The east\|west striking Northern Altyn Tagh Fault, about 240km long between Bashkaogong (90°E, 39°25′N) and Lapeiquan (92°15′E, 39°25′N), was previously mapped as a north\|dipping thrust, juxtap...The east\|west striking Northern Altyn Tagh Fault, about 240km long between Bashkaogong (90°E, 39°25′N) and Lapeiquan (92°15′E, 39°25′N), was previously mapped as a north\|dipping thrust, juxtaposing late Archean\|Mesoproterozoic gneisses in the hanging wall over Paleozoic volcanics, plutons, turbidite, and melange complexes in the footwall. In order to estimate the total magnitude of slip along the Cenozoic Altyn Tagh fault, we conducted geologic mapping along four traverses across the Jinyan Shan where the fault lies. Our field observations suggest that the fault is south\|dipping, with dip angles varying from <25° in the east to about 40° in the west. The eastern fault zone exhibits mylonitic fabrics, whereas the western fault zone is characterized by cataclastic deformation. Kinematic indicators in the ductily deformed mylonitic shear zone consistently show a top\|to\|the\|south sense of shear, suggesting that the Northern Altyn Tagh fault is a south\|dipping normal fault, not a north\|dipping thrust.. The ductile shear zone is typically 30～40m thick, consisting of highly sheared metasediments (pelite and marble), granites, and granitic veins.The latter are systematically cut by small\|scale, south\|dipping ductile normal faults with displacements between 10s of cm to several meters, forming spectacular asymmetric boudinages in the sheared meta\|pelite matrix.The minimum displacement along the detachment is about 20km, as measured by the north\|south width of the exposed footwall gneisses. We renamed the Northern Altyn Tagh Fault in the Jinyan Shan region as the Lapeiquan detachment fault to avoid confusion with other east\|west trending Cenozoic faults to the west along the northern edge of the Altyn Tagh range (e.g., the Cenozoic Jianglisai fault near Qiemo), collectively known as the Northern Altyn Tagh fault system (see Cowgill et al., Geology,in press). The lower age bound of the Lapeiquan fault is Ordovician, as the fault cuts Ordovician volcanics and plutons in its hanging wall. As the Ordovician volcanic rocks are folded together with Carboniferous marbles and Jurassic sedimentary strata, it is likely that normal faulting along the Lapeiquan detachment postdates the Jurassic. The Lapeiquan detachment fault is covered by Quaternary sediments of the Tarim basin in the west, and is apparently truncated by the Cenozoic left\|slip Altyn Tagh fault to the east as indicated by regional geologic maps. If true, this relationship implies that the Lapeiquan fault predates the Cenozoic Altyn Tagh fault. The apparent truncational relationship between the Lapeiquan fault and the Altyn Tagh fault posses an important question: where is the counterpart of the Lapeiquan fault south of the Altyn Tagh fault? Preliminary mapping in the Yema Nan Shan south of the Altyn Tagh fault reveals a fragment of a low\|angle mylonitic shear zone, which is interpreted as a detachment fault because it puts lower\|grade meta\|pelite over higher\|grade mylonitic quartzite. The correlation of detachment faults in the Yema Nan Shan and the Lapeiquan area would imply an amount of about 280～300km left slip along the Altyn Tagh fault. Alternatively, movement along the Lapeiquan detachment fault could have been synchronous with the development of the Cenozoic Altyn Tagh fault. This interpretation requires no counterpart of the Lapeiquan fault south of the Altyn Tagh fault. Instead, it implies that a major topographic collapse event occurred in the Cenozoic along the northern edge of the Tibetan plateau during movement along the Altyn Tagh fault. On\|going thermochronologic analysis will provide constraints on the age of the detachment fault and a test for the two distinctive hypotheses.展开更多
外涵静子叶片是大涵道比涡扇发动机气路的核心部件之一,外涵静子脱出是一种较为严重的故障模式,此故障可能会导致飞机或其他发动机部件损伤,进而造成灾难性事故。对外涵静子叶片脱出故障的预警是一项重要的工作。但因其早期特征不明显,...外涵静子叶片是大涵道比涡扇发动机气路的核心部件之一,外涵静子脱出是一种较为严重的故障模式,此故障可能会导致飞机或其他发动机部件损伤,进而造成灾难性事故。对外涵静子叶片脱出故障的预警是一项重要的工作。但因其早期特征不明显,现有的方法较难对此类故障进行有效的预警。因此,针对该问题,基于监控数据提出一种深度特征提取的支持向量数据域描述(Support vector data description,SVDD)的故障预警方法,以实现对外涵静子叶片脱出故障的早期预警。首先,采用基于发动机气路性能辨识的建模方法,建立发动机特定性能参数的观测模型对气路参数进行深度特征提取,以真实状态量与模型观测量的差值作为航空发动机是否发生故障的特征;然后利用SVDD算法建立决策边界,实现故障数据的自动划分,决策边界生成的阈值可在故障发生之前的一定时间之内给出告警;最后,经过多次计算,结果表明,在故障早期直至故障发生的区间内,表征其健康状态的性能参数都与观测量有较大的偏移,表明了所选特征的有效性。使用数据增强方法生成故障仿真数据与真实数据进行对比验证,预警时间比故障真实发生时间预警模型平均提前3.14 h。展开更多
文摘The east\|west striking Northern Altyn Tagh Fault, about 240km long between Bashkaogong (90°E, 39°25′N) and Lapeiquan (92°15′E, 39°25′N), was previously mapped as a north\|dipping thrust, juxtaposing late Archean\|Mesoproterozoic gneisses in the hanging wall over Paleozoic volcanics, plutons, turbidite, and melange complexes in the footwall. In order to estimate the total magnitude of slip along the Cenozoic Altyn Tagh fault, we conducted geologic mapping along four traverses across the Jinyan Shan where the fault lies. Our field observations suggest that the fault is south\|dipping, with dip angles varying from <25° in the east to about 40° in the west. The eastern fault zone exhibits mylonitic fabrics, whereas the western fault zone is characterized by cataclastic deformation. Kinematic indicators in the ductily deformed mylonitic shear zone consistently show a top\|to\|the\|south sense of shear, suggesting that the Northern Altyn Tagh fault is a south\|dipping normal fault, not a north\|dipping thrust.. The ductile shear zone is typically 30～40m thick, consisting of highly sheared metasediments (pelite and marble), granites, and granitic veins.The latter are systematically cut by small\|scale, south\|dipping ductile normal faults with displacements between 10s of cm to several meters, forming spectacular asymmetric boudinages in the sheared meta\|pelite matrix.The minimum displacement along the detachment is about 20km, as measured by the north\|south width of the exposed footwall gneisses. We renamed the Northern Altyn Tagh Fault in the Jinyan Shan region as the Lapeiquan detachment fault to avoid confusion with other east\|west trending Cenozoic faults to the west along the northern edge of the Altyn Tagh range (e.g., the Cenozoic Jianglisai fault near Qiemo), collectively known as the Northern Altyn Tagh fault system (see Cowgill et al., Geology,in press). The lower age bound of the Lapeiquan fault is Ordovician, as the fault cuts Ordovician volcanics and plutons in its hanging wall. As the Ordovician volcanic rocks are folded together with Carboniferous marbles and Jurassic sedimentary strata, it is likely that normal faulting along the Lapeiquan detachment postdates the Jurassic. The Lapeiquan detachment fault is covered by Quaternary sediments of the Tarim basin in the west, and is apparently truncated by the Cenozoic left\|slip Altyn Tagh fault to the east as indicated by regional geologic maps. If true, this relationship implies that the Lapeiquan fault predates the Cenozoic Altyn Tagh fault. The apparent truncational relationship between the Lapeiquan fault and the Altyn Tagh fault posses an important question: where is the counterpart of the Lapeiquan fault south of the Altyn Tagh fault? Preliminary mapping in the Yema Nan Shan south of the Altyn Tagh fault reveals a fragment of a low\|angle mylonitic shear zone, which is interpreted as a detachment fault because it puts lower\|grade meta\|pelite over higher\|grade mylonitic quartzite. The correlation of detachment faults in the Yema Nan Shan and the Lapeiquan area would imply an amount of about 280～300km left slip along the Altyn Tagh fault. Alternatively, movement along the Lapeiquan detachment fault could have been synchronous with the development of the Cenozoic Altyn Tagh fault. This interpretation requires no counterpart of the Lapeiquan fault south of the Altyn Tagh fault. Instead, it implies that a major topographic collapse event occurred in the Cenozoic along the northern edge of the Tibetan plateau during movement along the Altyn Tagh fault. On\|going thermochronologic analysis will provide constraints on the age of the detachment fault and a test for the two distinctive hypotheses.
文摘外涵静子叶片是大涵道比涡扇发动机气路的核心部件之一,外涵静子脱出是一种较为严重的故障模式,此故障可能会导致飞机或其他发动机部件损伤,进而造成灾难性事故。对外涵静子叶片脱出故障的预警是一项重要的工作。但因其早期特征不明显,现有的方法较难对此类故障进行有效的预警。因此,针对该问题,基于监控数据提出一种深度特征提取的支持向量数据域描述(Support vector data description,SVDD)的故障预警方法,以实现对外涵静子叶片脱出故障的早期预警。首先,采用基于发动机气路性能辨识的建模方法,建立发动机特定性能参数的观测模型对气路参数进行深度特征提取,以真实状态量与模型观测量的差值作为航空发动机是否发生故障的特征;然后利用SVDD算法建立决策边界,实现故障数据的自动划分,决策边界生成的阈值可在故障发生之前的一定时间之内给出告警;最后,经过多次计算,结果表明,在故障早期直至故障发生的区间内,表征其健康状态的性能参数都与观测量有较大的偏移,表明了所选特征的有效性。使用数据增强方法生成故障仿真数据与真实数据进行对比验证,预警时间比故障真实发生时间预警模型平均提前3.14 h。
