A new model of the petroleum system in the Northern Apennines, Italy

Davide Oppo, Rossella Capozzi, Vincenzo Picotti

Research output: Contribution to journalArticle

23 Citations (Scopus)

Abstract

A geochemical study on fluids from selected spontaneous seepages and drilled wells was carried out together with geologic investigation and deep cross-sections reconstruction to examine the petroleum system in the western Northern Apennines foothills. The hydrocarbons occurring in the Miocene foredeep units that form the reservoirs are commonly interpreted as generated in a source/reservoir system. However, the low Total Organic Carbon, its elevated dilution in the sediment pile and the limited amount of successions that entered in the oil window indicate a low potential for the hydrocarbons generation. The structures deformation in the Northern Apennines foothills is mainly late Miocene to Pliocene in age and involves successions that are progressively younger towards southeast. The earlier structure forms the Salsomaggiore anticline in the western sector. The comparison of the fluids from the wells and the mud volcanoes shows high geochemical and thermal history similarities. Saline waters originate from the connate pore water entrapped in the Miocene reservoir rocks during their deposition. The gaseous hydrocarbons are a mixture of secondary biogenic methane and primary and secondary thermogenic gases. The associated oils show both early and late maturities. These evidences account for different generation and migration steps, depending on burial conditions and deformation time. The various reservoirs appear confined by the thrust detachment at different depths and by the occurrence of reactivated lateral ramps. These results suggest the occurrence of a common source rock deeper than the Tertiary reservoir units, which progressively entered in the oil window. This source rock could have wide lateral extension, at least comparable with the width of the studied area, and represent a prime exploration target to evaluate the undiscovered oil and gas resources. © 2013 Elsevier Ltd.
Original languageEnglish
Pages (from-to)57-76
Number of pages20
JournalMarine and Petroleum Geology
Volume48
DOIs
Publication statusPublished - Dec 2013

Fingerprint

crude oil
Italy
petroleum
oils
oil
Miocene
hydrocarbons
source rock
rocks
hydrocarbon
well
mud volcano
fluid
hydrocarbon generation
occurrences
forearc basin
reservoir rock
anticlines
seepage
anticline

Keywords

  • Cold seeps
  • Geochemistry
  • Northern Apennines
  • Petroleum system

Cite this

A new model of the petroleum system in the Northern Apennines, Italy. / Oppo, Davide; Capozzi, Rossella; Picotti, Vincenzo.

In: Marine and Petroleum Geology, Vol. 48, 12.2013, p. 57-76.

Research output: Contribution to journalArticle

Oppo, Davide ; Capozzi, Rossella ; Picotti, Vincenzo. / A new model of the petroleum system in the Northern Apennines, Italy. In: Marine and Petroleum Geology. 2013 ; Vol. 48. pp. 57-76.
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abstract = "A geochemical study on fluids from selected spontaneous seepages and drilled wells was carried out together with geologic investigation and deep cross-sections reconstruction to examine the petroleum system in the western Northern Apennines foothills. The hydrocarbons occurring in the Miocene foredeep units that form the reservoirs are commonly interpreted as generated in a source/reservoir system. However, the low Total Organic Carbon, its elevated dilution in the sediment pile and the limited amount of successions that entered in the oil window indicate a low potential for the hydrocarbons generation. The structures deformation in the Northern Apennines foothills is mainly late Miocene to Pliocene in age and involves successions that are progressively younger towards southeast. The earlier structure forms the Salsomaggiore anticline in the western sector. The comparison of the fluids from the wells and the mud volcanoes shows high geochemical and thermal history similarities. Saline waters originate from the connate pore water entrapped in the Miocene reservoir rocks during their deposition. The gaseous hydrocarbons are a mixture of secondary biogenic methane and primary and secondary thermogenic gases. The associated oils show both early and late maturities. These evidences account for different generation and migration steps, depending on burial conditions and deformation time. The various reservoirs appear confined by the thrust detachment at different depths and by the occurrence of reactivated lateral ramps. These results suggest the occurrence of a common source rock deeper than the Tertiary reservoir units, which progressively entered in the oil window. This source rock could have wide lateral extension, at least comparable with the width of the studied area, and represent a prime exploration target to evaluate the undiscovered oil and gas resources. {\circledC} 2013 Elsevier Ltd.",
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note = "Acknowledgements The Authors are indebted with the administrations of the “Riserva Naturale delle Salse di Nirano” and of the “Terme di Salsomaggiore e di Tabiano S.p.A.” for the kind permission to sample the fluids from the mud volcanoes and the exploited wells, respectively. We wish to thank ENI S.p.A. personnel, Dr. Paolo Scotti, Dr. Angelo Riva, Dr. Roberto Galimberti and Dr. Laura Biassoni for the analyses of oils and gas, the bacterial cultures and for the fruitful discussions and suggestions. Funding was provided by the Italian PRIN 2009 Project (MIUR research grants to R. Capozzi). Fran{\cc}ois Roure and an anonymous reviewer are warmly thanked for suggestions and comments that improved the manuscript.",
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N1 - Acknowledgements The Authors are indebted with the administrations of the “Riserva Naturale delle Salse di Nirano” and of the “Terme di Salsomaggiore e di Tabiano S.p.A.” for the kind permission to sample the fluids from the mud volcanoes and the exploited wells, respectively. We wish to thank ENI S.p.A. personnel, Dr. Paolo Scotti, Dr. Angelo Riva, Dr. Roberto Galimberti and Dr. Laura Biassoni for the analyses of oils and gas, the bacterial cultures and for the fruitful discussions and suggestions. Funding was provided by the Italian PRIN 2009 Project (MIUR research grants to R. Capozzi). François Roure and an anonymous reviewer are warmly thanked for suggestions and comments that improved the manuscript.

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N2 - A geochemical study on fluids from selected spontaneous seepages and drilled wells was carried out together with geologic investigation and deep cross-sections reconstruction to examine the petroleum system in the western Northern Apennines foothills. The hydrocarbons occurring in the Miocene foredeep units that form the reservoirs are commonly interpreted as generated in a source/reservoir system. However, the low Total Organic Carbon, its elevated dilution in the sediment pile and the limited amount of successions that entered in the oil window indicate a low potential for the hydrocarbons generation. The structures deformation in the Northern Apennines foothills is mainly late Miocene to Pliocene in age and involves successions that are progressively younger towards southeast. The earlier structure forms the Salsomaggiore anticline in the western sector. The comparison of the fluids from the wells and the mud volcanoes shows high geochemical and thermal history similarities. Saline waters originate from the connate pore water entrapped in the Miocene reservoir rocks during their deposition. The gaseous hydrocarbons are a mixture of secondary biogenic methane and primary and secondary thermogenic gases. The associated oils show both early and late maturities. These evidences account for different generation and migration steps, depending on burial conditions and deformation time. The various reservoirs appear confined by the thrust detachment at different depths and by the occurrence of reactivated lateral ramps. These results suggest the occurrence of a common source rock deeper than the Tertiary reservoir units, which progressively entered in the oil window. This source rock could have wide lateral extension, at least comparable with the width of the studied area, and represent a prime exploration target to evaluate the undiscovered oil and gas resources. © 2013 Elsevier Ltd.

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