the matched samples obtained at diagnosis and at relapse of 13children with lymphoid malignancies. Results The clonal evolution occurred in 54%, 23%, 38%, 46%, 54%, 62%and 54% of 13 cases by PCR employing IgH, TCRγ, TCRVδ2, - Dδ3, TCRPVJ1, TCRPVJ2, TCRPD1,J2, TCRβD2J2primers respectively. NO change occurred only in one of those cases. Clonal evolution at relapse occurred at 50% ofsamples which had only one band PCR product at diagnosis and 78% of those had multiple bands PCR product atdiagnosis. No differences had been detected between diagnosis and relapse by SSCP analyzing those samples inwhich no band change occurred between that at diagnosis and at relapse in PAGE. Conclusion It should beoptimal that the one band rearranged gene at diagnosis acts as main monitoring marker, simultaneously referringto the main band in multiple bands rearranged gene in order to avoid false negative.展开更多
The regime of plate tectonics on early Earth is one of the fundamental problems in Earth sciences.Precambrian era takes the majority(ca.88%)of Earth’s history and thus plays a key role in understanding the onset of p...The regime of plate tectonics on early Earth is one of the fundamental problems in Earth sciences.Precambrian era takes the majority(ca.88%)of Earth’s history and thus plays a key role in understanding the onset of plate tectonics and the mechanism,distribution and process of Precambrian subduction zones.This paper presents a review on the progresses of subduction and subduction zones in different stages of Precambrian era,and sorts out some key issues and fields that merits further attention.We suggest that there was progressive onset and evolution of subduction and plate tectonics from Archean to Proterozoic eras.We emphasize the importance of comprehensive studies on subduction mechanism,metamorphic type,plate tectonics regime,the compositional evolution of continental crust,and petrogenesis of diverse granitoids formed in the Archean.It is proposed that innovative analytical techniques,big data,experimental petrology and numerical geodynamic modeling will facilitate future studies of Precambrian subduction zones.展开更多
The evolution of a mesoscale convective system （MCS） that caused strong precipitation in the northern area of Dabie Mountain during 21 22 June 2008 is analyzed, along with the evolution of the associated meso-β-sca...The evolution of a mesoscale convective system （MCS） that caused strong precipitation in the northern area of Dabie Mountain during 21 22 June 2008 is analyzed, along with the evolution of the associated meso-β-scale convective vortex （MCV）. The mesoscale reanalysis data generated by the Local Analysis and Prediction System （LAPS） at a 3-km horizontal resolution and a 1-h time resolution during the South China Heavy Rainfall Experiment （SCHeREX） were utilized. The results show that two processes played key roles in the enhancement of convective instability. First, the mesoscale low-level jet strengthened and shifted eastward, leading to the convergence of warm-wet airflow and increasing convective instability at middle and low levels. Second, the warm-wet airflow interacted with the cold airflow from the north, causing increased vertical vorticity in the vicinity of steeply sloping moist isentropic surfaces. The combined action of these two processes caused the MCS to shift progressively eastward. Condensation associated with the MCS released latent heat and formed a layer of large diabatic heating in the middle troposphere, increasing the potential vorticity below this layer. This increase in potential vorticity created favorable conditions for the development of a low-level vortex circulation. The vertical motion associated with this low-level vortex further promoted the development of convection, creating a positive feedback between the deep convection and the low-level vortex circulation. This feedback mechanism not only promoted the maturation of the MCS, but also played the primary role in the evolution of the MCV. The MCV formed and developed due to the enhancement of the positive feedback that accompanied the coming together of the center of the vortex and the center of the convection. The positive feedback peaked and the MCV matured when these two centers converged. The positive feedback weakened and the MCV began to decay as the two centers separated and diverged.展开更多
基金supported by China Geological Survey(No.11212011120118)the Fundamental Research Projects of China University of Geosciences,Beijing,China(No.2011YYL016)
文摘A total of 80 weathering pits （gnammas）, located on granite surfaces of Qing Mountain （青山）, Hexigten （克什克腾） Global Geopark, Inner Mongolia, were identified and measured in terms of dimensional and orientational features. This article attempts to extract characteristics of the weathering pits by descriptive statistics and orientation rose diagrams, investigate the multi-phase evolution by the modified gnamma morphological analysis （GMA） method, and shed new light on the possible genesis and the influencing factors. Following the modified GMA method, weathering pits in Qing Mountain have been divided into six groups and compared with analogous sites to deduce their approximate age, which might be no older than 30 ka B.P., and explore the possibility that the multi-phase evolution of weathering pits may arise from responses to climate change. In consequence, we suggest that the combination of weathering, especially salt weathering, and wind erosion, both of which are closely related to climatic variation, take the main responsibility for the formation and development of weathering pits in Qing Mountain.
基金The project supported by National Natural Science Foundation of China under Grant No. 90203008 and the Doctoral Foundation of the Ministry of Education of China
文摘Nonlinear time series prediction is studied by using an improved least squares support vector machine （LSSVM） regression based on chaotic mutation evolutionary programming （CMEP） approach for parameter optimization. We analyze how the prediction error varies with different parameters （σ, γ） in LS-SVM. In order to select appropriate parameters for the prediction model, we employ CMEP algorithm. Finally, Nasdaq stock data are predicted by using this LS-SVM regression based on CMEP, and satisfactory results are obtained.
文摘objective To study the clonal evolution of domestic children with lymphoid malignancies inorder to choose the optimal method for the detection of the minimal residual disease. methods To use the PCRwhich employs 22primers and SSCP, investigating the matched samples obtained at diagnosis and at relapse of 13children with lymphoid malignancies. Results The clonal evolution occurred in 54%, 23%, 38%, 46%, 54%, 62%and 54% of 13 cases by PCR employing IgH, TCRγ, TCRVδ2, - Dδ3, TCRPVJ1, TCRPVJ2, TCRPD1,J2, TCRβD2J2primers respectively. NO change occurred only in one of those cases. Clonal evolution at relapse occurred at 50% ofsamples which had only one band PCR product at diagnosis and 78% of those had multiple bands PCR product atdiagnosis. No differences had been detected between diagnosis and relapse by SSCP analyzing those samples inwhich no band change occurred between that at diagnosis and at relapse in PAGE. Conclusion It should beoptimal that the one band rearranged gene at diagnosis acts as main monitoring marker, simultaneously referringto the main band in multiple bands rearranged gene in order to avoid false negative.
基金the National Natural Science Foundation of China(Grant Nos.42025202,41890833&41430210).
文摘The regime of plate tectonics on early Earth is one of the fundamental problems in Earth sciences.Precambrian era takes the majority(ca.88%)of Earth’s history and thus plays a key role in understanding the onset of plate tectonics and the mechanism,distribution and process of Precambrian subduction zones.This paper presents a review on the progresses of subduction and subduction zones in different stages of Precambrian era,and sorts out some key issues and fields that merits further attention.We suggest that there was progressive onset and evolution of subduction and plate tectonics from Archean to Proterozoic eras.We emphasize the importance of comprehensive studies on subduction mechanism,metamorphic type,plate tectonics regime,the compositional evolution of continental crust,and petrogenesis of diverse granitoids formed in the Archean.It is proposed that innovative analytical techniques,big data,experimental petrology and numerical geodynamic modeling will facilitate future studies of Precambrian subduction zones.
基金Supported by the National Key Basic Research and Development (973) Program of China (2004CB418300)
文摘The evolution of a mesoscale convective system （MCS） that caused strong precipitation in the northern area of Dabie Mountain during 21 22 June 2008 is analyzed, along with the evolution of the associated meso-β-scale convective vortex （MCV）. The mesoscale reanalysis data generated by the Local Analysis and Prediction System （LAPS） at a 3-km horizontal resolution and a 1-h time resolution during the South China Heavy Rainfall Experiment （SCHeREX） were utilized. The results show that two processes played key roles in the enhancement of convective instability. First, the mesoscale low-level jet strengthened and shifted eastward, leading to the convergence of warm-wet airflow and increasing convective instability at middle and low levels. Second, the warm-wet airflow interacted with the cold airflow from the north, causing increased vertical vorticity in the vicinity of steeply sloping moist isentropic surfaces. The combined action of these two processes caused the MCS to shift progressively eastward. Condensation associated with the MCS released latent heat and formed a layer of large diabatic heating in the middle troposphere, increasing the potential vorticity below this layer. This increase in potential vorticity created favorable conditions for the development of a low-level vortex circulation. The vertical motion associated with this low-level vortex further promoted the development of convection, creating a positive feedback between the deep convection and the low-level vortex circulation. This feedback mechanism not only promoted the maturation of the MCS, but also played the primary role in the evolution of the MCV. The MCV formed and developed due to the enhancement of the positive feedback that accompanied the coming together of the center of the vortex and the center of the convection. The positive feedback peaked and the MCV matured when these two centers converged. The positive feedback weakened and the MCV began to decay as the two centers separated and diverged.
