000			02259nmc a2200313 4500
005			20260520010356.0
008			260224s2018 xxu esp
041			_aEspañol
082			_a068.82 553.28 C62 2018 0015655
245	0	0	_aVariaciones paleogeográficas de las unidades ricas en materia orgánica de la formación Vaca Muerta en el engolfamiento neuquino
260			_a _b _c2018
270			_a01/07/2022 ; 06/03/2019
300			_a16 p. ; 213-229
520			_aIn this study we analyzed the paleo geographical variabilities of the organic rich intervals of different stratigraphic units in the Neuquén Embayment. We developed five paleogeographic maps for units U1 to U5, based on regional mapping of clinoform breaks and toesets at key stratigraphic surfaces and mineralogical well log data, calibrated with core and sidewall core samples. Regardlessof climatic changes previously mentioned in the literature of the area, the results showed that in the successive units, it is remarkable how towards the north the composition is mainly carbonatic in a context of divergent stacking pattern and to the south the composition is mixed type in clinoforms.The interpretation of mineralogical distribution, plus thickness maps and clinoform distribution, lead to identifyand separate two main depositional basin centers (BC). The Eastern Basin center (EBC) characterized by rich organic intervals, in a dominantly calcareous rock and a Western Basin Center (WBC) characterized mainly bymix to siliciclastic rock composition.
773			_g
942			_cCONGTP
100	1		_aDomínguez, Ricardo Fabián _958440
100	1		_aBernhardt, Carolina _9857
100	1		_aGonzález Tomassini, Federico _9778
100	1		_aFantín, Manuel _9776
100	1		_aDi Benedetto, Matías _958441
111	2		_aCongreso de Exploración y Desarrollo de Hidrocarburos (10mo. : 2018 nov. 5 - 9 : Mendoza) _9573
111	2		_aSimposio de Recursos No Convencionales (2018 nov. 5 - 9 : Mendoza) _9781
650		0	_aVaca Muerta _9566
650		0	_aPaleogeografía _958461
650		0	_aMineralogía _9840
999			_c192694 _d192694
856			_uhttps://biblioteca.iapg.org.ar/ArchivosAdjuntos/Conexplor2018/SRNC/1685.pdf