On 21 May 2021(UTC),an MW 7.4 earthquake jolted the east Bayan Har block in the Tibetan Plateau.The earthquake received widespread attention as it is the largest event in the Tibetan Plateau and its surroundings since...On 21 May 2021(UTC),an MW 7.4 earthquake jolted the east Bayan Har block in the Tibetan Plateau.The earthquake received widespread attention as it is the largest event in the Tibetan Plateau and its surroundings since the 2008 Wenchuan earthquake,and especially in proximity to the seismic gaps on the east Kunlun fault.Here we use satellite interferometric synthetic aperture radar data and subpixel offset observations along the range directions to characterize the coseismic deformation of the earthquake.Range offset displacements depict clear surface ruptures with a total length of~170 km involving two possible activated fault segments in the earthquake.Coseismic modeling results indicate that the earthquake was dominated by left-lateral strike-slip motions of up to 7 m within the top 12 km of the crust.The well-resolved slip variations are characterized by five major slip patches along strike and 64%of shallow slip deficit,suggesting a young seismogenic structure.Spatial-temporal changes of the postseismic deformation are mapped from early 6-day and 24-day InSAR observations,and are well explained by time-dependent afterslip models.Analysis of Global Navigation Satellite System(GNSS)velocity profiles and strain rates suggests that the eastward extrusion of plateau is diffusely distributed across the east Bayan Har block,but exhibits significant lateral heterogeneities,as evidenced by magnetotelluric observations.The block-wide distributed deformation of the east Bayan Har block along with the significant co-and post-seismic stress loadings from the Madoi earthquake imply high seismic risks along regional faults,especially the Tuosuo Lake and Maqên-Maqu segments of the Kunlun fault that are known as seismic gaps.展开更多
全基因组关联分析(genome-wide association study,GWAS)的理论及应用是近十几年来国内外数量性状研究的热点,但是以往GWAS方法注重于个别主要QTL/基因的检测与发掘。为了相对全面地解析全基因组QTL及其等位基因构成,本研究提出了限制...全基因组关联分析(genome-wide association study,GWAS)的理论及应用是近十几年来国内外数量性状研究的热点,但是以往GWAS方法注重于个别主要QTL/基因的检测与发掘。为了相对全面地解析全基因组QTL及其等位基因构成,本研究提出了限制性两阶段多位点GWAS方法(RTM-GWAS,https://github.com/njau-sri/rtm-gwas)。RTM-GWAS首先将多个相邻且紧密连锁的SNP分组,成为具有多个单倍型(复等位变异)的连锁不平衡区段(SNPLDB)标记,然后采用两阶段分析策略,基于多位点复等位变异遗传模型,在节省计算空间的条件下保障全基因组QTL及其复等位变异检出的精确度。和以往GWAS方法相比,RTM-GWAS以性状遗传率为上限,能够较充分地检测出QTL及其相应的复等位变异并能有效地控制假阳性的膨胀。由其结果建立的QTL-allele矩阵代表了群体中所研究性状的全部遗传组成。依据这种QTL-allele矩阵的信息,可以设计最优基因型的遗传组成,预测群体中最优化的杂交组合,并用以进行群体遗传和特有与新生等位变异的研究。本研究首先对RTM-GWAS方法的特点和计算程序功能进行说明,然后通过大豆试验数据说明RTM-GWAS计算程序的使用方法。展开更多
基金supported by the Natural Science Foundation of Jiangsu Province(Grant No.SBK2020043202)by Key Laboratory of Geospace Environment and Geodesy,Ministry of Education,Wuhan University(No.19-01-08).
文摘On 21 May 2021(UTC),an MW 7.4 earthquake jolted the east Bayan Har block in the Tibetan Plateau.The earthquake received widespread attention as it is the largest event in the Tibetan Plateau and its surroundings since the 2008 Wenchuan earthquake,and especially in proximity to the seismic gaps on the east Kunlun fault.Here we use satellite interferometric synthetic aperture radar data and subpixel offset observations along the range directions to characterize the coseismic deformation of the earthquake.Range offset displacements depict clear surface ruptures with a total length of~170 km involving two possible activated fault segments in the earthquake.Coseismic modeling results indicate that the earthquake was dominated by left-lateral strike-slip motions of up to 7 m within the top 12 km of the crust.The well-resolved slip variations are characterized by five major slip patches along strike and 64%of shallow slip deficit,suggesting a young seismogenic structure.Spatial-temporal changes of the postseismic deformation are mapped from early 6-day and 24-day InSAR observations,and are well explained by time-dependent afterslip models.Analysis of Global Navigation Satellite System(GNSS)velocity profiles and strain rates suggests that the eastward extrusion of plateau is diffusely distributed across the east Bayan Har block,but exhibits significant lateral heterogeneities,as evidenced by magnetotelluric observations.The block-wide distributed deformation of the east Bayan Har block along with the significant co-and post-seismic stress loadings from the Madoi earthquake imply high seismic risks along regional faults,especially the Tuosuo Lake and Maqên-Maqu segments of the Kunlun fault that are known as seismic gaps.
文摘全基因组关联分析(genome-wide association study,GWAS)的理论及应用是近十几年来国内外数量性状研究的热点,但是以往GWAS方法注重于个别主要QTL/基因的检测与发掘。为了相对全面地解析全基因组QTL及其等位基因构成,本研究提出了限制性两阶段多位点GWAS方法(RTM-GWAS,https://github.com/njau-sri/rtm-gwas)。RTM-GWAS首先将多个相邻且紧密连锁的SNP分组,成为具有多个单倍型(复等位变异)的连锁不平衡区段(SNPLDB)标记,然后采用两阶段分析策略,基于多位点复等位变异遗传模型,在节省计算空间的条件下保障全基因组QTL及其复等位变异检出的精确度。和以往GWAS方法相比,RTM-GWAS以性状遗传率为上限,能够较充分地检测出QTL及其相应的复等位变异并能有效地控制假阳性的膨胀。由其结果建立的QTL-allele矩阵代表了群体中所研究性状的全部遗传组成。依据这种QTL-allele矩阵的信息,可以设计最优基因型的遗传组成,预测群体中最优化的杂交组合,并用以进行群体遗传和特有与新生等位变异的研究。本研究首先对RTM-GWAS方法的特点和计算程序功能进行说明,然后通过大豆试验数据说明RTM-GWAS计算程序的使用方法。
