Zobrazeno 1 - 10
of 75
pro vyhledávání: '"O. Campos-Enríquez"'
Autor:
E. L. Flores-Márquez, R. G. Martínez–Serrano, R. E. Chávez, Y. Crusillo, G. Jiménez, O. Campos-Enríquez
Publikováno v:
Geofísica Internacional, Vol 47, Iss 1, Pp 27-40 (2008)
Se presenta un modelo geohidrológico evolutivo 3D a corto plazo (para los años 2001, 2005 y 2015) del acuífero somero del Valle de Etla, Oaxaca, sureste de México, basado en los parámetros disponibles de geología, geofísica, geoquímica e hidr
Externí odkaz:
https://doaj.org/article/8e6c865db66945b2b8e7853b51f0989e
Autor:
J. Urrutia Fucugauchi, L. M. Alva Valdivia, J. Rosas Elguera, O. Campos-Enríquez, A. Goguitchaichvili, A. M. Soler Arechalde, C. Caballero Miranda, S. Venegas Salgado, S. Sánchez Reyes
Publikováno v:
Geofísica Internacional, Vol 39, Iss 3, Pp 247-265 (2000)
Resultados paleomagnéticos nuevos del Cañón de Río Grande de Santiago (RGS), correspondientes a 13 sitios en unidades volcánicas de las secciones de Huaxtla, Paso de Guadalupe y Lazo, así como de 5 sitios de la Sierra de la Primavera, se utiliz
Externí odkaz:
https://doaj.org/article/e3a20a46c3344762ad668e9ad2cec2b3
Publikováno v:
Journal of Volcanology and Geothermal Research. 375:1-17
Spectral analysis of NAMAG magnetic data enabled us to estimate depths to the Curie isotherm along the Pacific-North America plate boundary. The estimated depths for the Gulf of California, and southern Baja California peninsula, correlate quite well
Autor:
José Rosas-Elguera, J. O. Campos-Enríquez, Luis Quintanar-Robles, Emilia Fregoso-Becerra, Roberto Toscano-Fletes, Miguel Angel Alatorre-Zamora
Publikováno v:
Journal of South American Earth Sciences. 82:215-230
The Ameca tectonic depression (ATD) is located at the NE of the Jalisco Block along the southwestern fringe of the NW-SE trending Tepic-Zacoalco Rift, in the west-central part of the Trans-Mexican Volcanic Belt, western Mexico. To characterize its sh
Publikováno v:
Interpretation. 4:T497-T505
In Neogene geologic settings, seismic resolution plays an important role in the static characterization of large stratigraphically complex reservoirs. Attenuation of high frequencies due to absorption and scattering of waves propagating through the s
Publikováno v:
Journal of Volcanology and Geothermal Research. 311:135-149
Along an east–west profile crossing the Chicxulub impact structure in northern Yucatan, Mexico, Curie depths were obtained from statistical-spectral analysis of a grid of aeromagnetic data (256 km wide and 600 km long). These depths were corrected
Autor:
Ernesto González-Flores, Raúl Valenzuela Wong, David Ernesto Rivera-Recillas, J. O. Campos-Enríquez, Carlos Torres-Verdín, Erik Camacho-Ramírez
Publikováno v:
Journal of South American Earth Sciences. 103:102722
The shallow structures of the Chalco and Xochimilco sub-basins (southeastern Mexico Basin) are established based on a seismic line that stretches trough both depressions. Interpretation of the seismic line was constraint by the stratigraphic column c
Autor:
J. O. Campos Enríquez, Tim K. Takaro, E.A. Ojeda Olivares, S. Sandoval Torres, S.I. Belmonte Jiménez, John P. Tiefenbacher
Publikováno v:
Journal of Environmental Management. 261:110164
A methodology to evaluate groundwater vulnerability was developed and tested in a case study in the Central Valleys of the state of Oaxaca, Mexico, a region known for intensive agricultural activities and poor water management policies. An analysis w
Autor:
J.D. Keppie, Miguel Angel Alatorre-Zamora, V.M. Ramón-Márquez, J. O. Campos-Enríquez, Salvador Isidro Belmonte-Jiménez
Publikováno v:
Journal of South American Earth Sciences. 56:396-408
A gravity study was conducted across the northern Oaxaca terrane and its bounding faults: the Caltepec and Oaxaca Faults to the west and east, respectively. These faults juxtapose the Oaxaca terrane against the Mixteca and Juarez terranes, respective
Autor:
Ernesto González-Flores, David Ernesto Rivera-Recillas, J. O. Campos-Enríquez, Erick Camacho-Ramírez
Publikováno v:
Geofísica Internacional. 55
Multiresolution analysis, based on the discrete wavelet transform, is here incorporated in seismic signal processing. This analysis technique enables decomposing a seismic signal, in different frequency bands, and thus to analyze the information cont