Control spectra for Quito

被引:6
作者
Aguiar, Roberto [1 ,2 ]
Rivas-Medina, Alicia [1 ,3 ]
Caiza, Pablo [1 ]
Quizanga, Diego [4 ]
机构
[1] Univ Fuerzas Amadas ESPE, Dept Ciencias Tierra & Construcc, Quito, Ecuador
[2] Univ Laica Eloy Alfaro Manabi, Manabi, Ecuador
[3] Univ Concepcion, Dept Cs Geodes & Geomat, Campus Los Angeles, Los Angeles, Chile
[4] Escuela Politec Nacl, Dept Ingn Civil, Quito, Ecuador
关键词
EARTHQUAKE; SLIP; SEISMICITY; FREQUENCY; ECUADOR;
D O I
10.5194/nhess-17-397-2017
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The Metropolitan District of Quito is located on or very close to segments of reverse blind faults, Puengasi, Ilumbisi-La Bota, Carcelen-El Inca, Bellavista-Catequilla and Tangahuilla, making it one of the most seismically dangerous cities in the world. The city is divided into five areas: south, south-central, central, north-central and north. For each of the urban areas, elastic response spectra are presented in this paper, which are determined by utilizing some of the new models of the Pacific Earthquake Engineering Research Center (PEER) NGA-West2 program. These spectra are calculated considering the maximum magnitude that could be generated by the rupture of each fault segment, and taking into account the soil type that exists at different points of the city according to the Norma Ecuatoriana de la Construccion (2015). Subsequently, the recurrence period of earthquakes of high magnitude in each fault segment is determined from the physical parameters of the fault segments (size of the fault plane and slip rate) and the pattern of recurrence of type Gutenberg-Richter earthquakes with double truncation magnitude (M (min) and M (max)) is used.
引用
收藏
页码:397 / 407
页数:11
相关论文
共 34 条
[1]  
Abrahamson N.A., 2013, Update of the AS08 Ground-Motion Prediction Equations Based on the NGA-West 2 Data Set
[2]  
Aguiar R., 2003, MICROZONIFICACION SI, P212
[3]   Active tectonics in Quito, Ecuador,assessed by geomorphological studies,GPS data,and crustal seismicity [J].
Alvarado, A. ;
Audin, L. ;
Nocquet, J. M. ;
Lagreulet, S. ;
Segovia, M. ;
Font, Y. ;
Lamarque, G. ;
Yepes, H. ;
Mothes, P. ;
Rolandone, F. ;
Jarrin, P. ;
Quidelleur, X. .
TECTONICS, 2014, 33 (02) :67-83
[4]  
ANDERSON JG, 1983, B SEISMOL SOC AM, V73, P471
[5]  
ANDERSON JG, 1979, B SEISMOL SOC AM, V69, P135
[6]   NOTE ON RECURRENCE RELATIONS FOR EARTHQUAKES [J].
BATH, M .
TECTONOPHYSICS, 1978, 51 (1-2) :T23-T30
[7]   Locations and magnitudes of historical earthquakes in the Sierra of Ecuador (1587-1996) [J].
Beauval, Celine ;
Yepes, Hugo ;
Bakun, William H. ;
Egred, Jose ;
Alvarado, Alexandra ;
Singaucho, Juan-Carlos .
GEOPHYSICAL JOURNAL INTERNATIONAL, 2010, 181 (03) :1613-1633
[8]   SEISMIC MOMENT SEISMICITY AND RATE OF SLIP ALONG MAJOR FAULT ZONES [J].
BRUNE, JN .
JOURNAL OF GEOPHYSICAL RESEARCH, 1968, 73 (02) :777-+
[9]  
Campbell K.W., 2013, 201306 PEER U CAL
[10]  
Castillo D., 2014, THESIS, P160