Range extension of Lutjanus inermis (Peters, 1896) (Perciformes: Lutjanidae) to the central region of the Gulf of California, Mexico

2015 ◽  
Vol 31 (3) ◽  
pp. 541-543 ◽  
Author(s):  
F. J. Fernández-Rivera Melo ◽  
H. Reyes-Bonilla ◽  
L. Campos-Dávila ◽  
E. F. Balart
2018 ◽  
Vol 214 (2) ◽  
pp. 990-1003
Author(s):  
Raúl R Castro ◽  
Antonio Mendoza-Camberos ◽  
Arturo Pérez-Vertti

2018 ◽  
Vol 160 ◽  
pp. 58-63
Author(s):  
Marisol Arce-Acosta ◽  
Mauricio Ramírez-Rodríguez ◽  
Gustavo De-la-Cruz-Agüero

2017 ◽  
Vol 56 (2) ◽  
Author(s):  
Héctor E. Rodríguez-Lozoya ◽  
Tonatiuh Domínguez R. ◽  
Luis Quintanar Robles ◽  
Armando Aguilar Meléndez ◽  
Héctor E. Rodríguez-Leyva ◽  
...  

Coda waves were analyzed from events recorded by NARS seismic network deployed along both margins of the Gulf of California, Mexico, to estimate coda attenuation Qc. Sato’s (1977) single scattering model was used for a coda window of 20 to 25 s beginning at twice the S-wave travel time. Events recorded from 2003 to 2007 located in the central region of the Gulf of California were analyzed. Source-to-receiver distances are between 40 and 500 km. Assuming a power law of the form QC (f) = QO f a, QC values were averaged and a value of QO = 83±3 and a frequency-dependence α value of 1.06±0.03 in the frequency range from 1 to 7 Hz was obtained. QO value and the high frequency dependency agree with the values of other regions characterized by a high tectonic activity. Based on source-station distribution two subregions (north and south) were defined. QC values were calculated and correlated with tectonics and morphology of each area. The observed higher attenuation in the south region can be attributed to the fact that south region is more fractured since the greater earthquakes occur in central to south Gulf of California and the oceanic crust is reported to be thinner in the southern region.


2010 ◽  
Vol 3 ◽  
Author(s):  
Jazmín Hernández-Kantún ◽  
Rafael Riosmena-Rodríguez ◽  
Juan M. López-vivas ◽  
Isaí Pacheco-Ruíz

2001 ◽  
Vol 44 (5) ◽  
Author(s):  
R. Riosmena-Rodríguez ◽  
L. Paul-Chávez ◽  
G. Hinojosa-Arango

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