Por qué y cómo hacer un modelo conceptual de fracturas naturales, el ejemplo de la Fm. Cupén Mahuida (Record no. 194944)
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| 000 -LEADER | |
|---|---|
| fixed length control field | 02904nmc a2200325 4500 |
| 008 - CÓDIGOS DE INFORMACIÓN DE LONGITUD FIJA - INFORMACIÓN GENERAL | |
| Campo de control de longitud fija | 260224s2018 xxu esp |
| 041 ## - IDIOMA | |
| Idioma | Español |
| 082 ## - CLASIFICACIÓN DEWEY | |
| Número de clasificación | 068.82 553.28 C62 2018 0015658 |
| 245 00 - TITULO | |
| Título | Por qué y cómo hacer un modelo conceptual de fracturas naturales, el ejemplo de la Fm. Cupén Mahuida |
| 260 ## - PUBLICACION, DISTRIBUCION, ETC | |
| Lugar de publicación, distribución, etc. | |
| Nombre de publicador, distribuidor, etc. | |
| Fecha de publicación, distribución, etc. | 2018 |
| 270 ## - FECHA DE CARGA | |
| Fecha de carga | 02/09/2025 ; 28/06/2022 |
| 300 ## - DESCRIPCION FISICA | |
| Otra extensión | 16 p. ; 971-986 |
| 520 ## - RESUMEN, ETC | |
| Resumen | Natural fracture reservoirs are one of the most challenging ones in terms of understanding thus modeling. The available computational tools allow representing withgood degree of certainty the presence, intensity and orientation of natural fractures in subsurface. Still, from the geological point of view, the effort should be concentrated in establishing the origin of the fracturesystem, the so called Conceptual Model. Whichever the selected method for fracture modeling (e.g. Geometric, Geostatistic, Geophysic or Geomechanic) it should be tied to a geological logic and to the available data like geological and structural models, fracture data from image logs, cores, side well cores and even outcrop analogs when available. To develop a Conceptual Model, it is fundamental to stablish the natural fractures generation mechanisms, being the tectonism and the lithostatic weight the most common factors, and fracturing by intrusion or by cooling-down of volcanic rocks and related rocks. So, it is necessary to understand the deformation history in the study area.In this study an Upper Triassic to Lower Jurassic volcaniclastic sequence, characterized by ignimbrites, ash-fall tuffs, subaqueous flows and volcanogenic sedimentary deposits, was generated during a Syn-rift phase, later reactivated at least three times. Based on well data analysis and interpretation, six different cementation stageswere recognized.Two of them, so called E2 and E3, were interpreted as cretaceous due to microthermometry after fluid inclusions analysis. Other characteristics such as fracture sizes, orientations, aperture and a potential link within volcaniclastic facies were determined.All this information resulted in the main guidelines for the subsurface 3D Natural Fractures Model |
| 773 ## - CORRECCIÓN | |
| Partes relacionadas | |
| 942 ## - DESC. DE MATERIAL | |
| Tipo de item KOHA | Congresos (trabajos presentados) |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | López, Ramiro |
| 9 (RLIN) | 55776 |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Ruiz, Remigio |
| 9 (RLIN) | 58763 |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Spacapan, Juan |
| 9 (RLIN) | 60731 |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Hryb, Damián |
| 9 (RLIN) | 706 |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Manceda, René |
| 9 (RLIN) | 2667 |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Santiago, Emiliano |
| 9 (RLIN) | 884 |
| 100 1# - RESPONSABLE PERSONAL | |
| Apellido, Nombre | Montagna, Aldo |
| 9 (RLIN) | 882 |
| 111 2# - AUTORIDAD DE CONGRESO | |
| Nombre de congreso | Congreso de Exploración y Desarrollo de Hidrocarburos (10mo. : 2018 nov. 5 - 9 : Mendoza) |
| 9 (RLIN) | 573 |
| 650 #0 - MATERIA | |
| Término tópico | Fracturas naturales |
| 9 (RLIN) | 58545 |
| 650 #0 - MATERIA | |
| Término tópico | Volcaniclásticos |
| 9 (RLIN) | 60732 |
| 650 #0 - MATERIA | |
| Término tópico | Tectonismo |
| 9 (RLIN) | 60733 |
| 856 ## - LINK | |
| Link | <a href="https://biblioteca.iapg.org.ar/ArchivosAdjuntos/Conexplor2018/1489.pdf">https://biblioteca.iapg.org.ar/ArchivosAdjuntos/Conexplor2018/1489.pdf</a> |
| Biblioteca propietaria | Biblioteca actual | Ubicación | Fecha de adquisición | Inventario | Total de préstamos | Signatura topográfica | Inventario | Fecha de carga | Tipo de item KOHA |
|---|---|---|---|---|---|---|---|---|---|
| Colección Digital IAPG | Colección Digital IAPG | 068.82 553.28 C62 2018 0015658 | 06/03/2026 | 200067335 | 068.82 553.28 C62 2018 0015658 | 200067335 | 06/03/2026 | Archivo electrónico |
