| 000 | 03673nmc a2200313 4500 | ||
|---|---|---|---|
| 005 | 20260520010404.0 | ||
| 008 | 260224s2018 xxu esp | ||
| 041 | _aEspañol | ||
| 082 | _a068.82 553.28 C62 2018 0015658 | ||
| 245 | 0 | 0 |
_aPotencial hidrocarburífero en los Valles de Fiambalá y Chaschuil, provincia de Catamarca _bBase exploratoria actual |
| 260 |
_a _b _c2018 |
||
| 270 | _a02/09/2025 ; 05/04/2019 | ||
| 300 | _a33 p. ; 209-242 | ||
| 520 | _aFiambalá and Chaschuil valleys are located in the SW of the Catamarca province, Argentina, in a geological context in which several regional systems converge. In terms of hydrocarbons exploration, this is a new frontier basin, with very little background. There are no seismic records or exploratory wells in these areas. The generating potential is in a siliceous interval with oil stains and shows, belonging to the Upper Permian record of the Paganzo Basin. The basement of the basin would be formed by igneous and metamorphic rocks from the Precambrian to Lower Paleozoic.Over the basement fluvio-lacustrine deposits of Upper Carboniferous age are developed, followed by continental red layers of the Lower and Upper Permian. These sequences mainly consist of ephemeral fluvial-alluvial, aeolian and saline to hypersaline lacustrine deposits. These last sedimentary facies are of interest as potential source rocks by incorporating elements of marine affinity in the top sequences. The Permian deposits are overlaid by sediments of unknown age (Cretaceous?). A thick package of Tertiary sediments, Neogene in age, formed by fluvial-alluvial deposits related to the development of the Andean Orogeny lies discordant in turn. The regional structure is mainly associated to the development of a thick-skin fold and thrust belt with eastern vergence, with buttress in the crystalline basement massifs of the Sierras Pampeanas Noroccidentales.Hydrocarbon exploratory information comes from surface studies consisting of geological and geochemical surveys and detailed sampling; stratigraphic and structural geological mapping, stratigraphic detailed profiles in the column of interest, and mapping on a structural line, representative of the regional deformation of the basin. Samples taken from rocks and oil from outcrops, allowed to make estimations for oleogenetic potential and obtain curves for chemostratigraphic studies in the interval of interest. Surveys of Microbial and Gas prospection allowed to know the existence of thermogenic gases and butanotrophic microbes in soils, which would allow inferring the existence of a potential source rock in the subsoil. With the existing surface information, an initial 1D modeling of generation, migration and entrapment conditions was performed. The oil exploratory potential of the area regarding the potential organic content and its distribution, and the generating capacity of the Permian rocks, were evaluated in relation to the possible structural configuration of the deep subsurface | ||
| 773 | _g | ||
| 942 | _cCONGTP | ||
| 100 | 1 |
_aPérez, Miguel Ángel _952622 |
|
| 100 | 1 |
_aCaccaglio, Osvaldo _958742 |
|
| 100 | 1 |
_aCarini, Federico David _958743 |
|
| 100 | 1 |
_aWainstein, Leonel _958744 |
|
| 100 | 1 |
_aRosales, Leonel Jesús _958745 |
|
| 100 | 1 |
_aGarbán, Grony _958746 |
|
| 100 | 1 |
_aKokot, Pablo _958747 |
|
| 111 | 2 |
_aCongreso de Exploración y Desarrollo de Hidrocarburos (10mo. : 2018 nov. 5 - 9 : Mendoza) _9573 |
|
| 650 | 0 |
_aCatamarca _924236 |
|
| 650 | 0 |
_aCuenca de Paganzo _958748 |
|
| 999 |
_c192808 _d192808 |
||
| 856 | _uhttps://biblioteca.iapg.org.ar/ArchivosAdjuntos/Conexplor2018/1133.pdf | ||