Changes

  | isbn    = 0-89181-602-X

  | isbn    = 0-89181-602-X

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Overburden rock is the total stratigraphic section above the [[source rock]].<ref name=ch04r61>Magoon, L., B., Dow, W., G., 1994, The Petroleum System--From Source to Trap: [http://store.aapg.org/detail.aspx?id=1022 AAPG Memoir 60], p. 3–24.</ref> The thickness and age of overburden rock provides a history of the rate of burial of a [[source rock]] toward and through the increasing temperature domains of the basin. This includes the range of temperatures necessary for cracking kerogens into hydrocarbons. See also [[Kerogen type and hydrocarbon generation]].)

Overburden rock is the total stratigraphic section above the [[source rock]].<ref name=ch04r61>Magoon, L. B., and W. G. Dow, 1994, The Petroleum System--From Source to Trap: [http://store.aapg.org/detail.aspx?id=1022 AAPG Memoir 60], p. 3–24.</ref> The thickness and age of overburden rock provides a history of the rate of burial of a [[source rock]] toward and through the increasing temperature domains of the basin. This includes the range of temperatures necessary for cracking kerogens into hydrocarbons. See also [[Kerogen type and hydrocarbon generation]].)

Because the depth to the probable [[source rocks]] of the East Breaks 160-161 field hydrocarbons is unknown, multiple working hypotheses must be considered. Four intervals of identified source rock are reported by Gross et al..<ref name=ch04r40>Gross, O., P., Hood, K., C., Wenger, L., M., Harrison, S., C., 1995, Seismic imaging and analysis of source and migration within an integrated hydrocarbon system study, northern Gulf of Mexico basin: Abstracts, 1st Latin American Geophysical conference, p. 1–4.</ref> (Figure 4-5) and are plotted on Figure 4-45. Also plotted is the speculated middle Miocene source rock of Dow et al.<ref name=ch04r29>Dow, W., G., Yukler, M., A., Senftle, J., T., Kennicutt, M. C. II, Armentrout, J., M., 1990, Miocene oil source beds in the East Breaks basin, Flex-Trend, offshore Texas: Proceedings, Gulf Coast Section SEPM 9th Annual Research conference, p. 139–150.</ref> Gross et al.<ref name=ch04r40 />) consider the petroleum of the East Breaks area to have been sourced by [[Jurassic]] marine mudstones for the oil and [[Paleogene]] marine mudstones for the gas. Alternatively, Dow et al.<ref name=ch04r29 />) suggest middle [[Miocene]] marine mudstones as the probable source rock, although Taylor and Armentrout<ref name=ch04r93>Taylor, G., S., Armentrout, J., M., 1990, Rock geochemistry and relationships to produced oils from upper Pliocene turbidites, High Island area, Gulf of Mexico: Proceedings, Gulf Coast Section SEPM 9th Annual Research conference, p. 151–161.</ref> believe the source rock facies to be older than the Miocene slope mudstones.

Because the depth to the probable [[source rocks]] of the East Breaks 160-161 field hydrocarbons is unknown, multiple working hypotheses must be considered. Four intervals of identified source rock are reported by Gross et al..<ref name=ch04r40>Gross, O. P., K. C. Hood, L. M. Wenger, and S. C. Harrison, 1995, Seismic imaging and analysis of source and migration within an integrated hydrocarbon system study, northern Gulf of Mexico basin: Abstracts, 1st Latin American Geophysical conference, p. 1–4.</ref> (Figure 4-5) and are plotted on Figure 4-45. Also plotted is the speculated middle Miocene source rock of Dow et al.<ref name=ch04r29>Dow, W. G., M. A. Yukler, J. T. Senftle, M. C. Kennicutt, and J. M. Armentrout, 1990, Miocene oil source beds in the East Breaks basin, Flex-Trend, offshore Texas: Proceedings, Gulf Coast Section SEPM 9th Annual Research conference, p. 139–150.</ref> Gross et al.<ref name=ch04r40 />) consider the petroleum of the East Breaks area to have been sourced by [[Jurassic]] marine mudstones for the oil and [[Paleogene]] marine mudstones for the gas. Alternatively, Dow et al.<ref name=ch04r29 />) suggest middle [[Miocene]] marine mudstones as the probable source rock, although Taylor and Armentrout<ref name=ch04r93>Taylor, G. S., and J. M. Armentrout, 1990, Rock geochemistry and relationships to produced oils from upper Pliocene turbidites, High Island area, Gulf of Mexico: Proceedings, Gulf Coast Section SEPM 9th Annual Research conference, p. 151–161.</ref> believe the source rock facies to be older than the Miocene slope mudstones.

==Rate of accumulation==

==Rate of accumulation==