Thermal evolution of the Newark Basin

J. E. Huntoon, Kevin Patrick Furlong

Research output: Contribution to journalArticle

8 Citations (Scopus)

Abstract

A one-dimensional conductive thermal model is used to calculate the transient thermal history of the Newark basin. A burial and erosion history for the Newark basin is constructed for the modeling, including changes in heat flow through time, emplacement of Jurassic lava flows at the surface, and emplacement of the Palisades sill at depth. Vitrinite-reflectance values and apatite and zircon fission-track ages, for units of both Triassic and Jurassic age, are used to constrain the models. Modeling results indicate that initial formation of the Newark basin is not coincident in time with a thermal event. Elevated heat flow did affect the basin during its evolution, however, and was associated with igneous activity. The original sedimentary package in the Newark basin was approximately 2.5 km thicker than today. -from Authors

Original languageEnglish (US)
Pages (from-to)579-591
Number of pages13
JournalJournal of Geology
Volume100
Issue number5
DOIs
StatePublished - Jan 1 1992

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thermal evolution
basin
heat flow
emplacement
Jurassic
vitrinite reflectance
history
lava flow
sill
apatite
modeling
zircon
Triassic
erosion

All Science Journal Classification (ASJC) codes

  • Geology

Cite this

Huntoon, J. E. ; Furlong, Kevin Patrick. / Thermal evolution of the Newark Basin. In: Journal of Geology. 1992 ; Vol. 100, No. 5. pp. 579-591.
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Thermal evolution of the Newark Basin. / Huntoon, J. E.; Furlong, Kevin Patrick.

In: Journal of Geology, Vol. 100, No. 5, 01.01.1992, p. 579-591.

Research output: Contribution to journalArticle

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