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41. |
Ingeniería sísmica
by Sarria Molina, Alberto.
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Santafé de Bogotá Universidad de los Andes 1990
. 610 p. :
Date:1990
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42. |
Ensayo a escala natural de un edificio prefabricado ante cargas horizontales y su interpretación
by García Reyes, Luis Enrique
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43. |
Estado actual y necesidades futuras de la Red Sismológica Nacional de Colombia (Rsnc)
by Sarria Molina, Alberto.
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44. |
Aspectos bá sicos en la microzonificación sísmica del á rea urbana de la ciudad de Popayá n
by Sarria Molina, Alberto
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45. |
Consideraciones sobre la amenaza sísmica incluyendo la amplificación local :
by Sarria Molina, Alberto.
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46. |
Desastres naturales terremotos :
by Sarria Molina, Alberto.
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47. |
Consideraciones básicas para la implementación de la Red Sismológica y de Vigilancia de los Volcanes de Colombia (Rsnc)
by Sarria Molina, Alberto.
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48. |
Riesgo volcánico, evaluación y mitigación en América Latina :
by Giesecke M., Alberto A
Publication:
, Serie de Publicaciones del Proyecto SISRA
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49. |
Enseñanzas derivadas de los estudios de las misiones pos-terremoto enviadas por Unesco o por Ceresis-Unesco
by Sarria Molina, Alberto.
Publication:
Lima Centro Regional de Sismología para América del Sur 1986
. 33 p. :
Date:1986
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50. |
Terremotos :
by Sarria Molina, Alberto.
Publication:
Santafé de Bogotá Climent 1985
. 24 p. :
Date:1985
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51. |
Medidas de protección en caso de sismos
by Sarria Molina, Alberto.
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52. |
Aspectos bá sicos sobre la microzonificación sísmica de á reas urbanas
by Sarria Molina, Alberto.
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53. |
Estudio de amenaza sísmica para el puente El Pindo Tumaco - Colombia
by Sarria Molina, Alberto.
Publication:
Santafé de Bogotá LERI. Ingenieros Asociados LTDA. 1994
. 37 p. :
Date:1994
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54. |
Exitos y fracasos del diseño sismo resistente
by Sarria Molina, Alberto.
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55. |
Amenaza sísmica regional
by Sarria Molina, Alberto.
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56. |
Respuesta sísmica del subsuelo y microzonificación del área urbana de Popayán
by Sarria Molina, Alberto
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57. |
Aproximación a los desastres má s comunes
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58. |
Basement faults and uplift in the Colombian Llanos
Publication:
, Reccurrent movements of Precambrian-aged basement fault systems has influenced the thickness and distribution of phanerozonic strata in the Colombian Llanos backarc basin. North of 6° N, the overall river trend of the Arauca, Casanare and the eastern part of the Meta rivers is virtually E-W. The area between 6°N and 2°N contains ENE-WSW lineaments. Sounth of2°N and south of the Inirida and Guayabero rivers, the treends are increasingly disorganized with a predominance of N-S trends, especially west of 71°W. From plate tectonic considerations, movement north of 2°N along principal inferred basement faults should be right-lateral and left-lateral to the sounth. Basement uplift has ocuured along the Serrania de la Macarena. This feature is marked by earthquakes and serves as a drainage divide. The Serrania is a series of beds from precambrian through Oligocene, dipping to the ENE with a strike similar to that of the ridge crest, NNW-SSE. Along the southern edge of the Serrania lies the ENE-WSW trend of the Guaviare-Guayabero rivers. If a similar trend of the Meta-Metica rivers is extended to the WSW, then the extension would lie along the northern limit of the Serrania. Thus, the Serrania de la Macarena can be interpreted as athrust block, partially cutting the sub-Andean basin. Repetitiveness of basement swells appears to be part of the tectonic style of the sub-Andean backarc basin (AU).
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