Raman Spectroscopy Based Maturity Profiling of the Vaca Muerta Formation, Neuquén Basin, Argentina

2019 ◽  
Author(s):  
Alberto Ortiz ◽  
Bastian Sauerer ◽  
Jean-Paul Lafournère ◽  
Pablo Saldungaray ◽  
Wael Abdallah
Keyword(s):  
Raman Spectroscopy ◽  
Vaca Muerta ◽  
Neuquen Basin ◽  
Neuquén Basin ◽  
Vaca Muerta Formation

scholarly journals Evidence of precessional and eccentricity orbital cycles in a Tithonian source rock: The mid-outer carbonate ramp of the Vaca Muerta Formation, northern Neuquén Basin, Argentina

AAPG Bulletin ◽  
2011 ◽  
Vol 95 (9) ◽  
pp. 1459-1474 ◽  
Author(s):  
Diego A. Kietzmann ◽  
Javier Martín-Chivelet ◽  
Ricardo M. Palma ◽  
José López-Gómez ◽  
Marina Lescano ◽  
...  
Keyword(s):  
Source Rock ◽  
Carbonate Ramp ◽  
Orbital Cycles ◽  
Vaca Muerta ◽  
Neuquen Basin ◽  
Neuquén Basin ◽  
Vaca Muerta Formation

Reducing Drilling Risks in Highly Over-Pressurized Quintuco-Vaca Muerta Formation, a Case History in Neuquén Basin /Argentina

2018 ◽  
Author(s):  
Marcelo Frydman ◽  
Andres Acevedo ◽  
Jose Miguel Castellanos ◽  
Ocdomar Casanova ◽  
Jose Hasbani ◽  
...  
Keyword(s):  
Case History ◽  
Vaca Muerta ◽  
Neuquen Basin ◽  
Neuquén Basin ◽  
Vaca Muerta Formation

Elastic parameter estimation for the identification of sweet spots, Vaca Muerta Formation, Neuquén Basin, Argentina

2017 ◽  
Vol 36 (11) ◽  
pp. 948a1-948a10 ◽  
Author(s):  
Carlos Convers ◽  
Christian Hanitzsch ◽  
David Curia ◽  
Thomas Davis ◽  
Ali Tura
Keyword(s):  
Parameter Estimation ◽  
Elastic Parameter ◽  
Vaca Muerta ◽  
Neuquen Basin ◽  
Neuquén Basin ◽  
Vaca Muerta Formation ◽  
Sweet Spots

Tithonian stratigraphy and ammonite fauna of the Vaca Muerta Formation in Mallín Quemado (Neuquén Basin, Argentina), with remarks on the Andean chronostratigraphy

2018 ◽  
Vol XV (1) ◽  
pp. 1-26 ◽  
Author(s):  
Alberto C. GARRIDO ◽  
Horacio PARENT ◽  
Luciano BRAMBILLA
Keyword(s):  
Recent Literature ◽  
Time Correlation ◽  
Additional Information ◽  
Vaca Muerta ◽  
Rock Record ◽  
Neuquen Basin ◽  
Neuquén Basin ◽  
Vaca Muerta Formation

In the Cerro Mallín Quemado area (Sierra de la Vaca Muerta) the three members of the Vaca Muerta Formation (Portada Covunco, Los Catutos and Pichi Moncol) can be recognized, including the whole of the Tithonian rock-record. The ammonite fauna does not show significant differences with respect to that of the nearby locality Pampa Tril, but the record of faunal horizons is patchier. Eighteen species of ammonites were recorded through the studied sections, covering the whole of the Andean Tithonian. The current chronostratigraphic zonation of the Andean Tithonian is briefly discussed, updated and correlated with the most recent literature. From the current succession of ammonite bio-horizons previously defined in the basin, only three (picunleufuense alpha, picunleufuense beta and falculatum) were recognized definitely. Four other bio-horizons (perlaevis, erinoides, internispinosum alpha and vetustum) were recognized only tentatively, because the typical assemblages of morphotypes (morpho-species) were not clearly or completely recognized. The current regional time-correlation chart dated by the ammonite bio-horizons of the Neuquén Basin along a 70°W transect is updated with the results of the present study and additional information recently obtained from other localities.

Diagenesis of the Vaca Muerta Formation, Neuquén Basin: Evidence from petrography, microthermometry and geochemistry

2021 ◽  
Vol 124 ◽  
pp. 104769
Author(s):  
María del Rosario Lanz ◽  
Karem Azmy ◽  
Nora N. Cesaretti ◽  
Natalia B. Fortunatti
Keyword(s):  
Vaca Muerta ◽  
Neuquen Basin ◽  
Neuquén Basin ◽  
Vaca Muerta Formation

Intraspecific variability, biostratigraphy and paleobiological significance of the Southern Gondwana ammonoid genus Lytohoplites Spath

2019 ◽  
Vol 93 (04) ◽  
pp. 702-726 ◽  
Author(s):  
Verónica V. Vennari ◽  
Beatriz Aguirre-Urreta
Keyword(s):  
Intraspecific Variability ◽  
Taxonomic Revision ◽  
Vaca Muerta ◽  
Neuquen Basin ◽  
Assemblage Zone ◽  
Quantitative Analyses ◽  
Neuquén Basin ◽  
Lower Berriasian ◽  
Vaca Muerta Formation ◽  
Selection Of

AbstractLytohoplites Spath, 1925 is a late Tithonian–?early Berriasian ammonoid genus with a southern perigondwanean distribution. Two Lytohoplites species, L. burckhardti (Mayer-Eymar in Burckhardt, 1900) (type species) and L. vetustoides (Burckhardt, 1903), were originally described from carbonate successions of the Vaca Muerta Formation, Neuquén Basin, Argentina. Nevertheless, the holotype of L. burckhardti consisted of a single incomplete specimen that is currently missing. This situation compelled the search for new Lytohoplites specimens in Argentina and the selection of a neotype for L. burckardti. New Lytohoplites representatives were obtained through bed-by-bed collections performed at five localities in the Neuquén Basin. In addition to the taxonomic revision of the Lytohoplites species occurring in the basin, a paleobiological approach was preferred to conduct a paleontological analysis of L. burckhardti, including a description of its ontogeny, probable sexual dimorphism, and spectrum of intraspecific variability. Results of the qualitative and quantitative analyses supported the homogeneity of L. burckhardti as a taxonomic unit, thus implying that L. vetustoides should be considered its synonym. Lytohoplites in the Neuquén Basin is restricted to beds assigned to the Andean Substeueroceras koeneni Assemblage Zone (upper Tithonian–lower Berriasian), and not to the Andean Corongoceras alternans Assemblage Zone (upper Tithonian). Furthermore, the paleobiogeographic distribution of Lytohoplites around southern Gondwana and the herein reported occurrence of L. subcylindricus Collignon, 1962, otherwise only known from Madagascar, lend support to the existence of a functional trans-Gondawana seaway at least since the upper Tithonian.

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