| 000 | 01893nmc a2200253 4500 | ||
|---|---|---|---|
| 005 | 20260520005438.0 | ||
| 008 | 260224s xxu esp | ||
| 041 | _aEspañol | ||
| 082 | _a068.82 553.28 C62 2018 0015644 | ||
| 245 | 0 | 0 |
_aInterpretación sísmica de anomalías de gas _bClasificación de facies sísmicas y análisis avo para su caracterización |
| 270 | _a30/06/2022 ; 21/02/2019 | ||
| 300 | _a9 p. ; 477-486 | ||
| 520 | _aFrom cross sectional seismic interpretation, some Lobe-shaped anomalies were interpreted. Those anomalies are related with gas-bearing, tertiary reservoirs, which is of great interest since they lie in shallow depths and those reservoirs have free gas only.The anomalies were characterized from the pre-and post-stack seismic record; different seismic attributes maps were made (spectral decomposition, sweetness, Hilbert Transform, etc.), in order to define their geometry. Then, a seismic facies classification PCA was made to obtain rock-type characterization supported by well-log data. Since the AVO analysis is useful for fluid characterization, a qualitative AVO analysis was performed in this case of study.From this analysis, a number of workovers were identified. Three wells were intervened in order to perforate the reservoirs associated with seismic anomalies in Salamanca Formation (Maastrichtiano-Daniano). The flow-in test proved gas in all of them, with low CO2 content and static pressure. | ||
| 773 | _g | ||
| 942 | _cCONGTP | ||
| 100 | 1 |
_aArustizia, Ana _9663 |
|
| 100 | 1 |
_aKrenek, Daniel _9664 |
|
| 100 | 1 |
_aPérez, Carlos _9665 |
|
| 111 | 2 |
_aSimposio de Geofísica (2018 nov. 5 - 9 : Mendoza) _9561 |
|
| 650 | 0 |
_aGas somero _9666 |
|
| 650 | 0 |
_aFacies sísmicas _9667 |
|
| 999 |
_c128407 _d128407 |
||
| 856 | _uhttps://biblioteca.iapg.org.ar/ArchivosAdjuntos/Conexplor2018/SGeof/1125.pdf | ||