Petroleum generation and accumulation in the Golfo San Jorge Basin, Argentina: a basin modeling study

The Golfo San Jorge Basin, located in Patagonia, is very important for the oil and gas production of Argentina. In spite of the long history of exploration and production, few geochemical studies were performed until now. For this study, a set of possible source rocks was analyzed by organic geochem...

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Published in:Marine and petroleum geology Vol. 18; no. 9; pp. 995 - 1028
Main Authors: Rodriguez, Jorge F.R, Littke, Ralf
Format: Journal Article
Language:English
Published: Oxford Elsevier Ltd 01.11.2001
Elsevier Science
Subjects:
Applied sciences
Argentina
Crude oil, natural gas and petroleum products
Earth sciences
Earth, ocean, space
Energy
Exact sciences and technology
Fuels
Geology and geochemistry. Geological and geochemical prospecting. Petroliferous series
Golfo San Jorge Basin
Hydrocarbons
Petroleum generation
Prospecting and exploration
Prospecting and production of crude oil, natural gas, oil shales and tar sands
Sedimentary rocks
Stratigraphy
Subsidence modeling
Thermal modeling
Patagonia
Argentina
Golfo San Jorge Basin
Argentina
Subsidence modeling
Thermal modeling
Petroleum generation
South America
Neogene
upper Tertiary
algae
sedimentation rates
faults
maturation
burial
kerogen
subsidence
two-dimensional models
Cenozoic
petroleum
organic carbon
Thallophyta
tectonic controls
accumulation
hydrocarbons
reflectance
Tertiary
Plantae
source rocks
one-dimensional models
inversion tectonics
migration
vitrinite
Miocene
Phanerozoic
petroleum exploration
thermal models
ISSN:0264-8172, 1873-4073
Online Access:Get full text
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Abstract The Golfo San Jorge Basin, located in Patagonia, is very important for the oil and gas production of Argentina. In spite of the long history of exploration and production, few geochemical studies were performed until now. For this study, a set of possible source rocks was analyzed by organic geochemical and petrographical methods. The samples of the Pozo D-129 Fm. range from mature to overmature, and contain from less than 0.5 to 2.45% TOC. There is some evidence indicating an algal origin of the more hydrogen-rich kerogen present in part of the basin. Almost all the samples of Pozo Anticlinal Aguada Bandera and Pozo Cerro Guadal Fm. are overmature. TOC values range from less than 0.5 to 2.5%. The maturation of source rocks and generation, expulsion and migration of hydrocarbons was evaluated by means of 1D and 2D basin models. The 1D models constructed for the western part of the basin and 2D models applied for the eastern part both indicate maximum burial in Miocene times. The thickness of the Tertiary at times of maximum burial ranged from 1000 to 1500 m and the generally small Tertiary thickness now present in the fold belt region is assumed to be the result of erosion. The main tectonic inversion took place in the Late Neogene. The models strongly suggest that a magmatic event between 20 and 30 Ma, combined with the maximum burial at Miocene times produced a very important pulse in hydrocarbon generation within the major part of the basin. Dated intrusive and extrusive magmatic rocks extended all over the basin account for this period of elevated heat flow. Migration pathways are extensively discussed for the 2D model. Probably, major faults acted as important conduits for petroleum.
AbstractList The Golfo San Jorge Basin, located in Patagonia, is very important for the oil and gas production of Argentina. In spite of the long history of exploration and production, few geochemical studies were performed until now. For this study, a set of possible source rocks was analyzed by organic geochemical and petrographical methods. The samples of the Pozo D-129 Fm. range from mature to overmature, and contain from less than 0.5 to 2.45% TOC. There is some evidence indicating an algal origin of the more hydrogen-rich kerogen present in part of the basin. Almost all the samples of Pozo Anticlinal Aguada Bandera and Pozo Cerro Guadal Fm. are overmature. TOC values range from less than 0.5 to 2.5%. The maturation of source rocks and generation, expulsion and migration of hydrocarbons was evaluated by means of 1D and 2D basin models. The 1D models constructed for the western part of the basin and 2D models applied for the eastern part both indicate maximum burial in Miocene times. The thickness of the Tertiary at times of maximum burial ranged from 1000 to 1500 m and the generally small Tertiary thickness now present in the fold belt region is assumed to be the result of erosion. The main tectonic inversion took place in the Late Neogene. The models strongly suggest that a magmatic event between 20 and 30 Ma, combined with the maximum burial at Miocene times produced a very important pulse in hydrocarbon generation within the major part of the basin. Dated intrusive and extrusive magmatic rocks extended all over the basin account for this period of elevated heat flow. Migration pathways are extensively discussed for the 2D model. Probably, major faults acted as important conduits for petroleum.
The Golfo San Jorge Basin, located in Patagonia, is very important for the oil and gas production of Argentina. In spite of the long history of exploration and production, few geochemical studies were performed until now. For this study, a set of possible source rocks was analyzed by organic geochemical and petrographical methods. The samples of the Pozo D-129 Fm. range from mature to overmature, and contain from less than 0.5 to 2.45% TOC. There is some evidence indicating an algal origin of the more hydrogen-rich kerogen present in part of the basin. Almost all the samples of Pozo Anticlinal Aguada Bandera and Pozo Cerro Guadal Fm. are overmature. TOC values range from less than 0.5 to 2.5%. The maturation of source rocks and generation, expulsion and migration of hydrocarbons was evaluated by means of 1D and 2D basin models. The 1D models constructed for the western part of the basin and 2D models applied for the eastern part both indicate maximum burial in Miocene times. The thickness of the Tertiary at times of maximum burial ranged from 1000 to 1500 m and the generally small Tertiary thickness now present in the fold belt region is assumed to be the result of erosion. The main tectonic inversion took place in the Late Neogene. The models strongly suggest that a magmatic event between 20 and 30 Ma, combined with the maximum burial at Miocene times produced a very important pulse in hydrocarbon generation within the major part of the basin. Dated intrusive and extrusive magmatic rocks extended all over the basin account for this period of elevated heat flow. Migration pathways are extensively discussed for the 2D model. Probably, major faults acted as important conduits for petroleum.
Author Littke, Ralf
Rodriguez, Jorge F.R
Author_xml – sequence: 1
  givenname: Jorge F.R
  surname: Rodriguez
  fullname: Rodriguez, Jorge F.R
  email: zrodrigu@pecom.com.ar
  organization: Institute of Petroleum and Organic Geochemistry (ICG-4), Research Center Juelich, 52425 Juelich, Germany
– sequence: 2
  givenname: Ralf
  surname: Littke
  fullname: Littke, Ralf
  email: littke@lek.rwth-aachen.de
  organization: Institute of Geology and Geochemistry of Petroleum and Coal, Aachen University of Technology (RWTH), Lochnerstr. 4-20, D-52056 Aachen, Germany
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Issue 9
Keywords Golfo San Jorge Basin
Argentina
Subsidence modeling
Thermal modeling
Petroleum generation
South America
Neogene
upper Tertiary
algae
sedimentation rates
faults
maturation
burial
kerogen
subsidence
two-dimensional models
Cenozoic
petroleum
organic carbon
Thallophyta
tectonic controls
accumulation
hydrocarbons
reflectance
Tertiary
Plantae
source rocks
one-dimensional models
inversion tectonics
migration
vitrinite
Miocene
Phanerozoic
petroleum exploration
thermal models
Language English
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Elsevier Science
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Snippet The Golfo San Jorge Basin, located in Patagonia, is very important for the oil and gas production of Argentina. In spite of the long history of exploration and...
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StartPage 995
SubjectTerms Applied sciences
Argentina
Crude oil, natural gas and petroleum products
Earth sciences
Earth, ocean, space
Energy
Exact sciences and technology
Fuels
Geology and geochemistry. Geological and geochemical prospecting. Petroliferous series
Golfo San Jorge Basin
Hydrocarbons
Petroleum generation
Prospecting and exploration
Prospecting and production of crude oil, natural gas, oil shales and tar sands
Sedimentary rocks
Stratigraphy
Subsidence modeling
Thermal modeling
Title Petroleum generation and accumulation in the Golfo San Jorge Basin, Argentina: a basin modeling study
URI https://dx.doi.org/10.1016/S0264-8172(01)00038-1
https://www.proquest.com/docview/20714152
Volume 18
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