|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | THE CADD AND SIMULATION SYSTEM OFTHE NEW-TYPE GEAR显示文摘THECADDANDSIMULATIONSYSTEMOFTHENEW-TYPEGEARHongHanyu;GuanRongchangTHECADDANDSIMULATIONSYSTEMOFTHENEW-TYPEGEAR￥HongHanyu;GuanR... | Hong Hanyu Guan Rongchang | 1994 | Computer Aided Drafting,Design and Manufacturing1994，4，2： | 1 |
| 2 | Geological characteristics and genesis of subbottom pinnoite deposit of Da Qaidam salt lake in Qaidam Basin显示文摘Da Qaidam salt lake is known for its both liquid and solid boron resource.Data from previous investigation of the Da Qaidam salt lake provided a comparable framework for this study that focused on investigating the section beneath the bottom of the perennial salt lake,including the timing, | Gao Chunliang Yu Junqing Min Xiuyun Cheng Aiying Zhang Lisa He Xianhu Xin Shouzhen Hong Rongchang | 2014 | Acta Geologica Sinica(English Edition)2014，88，S1： | 1 |
| 3 | The Results and Comparison of 'Logical-Tree' Seismic Zoning in the Panxi Area显示文摘On the basis of the technological route of seismic hazard analysis,the methods for determining seismicity parameters,such as b value,annual occurrence rate,and the seismic spatial distribution function,are discussed.Then,the seismic intensity zoning in Panxi area in Southwest China is carried out by applying the 'logical-tree,'which is made up of multi-parameter schemes.It is clearly shown from the results that seismic intensity zoning is influenced by many uncertain factors and it is necessary to seek a certain balance between seismic safety and investment interest and a good way,with the present limited knowledge level,to obtain seismic intensity zoning is through the 'logical-tree' method. | Zhang Yaoguo,Lei Jiancheng,Tang Rongchang,and Qian Hong Seismological Bureau of Sichuan Province,Chengdu 610041,China | 1997 | Earthquake Research in China1997，11，3： | 0 |
| 4 | The Feature of Segmentation Activity on the Northern Segment of the Anninghe Fault Zone Since Late Pleistocene显示文摘Based on fault geometric features,composite pattern,faulting land-forms and seismic data,this paper discussed the activity behavior along the northern segment of the Anninghe fault(from Xichang to Shimian)since the Late Pleistocene.The fault can be divided into three active segments by discrepancies of their activity:the segment from Xichang to Mianning,the segment from Mianning to Zimakua,and the segment from Zimakua to Tianwan.The southern segment has the background of occurrence of great earthquakes,but the middle and the northern segments can generate strong and moderate events respectively.According to the features of quartz from fault gouges by scanning electron microscopy(SEM),this paper discussed the movement features along the fault and indicated the stick-slipping feature on the segment from Xichang to Zimakua,the creeping feature on the segment from Jiziping to Tianwan and the transitional feature on the segment in between. | Tang Rongchang,Qian Hong,Huang Zuzhi,Wen Dehua,Wu Xianguo,Cai Changxing and Tian Hong Seismological Bureau of Sichuan Province,Chengdu 610041,China | 1994 | Earthquake Research in China1994，8，4： | 0 |
| 5 | Main Feature and Potential Seismic Capability of Active Fault Belts in the Chengdu Depression显示文摘Chengdu fault depression is an important Quaternary basin in the piedmont of Longmenshan mountain.Formation and evolution of the fault depression are entirely controlled by the Longmenshan piedmont fault and the Longquanshan fault.Since the late Quaternary,Chengdu fault depression has been subjected to an NW-SE oriented compression.Many NE or NNE trending faults inside the depression or near its margins show thrust slip,resulting in moderate and strong earthquakes along the piedmont Longmenshan fault,the western slop Longquanshan fault,and Pujiang-Xinjin-Chengdu-Deyang fault.It is indicated that three faults as mentioned above have the potential capability for the occurrence of moderate earthquakes. | Tang Rongchang,Huang Zuzhi,Qian Hong,Gong Yu,Wen Dehua,Ma Senghao,and Zhou RongjunSeismological Bureau of Sichuan Province,Chengdu 610041,China | 1997 | Earthquake Research in China1997，11，1： | 0 |
您所在的机构暂未开通此部分的功能，请联系管理员