| 000 | 02658nmc a2200241 4500 | ||
|---|---|---|---|
| 005 | 20260520010331.0 | ||
| 008 | 260224s xxu | ||
| 082 | _aCD I116 64 0015469 | ||
| 245 | 0 | 0 | _aSedimentología y perfiles de rayos gamma de la formación pozo D-129 (aptiano) en la Sierra de San Bernardo, Chubut |
| 270 | _a10/11/2016 ; 10/11/2016 | ||
| 300 | _a25 p. | ||
| 520 | _aSedimentology and gamma-ray logs of the Pozo D-129 formation (Aptian) in the Sierra de San Bernardo, Chubut The study provides an outcrop analogue of productive hydrocarbon succesions of the uppermost part of the Pozo D-129 formation (Aptian) in the Golfo San Jorge basin. Although widely distributed in the subsurface of the basin, the Pozo D-129 formation is just exposed in three areas of the San Bernardo Fold Belt; this contribution presents the result of a sedimentological analysis carried out in the Sierra Silva (43 m thick) and Codo del Senguerr (140 m thick) anticlines. Facies analysis allowed the identification of thirteen lithofacies, which were grouped in three main lithofacies associations: (A) deep lacustrine, (B) sub-litoral lacustrine, and (C) shallow lacustrine. The later association consists of four sub-associations: C1 (carbonatic lake), C2 (distributary channels), C3 (distributary mouth bar) and C4 (interdistributary bay). Incomplete shallowing-upward cycles are common in both study areas, evidencing sedimentary progradation. Total and spectral gamma-ray (GR) measurements were obtained using a hand-held device. In Sierra Silva the shape of the U and total GR logs is similar, reflecting that minerals containing U are responsible of most of the emissions of this rocks; diagenetic enrichment of U occurred in a 4,5 m thick section, with measurements up to 500 ppm of U (378 g/tn de U3O8). At Codo del Senguerr, Th and K measurements in fine-grained rocks display better correlation with the total GR log than U, evidencing a different source of radioactive minerals. Integration of sedimentology and gammaray measurements bring data and lithological correspondences that could be useful for regional correlations and subsurface facies models. | ||
| 773 | _g | ||
| 942 | _cCONGTP | ||
| 100 | 1 |
_aParedes, José M. _955748 |
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| 100 | 1 |
_aAllard, José O. _955749 |
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| 100 | 1 |
_aFoix, Nicolás _9765 |
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| 100 | 1 |
_aÁlvarez, Bruno _955750 |
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| 100 | 1 |
_aOlazábal, Sabrina X. _955751 |
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| 111 | 2 |
_aCongreso de Exploración y Desarrollo de Hidrocarburos (9no. : 2014 nov. 3-7 : Mendoza) _954287 |
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| 999 |
_c189824 _d189824 |
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| 856 | _uhttps://biblioteca.iapg.org.ar/ArchivosAdjuntos/CONEXPLOR2014/455-Sedimentologiayperfiles.pdf | ||