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INTRODUCCION La mayoría de los mapas usados en la geología del petróleo son mapas del subsuelo, siendo los mapas geológicos de superficie, los tectonicos y los geofísicos, parte de la información utilizada en la evaluación geológica de un yacimiento. Al elaborar cualquier tipo de mapa se se deben tener en cuenta las siguientes precauciones:
Los datos deben ser representados según una escala y un intervalo apropiado.
Los mapas no deben estar sobrecargados de datos. Son un
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ISOHIPSAS ESTRUCTURALES Una isohipsa estructural es una línea definida por puntos de igual altura en una superficie estructural; trazada en una superficie plana es una recta y es sinónima de la línea de dirección de capa, y en superficies curviplanas se ven como curvas que en todas partes son tangentes a la dirección de capa. Se usan para indicar la forma de la
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ISOHIPSAS ESTRUCTURALES
La superficie representada por ellas puede sobresalir o puede estar interrumpida por fallas. En determinadas circunstancias también puede resultar útil tomar como plano de referencia uno inclinado en lugar de
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TRAZADO DE ISOHIPSAS ESTRUCTURALES
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MAPAS ESTRUCTURALES ELABORACION DE MAPAS ESTRUCTURALES Una curva estructural es una línea imaginaria que conecta puntos de igual posición estructural en el subsuelo, por consiguiente un mapa estructural muestra la configuración de un horizonte o estrato. Los datos para su construcción deben ser referidos a una línea base, que por lo general es el nivel del mar. Información Requerida: 1.
Ubicación exacta de cada punto de observación.
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ELABORACION DE MAPAS ESTRUCTURALES CONSTRUCCION: 1.
Interpolación.
2.
Trazado.
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ELABORACION DE MAPAS ESTRUCTURALES Trazado: el intervalo entre las curvas depende de la diferencia de elevación dentro del área de estudio, lográndose proporcionar un suficiente numero de isolíneas que muestren una interpretación razonablemente clara de la estructura del subsuelo.
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ELABORACION DE MAPAS ESTRUCTURALES 4.
5.
Excepcionalmente las isolíneas pueden cruzarse en el caso de pliegues volcados y fallas inversas. Por lo regular no se muestran las curvas en el bloque hundido o en el flanco inferior del pliegue volcado. Una curva finaliza solamente en un falla, línea de costa o discordancia. Las pequeñas depresiones se pueden indicar con achurados.
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ELABORACION DE MAPAS ESTRUCTURALES 9.
La geología regional proporciona indicadores del tipo de estructuras que pueden encontrarse en el área.
10.
En los sinclinales cuyo eje no es horizontal las curvas de nivel están subiendo por un flanco, cruzan el eje y regresan bajando por el blanco opuesto, formando una V con el extremo abierto
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ERRORES EN MAPAS ESTRUCTURALES
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METODOS DE TRAZADO
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METODOS DE TRAZADO
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ELABORACION DE MAPAS ISOPACOS
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ELABORACION DE MAPAS ISOPACOS
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ELABORACION DE MAPAS ISOPACOS
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