Article ID Journal Published Year Pages File Type
1753918 International Journal of Coal Geology 2010 24 Pages PDF
Abstract
The elevated geothermal gradient sparking hydrothermal alteration in the OM-bearing Um Irna Formation during the Late Permian may be accounted for as related to a precursor stage of the Dead Sea Rift, which is still active today in terms of migration of hot brines and hydrocarbons.
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Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Economic Geology
Preview
Deposition and alteration of carbonaceous series within a Neotethyan rift at the western boundary of the Arabian Plate: The Late Permian Um Irna Formation, NW Jordan, a petroleum system
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