L. Cuenca-de-sabinas, posee un área de 37000 km 2 , y esta situada en el noreste de México (Figura I.1)

. I. Fig, 1. Localización del área de estudio y sistema de fallas referidas en este trabajo. Abreviaciones

B. , C. De-burgos, A. Bsa, . Burro-salado, and . Cb, Bloque de Coahuila; LBf, Falla La Babia; LSPI, Isla Lampazos- Sabinas-Picacho; Lp, Cuenca La Popa; MSM, Mega-falla Mojave-Sonora

N. El-núcleo and . Cortó-en-la-formación-la-casita, Anexo 5), consiste de una caliza arenosa gris, gris oscuro, presentando en su parte media, una caliza arenosa biogena, Microscopicamente en su parte superior (C1) consiste de una arenisca ligeramente calcárea; su parte media consiste de un wackstone arenoso y biogeno con restos de equinodermos y bioclastos, pp.3620-3629

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. I. Fig, Columna estratigráfica de la Cuenca de Sabinas, y Eguiluz de Antuñano, 1991.

. Su-sedimentación, Graduaciones en XZ en metrosIOODII ..00110 1000<II> "'''100

V. Anexo, Línea sísmica SS-09, que muestran los espesores decompactados de las rocas generadoras en el tiempo, justo al final de su sedimentación

. Anexo-11, El diagrama de enterramiento del pozo PMX-263 y curvas de generación de HC de las rocas madres, muestran el Tmax así como las edades de la entrada a las ventanas del aceite y gas. Este pozo en especial, se calibro solo con la temperatura de fondo (BHT), ya que no se cuenta por el momento con datos de vitrinita, que permitan hacer una calibración mas precisa, Sin embargo la erosión para el calibrado del pozo alcanzo los 800 m., que esta dentro de lo estimado para la Cuenca de Piedras Negras

. Abreviaciones, +) = 0.5 a 1%; + 1 a 10%; ++ = 10 a 30%

I. Piedad-sánchez, N. Menetrier, C. Camacho-ortegón, L. F. Martínez, L. Izart et al., Thermal history of polyphasic (rift-postrift and foreland stage) Sabinas -Piedras Negras Basin (Northeastern Mexico) Insights from 1D modelling

I. Camacho-ortegón, L. F. Martínez, L. Piedad-sánchez, N. Pironon, J. Suárez-ruiz et al., Modelling of Hydrocarbon generation and migration in the PIRINEO Block

I. Camacho-ortegón, L. F. Martínez, L. Piedad-sánchez, N. Pironon, J. Suárez-ruiz et al., Modelling of Hydrocarbon generation and migration in the PIRINEO Block

I. Martínez, L. Camacho-ortegón, L. F. Piedad-sánchez, N. Pironon, J. Suárez-ruiz et al., Origin and Occurrence of TRS-BSR and CO 2, Pirineo Block

V. Camacho-ortegón, L. F. Piedad-sánchez, N. Martínez, and L. , Integración de técnicas geofísicas y geoquímicas en la exploración de nuevos prospectos petroleros para un Modelado Integral de Cuencas. Reunión anual de cierre de actividades, Servicio Geológico Mexicano, 2008.

V. Camacho-ortegón, L. F. Martínez, L. Piedad-sánchez, and N. , Origen del petróleo en Inclusiones fluidas de afloramientos cretácicos de fluorita y celestita, 11th ALAGO 2008 International Latin-American Congress on Organic Geochemistry, 2008.

V. Camacho-ortegón, L. F. Piedad-sánchez, N. Martínez, and L. , Modelado Numérico de la Generación, Migración y Acumulación de Hidrocarburos de la Cuenca de Sabinas, Bloque PIRINEO NE de México: implicación de la reconstrucción PTX de las Inclusiones fluidas, 11th ALAGO 2008 International Latin-American Congress on Organic Geochemistry, 2008.

I. Camacho-oregon, L. F. Martínez, L. Piedad-sánchez, and N. , Modelling of the CO2 and CH4 formation in Mesozoic sediments of the Mississippi Valley type: Study of geochemical implication in relation with heat flow evolution in the Pirineo block of the Sabinas basin of Northeastern Mexico, 22ème Réunion des Sciences de la Terre, pp.21-24, 2008.

X. Martínez, L. Gallardo, J. C. Camacho-ortegón, and L. F. , Stockage naturel de CH4, CO2 et H2S dans sediments carbonates de type Mississipy Valley: études géochimique et pétrographique de la distribution spatiale des réactions TSR et, pp.21-24, 2008.

X. Gallardo, J. C. Martínez, L. Coumon, G. Camacho-ortegón, and L. F. , A 3D distribution of the CO2 naturally stocked and/or formed into the Minero-Florida block in the Sabinas basin, north of Mexico, 22ème Réunion des Sciences de la Terre, pp.21-24, 2008.

X. Gallardo, J. C. Martínez, L. Coumon, G. Camacho-ortegón, and L. F. , A 3D study of the CO2 naturally stocked: the case of Minero-Florida block in the Sabinas basin, north of Mexico, pp.2-5, 2008.